{"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"a-1","ChoiceLabel":"A-1","ChoiceObsolete":0,"ChoiceDescription":"Granular materials (35% or less passing No. 200 sieve), silty or clayey gravel and sand. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"a-1-a","ChoiceLabel":"A-1-a","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"a-1-b","ChoiceLabel":"A-1-b","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"a-2","ChoiceLabel":"A-2","ChoiceObsolete":0,"ChoiceDescription":"Granular materials (35% or less passing No. 200), silty or clayey gravel and sand. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"a-2-4","ChoiceLabel":"A-2-4","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"a-2-5","ChoiceLabel":"A-2-5","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"a-2-6","ChoiceLabel":"A-2-6","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"a-2-7","ChoiceLabel":"A-2-7","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"a-3","ChoiceLabel":"A-3","ChoiceObsolete":0,"ChoiceDescription":"Granular materials (35% or less passing No. 200), fine sand. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"a-4","ChoiceLabel":"A-4","ChoiceObsolete":0,"ChoiceDescription":"Silt-Clay materials (more than 35% passing NO. 200), silty soils. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"a-5","ChoiceLabel":"A-5","ChoiceObsolete":0,"ChoiceDescription":"Silt-Clay Materials (more than 35% passing No. 200), clayey soils. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"a-6","ChoiceLabel":"A-6","ChoiceObsolete":0,"ChoiceDescription":"Silt-Clay materials (more than 35% passing No. 200) clayey soils. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"a-7","ChoiceLabel":"A-7","ChoiceObsolete":0,"ChoiceDescription":"Silt-Clay materials (more than 35% passing No. 200), clayey soils. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"a-7-5","ChoiceLabel":"A-7-5","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"a-7-6","ChoiceLabel":"A-7-6","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"a-8","ChoiceLabel":"A-8","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"aashtocl","ColumnLogicalName":"aashto_group_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"a-1","ChoiceLabel":"A-1","ChoiceObsolete":0,"ChoiceDescription":"Granular materials (35% or less passing No. 200 sieve), silty or clayey gravel and sand. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"a-1-a","ChoiceLabel":"A-1-a","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"a-1-b","ChoiceLabel":"A-1-b","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"a-2","ChoiceLabel":"A-2","ChoiceObsolete":0,"ChoiceDescription":"Granular materials (35% or less passing No. 200), silty or clayey gravel and sand. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"a-2-4","ChoiceLabel":"A-2-4","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"a-2-5","ChoiceLabel":"A-2-5","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"a-2-6","ChoiceLabel":"A-2-6","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"a-2-7","ChoiceLabel":"A-2-7","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"a-3","ChoiceLabel":"A-3","ChoiceObsolete":0,"ChoiceDescription":"Granular materials (35% or less passing No. 200), fine sand. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"a-4","ChoiceLabel":"A-4","ChoiceObsolete":0,"ChoiceDescription":"Silt-Clay materials (more than 35% passing NO. 200), silty soils. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"a-5","ChoiceLabel":"A-5","ChoiceObsolete":0,"ChoiceDescription":"Silt-Clay Materials (more than 35% passing No. 200), clayey soils. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"a-6","ChoiceLabel":"A-6","ChoiceObsolete":0,"ChoiceDescription":"Silt-Clay materials (more than 35% passing No. 200) clayey soils. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"a-7","ChoiceLabel":"A-7","ChoiceObsolete":0,"ChoiceDescription":"Silt-Clay materials (more than 35% passing No. 200), clayey soils. Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"a-7-5","ChoiceLabel":"A-7-5","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"a-7-6","ChoiceLabel":"A-7-6","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":99,"DomainName":"aashto_group_classification","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"a-8","ChoiceLabel":"A-8","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material for highway and airfield construction (Procedure M 145-73 in Am. Assoc. of State Highway and Transportation Officials, 1984.","ColumnPhysicalName":"osdaashtocl","ColumnLogicalName":"osd_aashto_grp_classification"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"1","ChoiceLabel":"1","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 1 have few limitations that restrict their use.","ColumnPhysicalName":"irrcapcl","ColumnLogicalName":"irrigated_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"2","ChoiceLabel":"2","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 2 have some limitations that reduce the choice of plants or require moderate conservation practices","ColumnPhysicalName":"irrcapcl","ColumnLogicalName":"irrigated_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"3","ChoiceLabel":"3","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 3 have severe limitations that reduce the choice of plants or require special conservation practices, or both.","ColumnPhysicalName":"irrcapcl","ColumnLogicalName":"irrigated_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"4","ChoiceLabel":"4","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 4 have very severe limitations that restrict the choice of plants, require very careful management, or both","ColumnPhysicalName":"irrcapcl","ColumnLogicalName":"irrigated_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"5","ChoiceLabel":"5","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 5 have little or no erosion hazard, but have other limitations impractical to remove that limit their use.","ColumnPhysicalName":"irrcapcl","ColumnLogicalName":"irrigated_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"6","ChoiceLabel":"6","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 6 have very severe limitations that make them generally unsuited to cultivation and limit their use largely to pasture, etc.","ColumnPhysicalName":"irrcapcl","ColumnLogicalName":"irrigated_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"7","ChoiceLabel":"7","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 7 have very severe limitations that make them unsuited to cultivation and that restrict their use to grazing, etc.","ColumnPhysicalName":"irrcapcl","ColumnLogicalName":"irrigated_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"8","ChoiceLabel":"8","ChoiceObsolete":0,"ChoiceDescription":"Soils (and landforms) in Class 8 have limitations that preclude their use for commercial plant production and restrict their use.","ColumnPhysicalName":"irrcapcl","ColumnLogicalName":"irrigated_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"1","ChoiceLabel":"1","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 1 have few limitations that restrict their use.","ColumnPhysicalName":"nirrcapcl","ColumnLogicalName":"nonirr_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"2","ChoiceLabel":"2","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 2 have some limitations that reduce the choice of plants or require moderate conservation practices","ColumnPhysicalName":"nirrcapcl","ColumnLogicalName":"nonirr_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"3","ChoiceLabel":"3","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 3 have severe limitations that reduce the choice of plants or require special conservation practices, or both.","ColumnPhysicalName":"nirrcapcl","ColumnLogicalName":"nonirr_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"4","ChoiceLabel":"4","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 4 have very severe limitations that restrict the choice of plants, require very careful management, or both","ColumnPhysicalName":"nirrcapcl","ColumnLogicalName":"nonirr_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"5","ChoiceLabel":"5","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 5 have little or no erosion hazard, but have other limitations impractical to remove that limit their use.","ColumnPhysicalName":"nirrcapcl","ColumnLogicalName":"nonirr_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"6","ChoiceLabel":"6","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 6 have very severe limitations that make them generally unsuited to cultivation and limit their use largely to pasture, etc.","ColumnPhysicalName":"nirrcapcl","ColumnLogicalName":"nonirr_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"7","ChoiceLabel":"7","ChoiceObsolete":0,"ChoiceDescription":"Soils in Class 7 have very severe limitations that make them unsuited to cultivation and that restrict their use to grazing, etc.","ColumnPhysicalName":"nirrcapcl","ColumnLogicalName":"nonirr_capability_class"} {"DomainID":100,"DomainName":"capability_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"8","ChoiceLabel":"8","ChoiceObsolete":0,"ChoiceDescription":"Soils (and landforms) in Class 8 have limitations that preclude their use for commercial plant production and restrict their use.","ColumnPhysicalName":"nirrcapcl","ColumnLogicalName":"nonirr_capability_class"} {"DomainID":101,"DomainName":"capability_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"e","ChoiceLabel":"e","ChoiceObsolete":0,"ChoiceDescription":"erosion","ColumnPhysicalName":"irrcapscl","ColumnLogicalName":"irrigated_capability_subclass"} {"DomainID":101,"DomainName":"capability_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"w","ChoiceLabel":"w","ChoiceObsolete":0,"ChoiceDescription":"excess water","ColumnPhysicalName":"irrcapscl","ColumnLogicalName":"irrigated_capability_subclass"} {"DomainID":101,"DomainName":"capability_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"s","ChoiceLabel":"s","ChoiceObsolete":0,"ChoiceDescription":"soil limitations within the rooting zone","ColumnPhysicalName":"irrcapscl","ColumnLogicalName":"irrigated_capability_subclass"} {"DomainID":101,"DomainName":"capability_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"c","ChoiceLabel":"c","ChoiceObsolete":0,"ChoiceDescription":"climate condition","ColumnPhysicalName":"irrcapscl","ColumnLogicalName":"irrigated_capability_subclass"} {"DomainID":101,"DomainName":"capability_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"e","ChoiceLabel":"e","ChoiceObsolete":0,"ChoiceDescription":"erosion","ColumnPhysicalName":"nirrcapscl","ColumnLogicalName":"nonirr_capability_subclass"} {"DomainID":101,"DomainName":"capability_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"w","ChoiceLabel":"w","ChoiceObsolete":0,"ChoiceDescription":"excess water","ColumnPhysicalName":"nirrcapscl","ColumnLogicalName":"nonirr_capability_subclass"} {"DomainID":101,"DomainName":"capability_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"s","ChoiceLabel":"s","ChoiceObsolete":0,"ChoiceDescription":"soil limitations within the rooting zone","ColumnPhysicalName":"nirrcapscl","ColumnLogicalName":"nonirr_capability_subclass"} {"DomainID":101,"DomainName":"capability_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"c","ChoiceLabel":"c","ChoiceObsolete":0,"ChoiceDescription":"climate condition","ColumnPhysicalName":"nirrcapscl","ColumnLogicalName":"nonirr_capability_subclass"} {"DomainID":102,"DomainName":"component_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"family","ChoiceLabel":"Family","ChoiceObsolete":0,"ChoiceDescription":"The component is classified and described at the family level of Soil Taxonomy.","ColumnPhysicalName":"compkind","ColumnLogicalName":"component_kind"} {"DomainID":102,"DomainName":"component_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":2,"ChoiceName":"taxon above family","ChoiceLabel":"Taxon above family","ChoiceObsolete":0,"ChoiceDescription":"The component is described and classified at some level of Soil Taxonomy above the family level.","ColumnPhysicalName":"compkind","ColumnLogicalName":"component_kind"} {"DomainID":102,"DomainName":"component_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":3,"ChoiceName":"miscellaneous area","ChoiceLabel":"Miscellaneous area","ChoiceObsolete":0,"ChoiceDescription":"The component is classified and described as a non-soil area.","ColumnPhysicalName":"compkind","ColumnLogicalName":"component_kind"} {"DomainID":102,"DomainName":"component_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":4,"ChoiceName":"series","ChoiceLabel":"Series","ChoiceObsolete":0,"ChoiceDescription":"The component is classified and described at the soil series level, the lowest level of Soil Taxonomy.","ColumnPhysicalName":"compkind","ColumnLogicalName":"component_kind"} {"DomainID":102,"DomainName":"component_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":5,"ChoiceName":"taxadjunct","ChoiceLabel":"Taxadjunct","ChoiceObsolete":0,"ChoiceDescription":"The component is described slightly outside the Soil Taxomonic limits of the name assigned. However, these differences are not significant enough to affect use and management of the soil.","ColumnPhysicalName":"compkind","ColumnLogicalName":"component_kind"} {"DomainID":102,"DomainName":"component_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"variant","ChoiceLabel":"Variant","ChoiceObsolete":1,"ChoiceDescription":"The component is described as being outside the range of the series for which it is named. 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Some are saturated with water for long periods, or were once saturated but are now artificially drained; others have never been saturated.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"A","ChoiceLabel":"A","ChoiceObsolete":0,"ChoiceDescription":"Mineral horizons which have formed at the surface or below an O horizon; they exhibit obliteration of all or much of the original rock structure and show one or both of the following: (1) an accumulation of humified organic closely mixed with the mineral fraction and not dominated by properties characteristic of E or B horizons, or (2) properties resulting from cultivation, pasturing, or similar kinds of disturbance.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"E","ChoiceLabel":"E","ChoiceObsolete":0,"ChoiceDescription":"Mineral horizons in which the main feature is loss of silicate clay, iron, or aluminum, or some combination of these, leaving a concentration of sand and silt particles. These horizons exhibit obliteration of all or much of the original rock structure.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"B","ChoiceLabel":"B","ChoiceObsolete":0,"ChoiceDescription":"Horizons which have formed below an A, E, or O horizon. They are dominated by the obliteration of all or much of the original rock structure and show one or more of the following:\r\n\r\n1. Illuvial concentration of silicate clay, iron, aluminum, humus, carbonates, gypsum, or silica, alone or in combination;\r\n2. Evidence of the removal or addition of carbonates;\r\n3. Residual concentration of oxides;\r\n4. Coatings of sesquioxides that make the horizon conspicuously lower in color value, higher in chroma, or redder in hue, without apparent illuviation of iron; \r\n5. Alteration that forms silicate clay or liberates oxides, or both, and that forms a granular, blocky, or prismatic structure if volume changes accompany changes in moisture content; \r\n6. Brittleness; or\r\n7. Strong gleying.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"C","ChoiceLabel":"C","ChoiceObsolete":0,"ChoiceDescription":"Horizons or layers, excluding hard bedrock, that are little affected by pedogenic processes and lack the properties of O, A, E, or B horizons. Most are mineral layers. The material of C layers may be either like or unlike the material from which the solum has presumably formed. The C horizon may have been modified, even if there is no evidence of pedogenesis.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"R","ChoiceLabel":"R","ChoiceObsolete":0,"ChoiceDescription":"Strongly cemented to indurated bedrock.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"AB","ChoiceLabel":"AB","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"AE","ChoiceLabel":"AE","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"AC","ChoiceLabel":"AC","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"EA","ChoiceLabel":"EA","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"EB","ChoiceLabel":"EB","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"BA","ChoiceLabel":"BA","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"BE","ChoiceLabel":"BE","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"BC","ChoiceLabel":"BC","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"CA","ChoiceLabel":"CA","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"CB","ChoiceLabel":"CB","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"A/E","ChoiceLabel":"A/E","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"A/B","ChoiceLabel":"A/B","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"A/C","ChoiceLabel":"A/C","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":20,"ChoiceName":"E/A","ChoiceLabel":"E/A","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":21,"ChoiceName":"E/B","ChoiceLabel":"E/B","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":22,"ChoiceName":"B/A","ChoiceLabel":"B/A","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":23,"ChoiceName":"B/E","ChoiceLabel":"B/E","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":24,"ChoiceName":"B/C","ChoiceLabel":"B/C","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":25,"ChoiceValue":25,"ChoiceName":"C/A","ChoiceLabel":"C/A","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":26,"ChoiceName":"C/B","ChoiceLabel":"C/B","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":27,"ChoiceValue":27,"ChoiceName":"E and B","ChoiceLabel":"E and B","ChoiceObsolete":0,"ChoiceDescription":"Horizons that are composed of lamellae that are separated from each other by eluvial layers.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":28,"ChoiceValue":28,"ChoiceName":"O'","ChoiceLabel":"O'","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":29,"ChoiceName":"A'","ChoiceLabel":"A'","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":30,"ChoiceValue":30,"ChoiceName":"E'","ChoiceLabel":"E'","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":31,"ChoiceValue":31,"ChoiceName":"B'","ChoiceLabel":"B'","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":32,"ChoiceValue":32,"ChoiceName":"C'","ChoiceLabel":"C'","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":33,"ChoiceValue":33,"ChoiceName":"O''","ChoiceLabel":"O''","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":34,"ChoiceValue":34,"ChoiceName":"A''","ChoiceLabel":"A''","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":35,"ChoiceValue":35,"ChoiceName":"E''","ChoiceLabel":"E''","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":36,"ChoiceValue":36,"ChoiceName":"B''","ChoiceLabel":"B''","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":37,"ChoiceValue":37,"ChoiceName":"C''","ChoiceLabel":"C''","ChoiceObsolete":1,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":38,"ChoiceValue":38,"ChoiceName":"H","ChoiceLabel":"H","ChoiceObsolete":1,"ChoiceDescription":"A horizon designation that will only be used for conversion from SSSD layers to NASIS horizons. This designation should never be used aside for this one purpose.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":39,"ChoiceValue":39,"ChoiceName":"W","ChoiceLabel":"W","ChoiceObsolete":0,"ChoiceDescription":"Water. This symbol indicates water layers within or beneath the soil. The water layer is designated as Wf if it is permanently frozen and as W if it is not permanently frozen. The W (or Wf) designation is not used for shallow water, ice, or snow above the soil surface.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":40,"ChoiceValue":40,"ChoiceName":"L","ChoiceLabel":"L","ChoiceObsolete":0,"ChoiceDescription":"Layers dominated by limnic material. Limnic horizons or layers include both organic and mineral limnic materials that were either (1) deposited in water by precipitation or through the actions of aquatic organisms, such as algae and diatoms, or (2) derived from underwater and floating aquatic plants and subsequently modified by aquatic animals.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":41,"ChoiceValue":41,"ChoiceName":"EC","ChoiceLabel":"EC","ChoiceObsolete":0,"ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":42,"ChoiceValue":42,"ChoiceName":"B and E","ChoiceLabel":"B and E","ChoiceObsolete":0,"ChoiceDescription":"Horizons that are composed of lamellae that are separated from each other by eluvial layers.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":43,"ChoiceValue":43,"ChoiceName":"M","ChoiceLabel":"M","ChoiceObsolete":0,"ChoiceDescription":"Root-limiting, subsoil layers consisting of nearly continuous, horizontally oriented, human manufactured materials. Examples of materials designated by the letter M include geotextile liners, asphalt, concrete, rubber, and plastic.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":44,"ChoiceValue":44,"ChoiceName":"^O","ChoiceLabel":"^O","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"O\" indicates layers dominated by organic material. Some are saturated with water for long periods, or were once saturated but are now artificially drained; others have never been saturated.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":45,"ChoiceValue":45,"ChoiceName":"^A","ChoiceLabel":"^A","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"A\" is assigned to mineral horizons which have formed at the surface or below an O horizon; they exhibit obliteration of all or much of the original rock structure and show one or both of the following: (1) an accumulation of humified organic closely mixed with the mineral fraction and not dominated by properties characteristic of E or B horizons, or (2) properties resulting from cultivation, pasturing, or similar kinds of disturbance.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":46,"ChoiceValue":46,"ChoiceName":"^E","ChoiceLabel":"^E","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"E\" is assigned to mineral horizons in which the main feature is loss of silicate clay, iron, or aluminum, or some combination of these, leaving a concentration of sand and silt particles. These horizons exhibit obliteration of all or much of the original rock structure.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":47,"ChoiceValue":47,"ChoiceName":"^B","ChoiceLabel":"^B","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"B\" is assiged to horizons which have formed below an A, E, or O horizon. They are dominated by the obliteration of all or much of the original rock structure and show one or more of the following:\r\n\r\n1. Illuvial concentration of silicate clay, iron, aluminum, humus, carbonates, gypsum, or silica, alone or in combination;\r\n2. Evidence of the removal or addition of carbonates;\r\n3. Residual concentration of oxides;\r\n4. Coatings of sesquioxides that make the horizon conspicuously lower in color value, higher in chroma, or redder in hue, without apparent illuviation of iron; \r\n5. Alteration that forms silicate clay or liberates oxides, or both, and that forms a granular, blocky, or prismatic structure if volume changes accompany changes in moisture content; \r\n6. Brittleness; or\r\n7. Strong gleying.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":48,"ChoiceValue":48,"ChoiceName":"^C","ChoiceLabel":"^C","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"C\" is assigned to horizons or layers, excluding hard bedrock, that are little affected by pedogenic processes and lack the properties of O, A, E, or B horizons. Most are mineral layers. The material of C layers may be either like or unlike the material from which the solum has presumably formed. The C horizon may have been modified, even if there is no evidence of pedogenesis.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":49,"ChoiceValue":49,"ChoiceName":"^AB","ChoiceLabel":"^AB","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":50,"ChoiceValue":50,"ChoiceName":"^BA","ChoiceLabel":"^BA","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":51,"ChoiceValue":51,"ChoiceName":"^AE","ChoiceLabel":"^AE","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":52,"ChoiceValue":52,"ChoiceName":"^EA","ChoiceLabel":"^EA","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":53,"ChoiceValue":53,"ChoiceName":"^EB","ChoiceLabel":"^EB","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":54,"ChoiceValue":54,"ChoiceName":"^BE","ChoiceLabel":"^BE","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":55,"ChoiceValue":55,"ChoiceName":"^AC","ChoiceLabel":"^AC","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":56,"ChoiceValue":56,"ChoiceName":"^CA","ChoiceLabel":"^CA","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":57,"ChoiceValue":57,"ChoiceName":"^BC","ChoiceLabel":"^BC","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":58,"ChoiceValue":58,"ChoiceName":"^CB","ChoiceLabel":"^CB","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":59,"ChoiceValue":59,"ChoiceName":"^A/B","ChoiceLabel":"^A/B","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":60,"ChoiceValue":60,"ChoiceName":"^B/A","ChoiceLabel":"^B/A","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":61,"ChoiceValue":61,"ChoiceName":"^A/E","ChoiceLabel":"^A/E","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":62,"ChoiceValue":62,"ChoiceName":"^E/A","ChoiceLabel":"^E/A","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":63,"ChoiceValue":63,"ChoiceName":"^A/C","ChoiceLabel":"^A/C","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":64,"ChoiceValue":64,"ChoiceName":"^C/A","ChoiceLabel":"^C/A","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":65,"ChoiceValue":65,"ChoiceName":"^B/C","ChoiceLabel":"^B/C","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":66,"ChoiceValue":66,"ChoiceName":"^C/B","ChoiceLabel":"^C/B","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":67,"ChoiceValue":67,"ChoiceName":"V","ChoiceLabel":"V","ChoiceObsolete":0,"ChoiceDescription":"V horizon can be defined as: Mineral horizons that have formed at the soil surface, or below a layer of rock fragments (e.g., desert pavement) or a physical or biological crust in arid environments. They are recognized by the predominance of vesicular pores indicating a soil morphology that drastically reduces or prevents the infiltration of rainfall, and air exchange with the atmosphere. They are unvegetated and appear with unbroken massive structural morphology that is often very friable when moist, slightly hard to very hard when dry, but not cemented. They have no or only very weak secondary structural aggregates. V horizons are often lighter in color ( higher value) and lower in organic carbon than the horizon below it.","ColumnPhysicalName":"desgnmaster","ColumnLogicalName":"horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"O","ChoiceLabel":"O","ChoiceObsolete":0,"ChoiceDescription":"Layers dominated by organic material. Some are saturated with water for long periods, or were once saturated but are now artificially drained; others have never been saturated.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"A","ChoiceLabel":"A","ChoiceObsolete":0,"ChoiceDescription":"Mineral horizons which have formed at the surface or below an O horizon; they exhibit obliteration of all or much of the original rock structure and show one or both of the following: (1) an accumulation of humified organic closely mixed with the mineral fraction and not dominated by properties characteristic of E or B horizons, or (2) properties resulting from cultivation, pasturing, or similar kinds of disturbance.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"E","ChoiceLabel":"E","ChoiceObsolete":0,"ChoiceDescription":"Mineral horizons in which the main feature is loss of silicate clay, iron, or aluminum, or some combination of these, leaving a concentration of sand and silt particles. These horizons exhibit obliteration of all or much of the original rock structure.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"B","ChoiceLabel":"B","ChoiceObsolete":0,"ChoiceDescription":"Horizons which have formed below an A, E, or O horizon. They are dominated by the obliteration of all or much of the original rock structure and show one or more of the following:\r\n\r\n1. Illuvial concentration of silicate clay, iron, aluminum, humus, carbonates, gypsum, or silica, alone or in combination;\r\n2. Evidence of the removal or addition of carbonates;\r\n3. Residual concentration of oxides;\r\n4. Coatings of sesquioxides that make the horizon conspicuously lower in color value, higher in chroma, or redder in hue, without apparent illuviation of iron; \r\n5. Alteration that forms silicate clay or liberates oxides, or both, and that forms a granular, blocky, or prismatic structure if volume changes accompany changes in moisture content; \r\n6. Brittleness; or\r\n7. Strong gleying.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"C","ChoiceLabel":"C","ChoiceObsolete":0,"ChoiceDescription":"Horizons or layers, excluding hard bedrock, that are little affected by pedogenic processes and lack the properties of O, A, E, or B horizons. Most are mineral layers. The material of C layers may be either like or unlike the material from which the solum has presumably formed. The C horizon may have been modified, even if there is no evidence of pedogenesis.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"R","ChoiceLabel":"R","ChoiceObsolete":0,"ChoiceDescription":"Strongly cemented to indurated bedrock.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"AB","ChoiceLabel":"AB","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"AE","ChoiceLabel":"AE","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"AC","ChoiceLabel":"AC","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"EA","ChoiceLabel":"EA","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"EB","ChoiceLabel":"EB","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"BA","ChoiceLabel":"BA","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"BE","ChoiceLabel":"BE","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"BC","ChoiceLabel":"BC","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"CA","ChoiceLabel":"CA","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"CB","ChoiceLabel":"CB","ChoiceObsolete":0,"ChoiceDescription":"Horizons dominated by properties of one master horizon but having subordinate properties of another. The first of these symbols indicates that the properties of the horizon so designated dominate the transitional horizon. An AB horizon, for example, has characteristics of both an overlying A horizon and an underlying B horizon, but it is more like the A than like the B.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"A/E","ChoiceLabel":"A/E","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"A/B","ChoiceLabel":"A/B","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"A/C","ChoiceLabel":"A/C","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":20,"ChoiceName":"E/A","ChoiceLabel":"E/A","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":21,"ChoiceName":"E/B","ChoiceLabel":"E/B","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":22,"ChoiceName":"B/A","ChoiceLabel":"B/A","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":23,"ChoiceName":"B/E","ChoiceLabel":"B/E","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":24,"ChoiceName":"B/C","ChoiceLabel":"B/C","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":25,"ChoiceValue":25,"ChoiceName":"C/A","ChoiceLabel":"C/A","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":26,"ChoiceName":"C/B","ChoiceLabel":"C/B","ChoiceObsolete":0,"ChoiceDescription":"Horizons with two distinct parts that have recognizable properties of the two kinds of master horizons indicated by the capital letters. Most of the individual parts of one horizon component are surrounded by the other.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":27,"ChoiceValue":27,"ChoiceName":"E and B","ChoiceLabel":"E and B","ChoiceObsolete":0,"ChoiceDescription":"Horizons that are composed of lamellae that are separated from each other by eluvial layers.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":28,"ChoiceValue":28,"ChoiceName":"O'","ChoiceLabel":"O'","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":29,"ChoiceName":"A'","ChoiceLabel":"A'","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":30,"ChoiceValue":30,"ChoiceName":"E'","ChoiceLabel":"E'","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":31,"ChoiceValue":31,"ChoiceName":"B'","ChoiceLabel":"B'","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":32,"ChoiceValue":32,"ChoiceName":"C'","ChoiceLabel":"C'","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":33,"ChoiceValue":33,"ChoiceName":"O''","ChoiceLabel":"O''","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":34,"ChoiceValue":34,"ChoiceName":"A''","ChoiceLabel":"A''","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":35,"ChoiceValue":35,"ChoiceName":"E''","ChoiceLabel":"E''","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":36,"ChoiceValue":36,"ChoiceName":"B''","ChoiceLabel":"B''","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":37,"ChoiceValue":37,"ChoiceName":"C''","ChoiceLabel":"C''","ChoiceObsolete":1,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":38,"ChoiceValue":38,"ChoiceName":"H","ChoiceLabel":"H","ChoiceObsolete":1,"ChoiceDescription":"A horizon designation that will only be used for conversion from SSSD layers to NASIS horizons. This designation should never be used aside for this one purpose.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":39,"ChoiceValue":39,"ChoiceName":"W","ChoiceLabel":"W","ChoiceObsolete":0,"ChoiceDescription":"Water. This symbol indicates water layers within or beneath the soil. The water layer is designated as Wf if it is permanently frozen and as W if it is not permanently frozen. The W (or Wf) designation is not used for shallow water, ice, or snow above the soil surface.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":40,"ChoiceValue":40,"ChoiceName":"L","ChoiceLabel":"L","ChoiceObsolete":0,"ChoiceDescription":"Layers dominated by limnic material. Limnic horizons or layers include both organic and mineral limnic materials that were either (1) deposited in water by precipitation or through the actions of aquatic organisms, such as algae and diatoms, or (2) derived from underwater and floating aquatic plants and subsequently modified by aquatic animals.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":41,"ChoiceValue":41,"ChoiceName":"EC","ChoiceLabel":"EC","ChoiceObsolete":0,"ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":42,"ChoiceValue":42,"ChoiceName":"B and E","ChoiceLabel":"B and E","ChoiceObsolete":0,"ChoiceDescription":"Horizons that are composed of lamellae that are separated from each other by eluvial layers.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":43,"ChoiceValue":43,"ChoiceName":"M","ChoiceLabel":"M","ChoiceObsolete":0,"ChoiceDescription":"Root-limiting, subsoil layers consisting of nearly continuous, horizontally oriented, human manufactured materials. Examples of materials designated by the letter M include geotextile liners, asphalt, concrete, rubber, and plastic.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":44,"ChoiceValue":44,"ChoiceName":"^O","ChoiceLabel":"^O","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"O\" indicates layers dominated by organic material. Some are saturated with water for long periods, or were once saturated but are now artificially drained; others have never been saturated.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":45,"ChoiceValue":45,"ChoiceName":"^A","ChoiceLabel":"^A","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"A\" is assigned to mineral horizons which have formed at the surface or below an O horizon; they exhibit obliteration of all or much of the original rock structure and show one or both of the following: (1) an accumulation of humified organic closely mixed with the mineral fraction and not dominated by properties characteristic of E or B horizons, or (2) properties resulting from cultivation, pasturing, or similar kinds of disturbance.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":46,"ChoiceValue":46,"ChoiceName":"^E","ChoiceLabel":"^E","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"E\" is assigned to mineral horizons in which the main feature is loss of silicate clay, iron, or aluminum, or some combination of these, leaving a concentration of sand and silt particles. These horizons exhibit obliteration of all or much of the original rock structure.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":47,"ChoiceValue":47,"ChoiceName":"^B","ChoiceLabel":"^B","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"B\" is assiged to horizons which have formed below an A, E, or O horizon. They are dominated by the obliteration of all or much of the original rock structure and show one or more of the following:\r\n\r\n1. Illuvial concentration of silicate clay, iron, aluminum, humus, carbonates, gypsum, or silica, alone or in combination;\r\n2. Evidence of the removal or addition of carbonates;\r\n3. Residual concentration of oxides;\r\n4. Coatings of sesquioxides that make the horizon conspicuously lower in color value, higher in chroma, or redder in hue, without apparent illuviation of iron; \r\n5. Alteration that forms silicate clay or liberates oxides, or both, and that forms a granular, blocky, or prismatic structure if volume changes accompany changes in moisture content; \r\n6. Brittleness; or\r\n7. Strong gleying.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":48,"ChoiceValue":48,"ChoiceName":"^C","ChoiceLabel":"^C","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).\r\n\r\nThe \"C\" is assigned to horizons or layers, excluding hard bedrock, that are little affected by pedogenic processes and lack the properties of O, A, E, or B horizons. Most are mineral layers. The material of C layers may be either like or unlike the material from which the solum has presumably formed. The C horizon may have been modified, even if there is no evidence of pedogenesis.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":49,"ChoiceValue":49,"ChoiceName":"^AB","ChoiceLabel":"^AB","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":50,"ChoiceValue":50,"ChoiceName":"^BA","ChoiceLabel":"^BA","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":51,"ChoiceValue":51,"ChoiceName":"^AE","ChoiceLabel":"^AE","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":52,"ChoiceValue":52,"ChoiceName":"^EA","ChoiceLabel":"^EA","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":53,"ChoiceValue":53,"ChoiceName":"^EB","ChoiceLabel":"^EB","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":54,"ChoiceValue":54,"ChoiceName":"^BE","ChoiceLabel":"^BE","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":55,"ChoiceValue":55,"ChoiceName":"^AC","ChoiceLabel":"^AC","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":56,"ChoiceValue":56,"ChoiceName":"^CA","ChoiceLabel":"^CA","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":57,"ChoiceValue":57,"ChoiceName":"^BC","ChoiceLabel":"^BC","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":58,"ChoiceValue":58,"ChoiceName":"^CB","ChoiceLabel":"^CB","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":59,"ChoiceValue":59,"ChoiceName":"^A/B","ChoiceLabel":"^A/B","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":60,"ChoiceValue":60,"ChoiceName":"^B/A","ChoiceLabel":"^B/A","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":61,"ChoiceValue":61,"ChoiceName":"^A/E","ChoiceLabel":"^A/E","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":62,"ChoiceValue":62,"ChoiceName":"^E/A","ChoiceLabel":"^E/A","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":63,"ChoiceValue":63,"ChoiceName":"^A/C","ChoiceLabel":"^A/C","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":64,"ChoiceValue":64,"ChoiceName":"^C/A","ChoiceLabel":"^C/A","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":65,"ChoiceValue":65,"ChoiceName":"^B/C","ChoiceLabel":"^B/C","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":66,"ChoiceValue":66,"ChoiceName":"^C/B","ChoiceLabel":"^C/B","ChoiceObsolete":0,"ChoiceDescription":"The \"caret\" symbol (^) is used as a prefix to master horizon designations to indicate mineral or organic layers of human-transported material. This material has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. All horizons and layers formed in human-transported material are indicated by a \"caret\" prefix (e.g., ^A-^C-Ab-Btb).","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":113,"DomainName":"horz_desgn_master","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":67,"ChoiceValue":67,"ChoiceName":"V","ChoiceLabel":"V","ChoiceObsolete":0,"ChoiceDescription":"V horizon can be defined as: Mineral horizons that have formed at the soil surface, or below a layer of rock fragments (e.g., desert pavement) or a physical or biological crust in arid environments. They are recognized by the predominance of vesicular pores indicating a soil morphology that drastically reduces or prevents the infiltration of rainfall, and air exchange with the atmosphere. They are unvegetated and appear with unbroken massive structural morphology that is often very friable when moist, slightly hard to very hard when dry, but not cemented. They have no or only very weak secondary structural aggregates. V horizons are often lighter in color ( higher value) and lower in organic carbon than the horizon below it.","ColumnPhysicalName":"osddesgnmaster","ColumnLogicalName":"osd_horz_desgn_master"} {"DomainID":114,"DomainName":"hydric_condition","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"farmable","ChoiceLabel":"Farmable under natural conditions","ChoiceObsolete":0,"ChoiceDescription":"Farmable under natureal conditions.","ColumnPhysicalName":"hydricon","ColumnLogicalName":"hydric_condition"} {"DomainID":114,"DomainName":"hydric_condition","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":3,"ChoiceValue":2,"ChoiceName":"wooded","ChoiceLabel":"Wooded under natural conditions","ChoiceObsolete":0,"ChoiceDescription":"Wooded under natural conditions.","ColumnPhysicalName":"hydricon","ColumnLogicalName":"hydric_condition"} {"DomainID":114,"DomainName":"hydric_condition","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":2,"ChoiceValue":3,"ChoiceName":"neither","ChoiceLabel":"Neither wooded nor farmable under natural conditions","ChoiceObsolete":0,"ChoiceDescription":"Neither wooded nor farmable under natural conditions.","ColumnPhysicalName":"hydricon","ColumnLogicalName":"hydric_condition"} {"DomainID":115,"DomainName":"hydrologic_group","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"a","ChoiceLabel":"A","ChoiceObsolete":0,"ChoiceDescription":"Soils in this group have low runoff potential when thoroughly wet. Water is transmitted freely through the soil.","ColumnPhysicalName":"hydgrp","ColumnLogicalName":"hydrologic_group"} {"DomainID":115,"DomainName":"hydrologic_group","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"b","ChoiceLabel":"B","ChoiceObsolete":0,"ChoiceDescription":"Soils in this group have moderately low runoff potential when thoroughly wet. Water transmission through the soil is unimpeded.","ColumnPhysicalName":"hydgrp","ColumnLogicalName":"hydrologic_group"} {"DomainID":115,"DomainName":"hydrologic_group","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"c","ChoiceLabel":"C","ChoiceObsolete":0,"ChoiceDescription":"Soils in this group have moderately high runoff potential when thoroughly wet. Water transmission through the soil is somewhat restricted.","ColumnPhysicalName":"hydgrp","ColumnLogicalName":"hydrologic_group"} {"DomainID":115,"DomainName":"hydrologic_group","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"d","ChoiceLabel":"D","ChoiceObsolete":0,"ChoiceDescription":"Soils in this group have high runoff potential when thoroughly wet. Water movement through the soil is restricted or very restricted.","ColumnPhysicalName":"hydgrp","ColumnLogicalName":"hydrologic_group"} {"DomainID":115,"DomainName":"hydrologic_group","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"a/d","ChoiceLabel":"A/D","ChoiceObsolete":0,"ChoiceDescription":"These soils have low runoff potential when drained and high runoff potential when undrained.","ColumnPhysicalName":"hydgrp","ColumnLogicalName":"hydrologic_group"} {"DomainID":115,"DomainName":"hydrologic_group","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"b/d","ChoiceLabel":"B/D","ChoiceObsolete":0,"ChoiceDescription":"These soils have moderately low runoff potential when drained and high runoff potential when undrained.","ColumnPhysicalName":"hydgrp","ColumnLogicalName":"hydrologic_group"} {"DomainID":115,"DomainName":"hydrologic_group","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"c/d","ChoiceLabel":"C/D","ChoiceObsolete":0,"ChoiceDescription":"These soils have moderately high runoff potential when drained and high runoff potential when undrained.","ColumnPhysicalName":"hydgrp","ColumnLogicalName":"hydrologic_group"} {"DomainID":118,"DomainName":"mapunit_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"association","ChoiceLabel":"Association","ChoiceObsolete":0,"ChoiceDescription":"Two or more dissimilar soils that occur in a regularly repeating pattern that could have been separated at the scale of field mapping, but were not separated due to the intended purpose of the survey.","ColumnPhysicalName":"mukind","ColumnLogicalName":"mapunit_kind"} {"DomainID":118,"DomainName":"mapunit_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":2,"ChoiceName":"consociation","ChoiceLabel":"Consociation","ChoiceObsolete":0,"ChoiceDescription":"At least seventy-five percent (75%) of the map unit is within the range of the soil providing the name of the unit, and closely similar soils.","ColumnPhysicalName":"mukind","ColumnLogicalName":"mapunit_kind"} {"DomainID":118,"DomainName":"mapunit_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":3,"ChoiceName":"undifferentiated group","ChoiceLabel":"Undifferentiated group","ChoiceObsolete":0,"ChoiceDescription":"Two or more similar soils that are not always geographically associated, and are mapped together due to them having the same or very similar use and management concerns.","ColumnPhysicalName":"mukind","ColumnLogicalName":"mapunit_kind"} {"DomainID":118,"DomainName":"mapunit_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":4,"ChoiceName":"complex","ChoiceLabel":"Complex","ChoiceObsolete":0,"ChoiceDescription":"Two or more dissimilar soils that occur in a regularly repeating pattern, that cannot be separated at the scale of field mapping.","ColumnPhysicalName":"mukind","ColumnLogicalName":"mapunit_kind"} {"DomainID":120,"DomainName":"potential_frost_action","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none","ChoiceLabel":"None","ChoiceObsolete":0,"ColumnPhysicalName":"frostact","ColumnLogicalName":"potential_frost_action"} {"DomainID":120,"DomainName":"potential_frost_action","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"low","ChoiceLabel":"Low","ChoiceObsolete":0,"ColumnPhysicalName":"frostact","ColumnLogicalName":"potential_frost_action"} {"DomainID":120,"DomainName":"potential_frost_action","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ColumnPhysicalName":"frostact","ColumnLogicalName":"potential_frost_action"} {"DomainID":120,"DomainName":"potential_frost_action","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"high","ChoiceLabel":"High","ChoiceObsolete":0,"ColumnPhysicalName":"frostact","ColumnLogicalName":"potential_frost_action"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":".02","ChoiceLabel":".02","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kffact","ColumnLogicalName":"soil_erodibility_factor_rf"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":".05","ChoiceLabel":".05","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. 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National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kffact","ColumnLogicalName":"soil_erodibility_factor_rf"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":".17","ChoiceLabel":".17","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. 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National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kffact","ColumnLogicalName":"soil_erodibility_factor_rf"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":".28","ChoiceLabel":".28","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. 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National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kffact","ColumnLogicalName":"soil_erodibility_factor_rf"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":".43","ChoiceLabel":".43","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. 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National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kffact","ColumnLogicalName":"soil_erodibility_factor_rf"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":".64","ChoiceLabel":".64","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. 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National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kwfact","ColumnLogicalName":"soil_erodibility_factor_whole"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":".10","ChoiceLabel":".10","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. 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National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kwfact","ColumnLogicalName":"soil_erodibility_factor_whole"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":".20","ChoiceLabel":".20","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. 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National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kwfact","ColumnLogicalName":"soil_erodibility_factor_whole"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":".32","ChoiceLabel":".32","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. 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National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kwfact","ColumnLogicalName":"soil_erodibility_factor_whole"} {"DomainID":124,"DomainName":"soil_erodibility_factor","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":".49","ChoiceLabel":".49","ChoiceObsolete":0,"ChoiceDescription":"References: Soil Survey Manual, Agricultural Handbook No. 18, Soil Survey Staff, USDA, Natural Resources Conservation Service. National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. 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National Soil Survey Handbook, Part 618.58 Soil Erodibility Factors, USLE, RUSLE2. Agricultural Handbook 703, ARS 1997.","ColumnPhysicalName":"kwfact","ColumnLogicalName":"soil_erodibility_factor_whole"} {"DomainID":125,"DomainName":"soil_survey_area_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":1,"ChoiceName":"out-of-date","ChoiceLabel":"Out-of-date","ChoiceObsolete":0,"ChoiceDescription":"Soil survey area has a published report, but it no longer meets user needs; it requires extensive revision, as defined in NSSH Part 610.06.","ColumnPhysicalName":"ssastatus","ColumnLogicalName":"soil_survey_area_status"} {"DomainID":125,"DomainName":"soil_survey_area_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":2,"ChoiceName":"published","ChoiceLabel":"Published","ChoiceObsolete":0,"ChoiceDescription":"Soil survey area has been printed, or otherwise reproduced and issued by a Federal or State agency, and meets the current needs of users. Publication is defined as a traditional hard copy printed report, CD-ROM, web publication, or other media as agreed to by the National Cooperative Soil Survey cooperators in the memorandum of understanding.","ColumnPhysicalName":"ssastatus","ColumnLogicalName":"soil_survey_area_status"} {"DomainID":125,"DomainName":"soil_survey_area_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"nonproject","ChoiceLabel":"Nonproject","ChoiceObsolete":0,"ChoiceDescription":"Soil survey area has neither the initial mapping complete nor a signed correlation document.","ColumnPhysicalName":"ssastatus","ColumnLogicalName":"soil_survey_area_status"} {"DomainID":125,"DomainName":"soil_survey_area_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":4,"ChoiceName":"initial","ChoiceLabel":"Initial","ChoiceObsolete":0,"ChoiceDescription":"Soil survey area has a signed Memorandum of Understanding and assigned staffing to complete the initial mapping and field documentation in 3 to 5 years.","ColumnPhysicalName":"ssastatus","ColumnLogicalName":"soil_survey_area_status"} {"DomainID":125,"DomainName":"soil_survey_area_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":5,"ChoiceName":"extensive revision","ChoiceLabel":"Extensive revision","ChoiceObsolete":0,"ChoiceDescription":"Soil Survey area has a published report that requires extensive revision, as defined in NSSH Part 610.06. 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A comprehensive evaluation documents deficiencies for the entire survey area, and National Cooperative Soil Survey cooperators have agreed on the evaluation; staffing is assigned and other necessary resources are available to complete all revisions within 2 years or less.","ColumnPhysicalName":"ssastatus","ColumnLogicalName":"soil_survey_area_status"} {"DomainID":125,"DomainName":"soil_survey_area_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"update needed","ChoiceLabel":"Update needed","ChoiceObsolete":0,"ChoiceDescription":"Soil survey area has a published report that requires some degree of revision (primarily to soil maps), as defined in NSSH Part 610.06. 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{"DomainID":126,"DomainName":"taxonomic_family_mineralogy","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":39,"ChoiceName":"magnesic","ChoiceLabel":"magnesic","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"taxminalogy","ColumnLogicalName":"taxonomic_family_mineralogy"} {"DomainID":126,"DomainName":"taxonomic_family_mineralogy","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":33,"ChoiceValue":40,"ChoiceName":"paramicaceous","ChoiceLabel":"paramicaceous","ChoiceObsolete":1,"ColumnPhysicalName":"taxminalogy","ColumnLogicalName":"taxonomic_family_mineralogy"} {"DomainID":126,"DomainName":"taxonomic_family_mineralogy","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":34,"ChoiceValue":41,"ChoiceName":"parasesquic","ChoiceLabel":"parasesquic","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey 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{"DomainID":126,"DomainName":"taxonomic_family_mineralogy","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":44,"ChoiceValue":44,"ChoiceName":"anhydritic","ChoiceLabel":"anhydritic","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"taxminalogy","ColumnLogicalName":"taxonomic_family_mineralogy"} {"DomainID":126,"DomainName":"taxonomic_family_mineralogy","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":45,"ChoiceValue":45,"ChoiceName":"opaline","ChoiceLabel":"opaline","ChoiceObsolete":0,"ChoiceDescription":"Opaline\r\n30 percent or more (by weight) diatoms, plant opal and sponge spicules in the fine-earth fraction. \r\n\r\nOpaline is being added as a new mineralogy choice/class for soil layers with a substitute particle-size class (except fragmental). 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{"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":13,"ChoiceName":"ashy over loamy-skeletal","ChoiceLabel":"ashy over loamy-skeletal","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":78,"ChoiceValue":14,"ChoiceName":"medial over clayey","ChoiceLabel":"medial over clayey","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":15,"ChoiceName":"cindery over medial-skeletal","ChoiceLabel":"cindery over medial-skeletal","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":80,"ChoiceValue":16,"ChoiceName":"medial over fragmental","ChoiceLabel":"medial over fragmental","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":17,"ChoiceName":"cindery over medial","ChoiceLabel":"cindery over medial","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":82,"ChoiceValue":18,"ChoiceName":"medial over loamy","ChoiceLabel":"medial over loamy","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} 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{"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":107,"ChoiceValue":26,"ChoiceName":"thixotropic over fragmental","ChoiceLabel":"thixotropic over fragmental","ChoiceObsolete":1,"ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":110,"ChoiceValue":27,"ChoiceName":"thixotropic over sandy or sandy-skeletal","ChoiceLabel":"thixotropic over sandy or sandy-skeletal","ChoiceObsolete":1,"ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":109,"ChoiceValue":28,"ChoiceName":"thixotropic over loamy-skeletal","ChoiceLabel":"thixotropic over 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{"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":68,"ChoiceValue":33,"ChoiceName":"loamy-skeletal","ChoiceLabel":"loamy-skeletal","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":72,"ChoiceValue":34,"ChoiceName":"loamy-skeletal over fragmental","ChoiceLabel":"loamy-skeletal over fragmental","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":74,"ChoiceValue":35,"ChoiceName":"loamy-skeletal over sandy or sandy-skeletal","ChoiceLabel":"loamy-skeletal over sandy or sandy-skeletal","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} {"DomainID":127,"DomainName":"taxonomic_family_particle_size","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":71,"ChoiceValue":36,"ChoiceName":"loamy-skeletal over clayey","ChoiceLabel":"loamy-skeletal over clayey","ChoiceObsolete":0,"ChoiceDescription":"Reference: Keys to Soil Taxonomy Twelfth Edition, Soil Survey Staff, USDA, Natural Resources Conservation Service","ColumnPhysicalName":"osdtaxfamparticlesize","ColumnLogicalName":"osd_taxonomic_fam_particle_sz"} 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Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"drainagecl","ColumnLogicalName":"drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"well","ChoiceLabel":"Well drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed from the soil readily but not rapidly. Internal free water occurrence commonly is deep or very deep; annual duration is not specified. Water is available to plants throughout most of the growing season in humid regions. Wetness does not inhibit growth of roots for significant periods during most growing seasons. The soils are mainly free of the deep to redoximorphic features that are related to wetness. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"drainagecl","ColumnLogicalName":"drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderately well","ChoiceLabel":"Moderately well drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed from the soil somewhat slowly during some periods of the year. Internal free water occurrence commonly is moderately deep and transitory through permanent. The soils are wet for only a short time within the rooting depth during the growing season, but long enough that most mesophytic crops are affected. They commonly have a moderately low or lower saturated hydraulic conductivity in a layer within the upper 1 m, periodically receive high rainfall, or both. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"drainagecl","ColumnLogicalName":"drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"somewhat poorly","ChoiceLabel":"Somewhat poorly drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed slowly so that the soil is wet at a shallow depth for significant periods during the growing season. The occurrence of internal free water commonly is shallow to moderately deep and transitory to permanent. Wetness markedly restricts the growth of mesophytic crops, unless artificial drainage is provided. The soils commonly have one or more of the following characteristics: low or very low saturated hydraulic conductivity, a high water table, additional water from seepage, or nearly continuous rainfall. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"drainagecl","ColumnLogicalName":"drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"poorly","ChoiceLabel":"Poorly drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed so slowly that the soil is wet at shallow depths periodically during the growing season or remains wet for long periods. The occurrence of internal free water is shallow or very shallow and common or persistent. Free water is commonly at or near the surface long enough during the growing season so that most mesophytic crops cannot be grown, unless the soil is artificially drained. The soil, however, is not continuously wet directly below plow-depth. Free water at shallow depth is usually present. This water table is commonly the result of low or very low saturated hydraulic conductivity of nearly continuous rainfall, or of a combination of these. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"drainagecl","ColumnLogicalName":"drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"very poorly","ChoiceLabel":"Very poorly drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed from the soil so slowly that free water remains at or very near the ground surface during much of the growing season. The occurrence of internal free water is very shallow and persistent or permanent. Unless the soil is artificially drained, most mesophytic crops cannot be grown. The soils are commonly level or depressed and frequently ponded. If rainfall is high or nearly continuous, slope gradients may be greater. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"drainagecl","ColumnLogicalName":"drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"subaqueous","ChoiceLabel":"Subaqueous","ChoiceObsolete":0,"ChoiceDescription":"Free water is above the soil surface. The occurrence of internal free water is permanent and there is a positive water potential at the soil surface for more than 21 hours of each day. The soils have a peraquic soil moisture regime.","ColumnPhysicalName":"drainagecl","ColumnLogicalName":"drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"excessively","ChoiceLabel":"Excessively drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed very rapidly. The occurrence of internal free water commonly is very rare or very deep. 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Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"osddrainagecl","ColumnLogicalName":"osd_drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"well","ChoiceLabel":"Well drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed from the soil readily but not rapidly. Internal free water occurrence commonly is deep or very deep; annual duration is not specified. Water is available to plants throughout most of the growing season in humid regions. Wetness does not inhibit growth of roots for significant periods during most growing seasons. The soils are mainly free of the deep to redoximorphic features that are related to wetness. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"osddrainagecl","ColumnLogicalName":"osd_drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderately well","ChoiceLabel":"Moderately well drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed from the soil somewhat slowly during some periods of the year. Internal free water occurrence commonly is moderately deep and transitory through permanent. The soils are wet for only a short time within the rooting depth during the growing season, but long enough that most mesophytic crops are affected. They commonly have a moderately low or lower saturated hydraulic conductivity in a layer within the upper 1 m, periodically receive high rainfall, or both. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"osddrainagecl","ColumnLogicalName":"osd_drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"somewhat poorly","ChoiceLabel":"Somewhat poorly drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed slowly so that the soil is wet at a shallow depth for significant periods during the growing season. The occurrence of internal free water commonly is shallow to moderately deep and transitory to permanent. Wetness markedly restricts the growth of mesophytic crops, unless artificial drainage is provided. The soils commonly have one or more of the following characteristics: low or very low saturated hydraulic conductivity, a high water table, additional water from seepage, or nearly continuous rainfall. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"osddrainagecl","ColumnLogicalName":"osd_drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"poorly","ChoiceLabel":"Poorly drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed so slowly that the soil is wet at shallow depths periodically during the growing season or remains wet for long periods. The occurrence of internal free water is shallow or very shallow and common or persistent. Free water is commonly at or near the surface long enough during the growing season so that most mesophytic crops cannot be grown, unless the soil is artificially drained. The soil, however, is not continuously wet directly below plow-depth. Free water at shallow depth is usually present. This water table is commonly the result of low or very low saturated hydraulic conductivity of nearly continuous rainfall, or of a combination of these. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"osddrainagecl","ColumnLogicalName":"osd_drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"very poorly","ChoiceLabel":"Very poorly drained","ChoiceObsolete":0,"ChoiceDescription":"Water is removed from the soil so slowly that free water remains at or very near the ground surface during much of the growing season. The occurrence of internal free water is very shallow and persistent or permanent. Unless the soil is artificially drained, most mesophytic crops cannot be grown. The soils are commonly level or depressed and frequently ponded. If rainfall is high or nearly continuous, slope gradients may be greater. Soil Survey Manual, Chapter 3.","ColumnPhysicalName":"osddrainagecl","ColumnLogicalName":"osd_drainage_class"} {"DomainID":148,"DomainName":"drainage_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"subaqueous","ChoiceLabel":"Subaqueous","ChoiceObsolete":0,"ChoiceDescription":"Free water is above the soil surface. The occurrence of internal free water is permanent and there is a positive water potential at the soil surface for more than 21 hours of each day. 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Compare - `a`a lava, pahoehoe lava, pillow lava.","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":127,"ChoiceValue":162,"ChoiceName":"pillow lava","ChoiceLabel":"Pillow lava fragments","ChoiceObsolete":0,"ChoiceDescription":"A general term for lava displaying pillow structure (discontinuous, close-fitting, bun-shaped or ellipsoidal masses, generally < 1 m in diameter); considered to have formed in a subaqueous environment; such lava is usually basaltic or andesitic. 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It has a harsh, rough feel and is used to polish metals and stones.","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":49,"ChoiceValue":169,"ChoiceName":"gneiss, hornblende","ChoiceLabel":"Hornblende gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":100,"ChoiceValue":170,"ChoiceName":"metasiltstone","ChoiceLabel":"Metasiltstone fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":50,"ChoiceValue":171,"ChoiceName":"gneiss, migmatitic","ChoiceLabel":"Migmatitic gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":51,"ChoiceValue":172,"ChoiceName":"gneiss, muscovite-biotite","ChoiceLabel":"Muscovite-biotite gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":149,"ChoiceValue":173,"ChoiceName":"schist, graphitic","ChoiceLabel":"Graphitic schist fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":170,"ChoiceValue":174,"ChoiceName":"slate, sulfidic","ChoiceLabel":"Sulfidic slate fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":47,"ChoiceValue":175,"ChoiceName":"gneiss, biotite","ChoiceLabel":"Biotite gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":48,"ChoiceValue":176,"ChoiceName":"gneiss, granodioritic","ChoiceLabel":"Granodioritic gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":55,"ChoiceValue":177,"ChoiceName":"granitoid","ChoiceLabel":"Granitoid fragments","ChoiceObsolete":0,"ChoiceDescription":"a) In the IUGS classification, a preliminary term for (for field use) for a plutonic rock with Q (quartz) between 20 and 40 (%). b) A general term for all phaneritic igneous rocks (mineral crystals visible unaided and all about the same size) dominated by quartz and feldspars.","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":178,"ChoiceName":"bauxite","ChoiceLabel":"Bauxite fragments","ChoiceObsolete":0,"ChoiceDescription":"An off-white to dark red brown weathered detritus or rock composed of aluminum oxides (mainly gibbsite with some boehmite and diaspore), iron hydroxides, silica, silt, and especially clay minerals. Bauxite originates in tropical and subtropical environments as highly weathered residue from carbonate or silicate rocks and can occur in concretionary, earthy, pisolitic or oolitic forms. SW & GG","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":84,"ChoiceValue":179,"ChoiceName":"limestone, coral","ChoiceLabel":"Coral limestone fragments","ChoiceObsolete":0,"ChoiceDescription":"An informal term for massive limestone composed primarily of coral and coral fragments commonly associated with marine islands or coral reefs in tropical or subtropical waters. Compare - coral island. SW","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":180,"ChoiceName":"anhydrite, rock","ChoiceLabel":"Rock anhydrite fragments","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed chiefly of mineral anhydrite (anhydrous CaSO4); The rock is generally massive, cryptocrystalline, and may exhibit rhythmic sedimentation (rhymites). Compare - rock gypsum, rock halite. SW","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":63,"ChoiceValue":181,"ChoiceName":"halite, rock","ChoiceLabel":"Rock halite fragments","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed primarily of halite (NaCl). SW","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":80,"ChoiceValue":182,"ChoiceName":"lignite","ChoiceLabel":"Lignite fragments","ChoiceObsolete":0,"ChoiceDescription":"A brownish-black carbon-rich deposit that is a metamorphic intermediate between peat and sub-bituminous coal . Dry lignite typically contains 60-70 % carbon. SW & GG","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":115,"ChoiceValue":183,"ChoiceName":"novaculite","ChoiceLabel":"Novaculite","ChoiceObsolete":0,"ChoiceDescription":"A dense, extremely finely grained, even-textured, siliceous, sedimentary rock similar to chert. It is hard, white to grayish-black in color, translucent on thin edges, has a dull to waxy luster, and displays smooth conchoidal fracture when broken. \r\n\r\nNovaculite principally occurs in the Marathon Uplift of Texas and Ouachita Mountains of Arkansas and Oklahoma where it forms erosion resistant ridges. Novaculite appears to form from chert recrystallization with microcrystalline quartz dominant over cryptocrystalline chalcedony. At the Ouachita Mountains type occurrence, novaculite formed by low-grade, thermal metamorphism of bedded chert. Novaculite is commercially quarried as a whetstone or oilstone. Compare - chert. GG & SW","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":165,"ChoiceValue":184,"ChoiceName":"siltite","ChoiceLabel":"Siltite fragments","ChoiceObsolete":0,"ChoiceDescription":"A compact, weakly metamorphosed rock formed by alteration of siltstone, mudstone, or silty shale. Siltite is more indurated than mudstone or shale and lacks either shale fissility or slate-like cleavage. Siltite differs from argillite in that silt-size grains (0.002 to 0.062 mm) rather than clay-size (<0.002 mm) dominate the matrix. Siltite differs from siltstone, mudstone, or shale in that it exhibits very low to low grade metamorphic or diagenetic layer silicate and feldspar alteration to sericite, chlorite, and albite (subgreenschist to greenschist metamorphic facies) (Maxwell, 1973; Kidder, 1987).","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":148,"ChoiceValue":185,"ChoiceName":"schist, biotite","ChoiceLabel":"Biotite schist fragments","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily biotite.","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":151,"ChoiceValue":186,"ChoiceName":"schist, muscovite","ChoiceLabel":"Muscovite schist fragments","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily muscovite.","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":102,"ChoiceValue":187,"ChoiceName":"mica","ChoiceLabel":"Mica fragments","ChoiceObsolete":0,"ChoiceDescription":"A group of monoclinic phyllosilicate minerals with perfect basal cleavage that splits into thin elastic laminae and range from colorless to black. Large crystals of mica are referred to as a mica book.","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":91,"ChoiceValue":188,"ChoiceName":"limonite","ChoiceLabel":"Limonite","ChoiceObsolete":0,"ChoiceDescription":"A general 'field' term for various brown to yellowish brown, amorphous- to- cryptocrystalline hydrous ferric oxides that are an undetermined mixture of goethite, hematite, and lepidocrocite formed by weathering and iron oxidation from iron-bearing, rocks and minerals. SW & GG","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":152,"ChoiceValue":189,"ChoiceName":"schist, sericite","ChoiceLabel":"Sericite schist","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily sericite. A fine-grained muscovite","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":61,"ChoiceValue":190,"ChoiceName":"gypsum crystals","ChoiceLabel":"Gypsum crystal fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":41,"ChoiceValue":191,"ChoiceName":"fanglomerate","ChoiceLabel":"Fanglomerate fragments","ChoiceObsolete":0,"ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":34,"ChoiceValue":192,"ChoiceName":"diatomite fragments","ChoiceLabel":"Diatomite fragments","ChoiceObsolete":0,"ChoiceDescription":"A light-colored, soft, siliceous sedimentary rock (generally consolidated) consisting chiefly of opaline diatom frustules deposited in a lacustrine or marine environment. Diatomite has a number of uses owing to its high surface area, absorptive capacity, and relative chemical stability but the term is generally reserved for deposits of actual or potential commercial value.","ColumnPhysicalName":"fragkind","ColumnLogicalName":"fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":142,"ChoiceValue":1,"ChoiceName":"sandstone, unspecified","ChoiceLabel":"Sandstone fragments","ChoiceObsolete":0,"ChoiceDescription":"Sedimentary rock containing dominantly sand-size clastic particles.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":141,"ChoiceValue":2,"ChoiceName":"sandstone, noncalcareous","ChoiceLabel":"Noncalcareous sandstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":3,"ChoiceName":"arkose","ChoiceLabel":"Arkose fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":139,"ChoiceValue":4,"ChoiceName":"sandstone, calcareous","ChoiceLabel":"Calcareous sandstone fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":74,"ChoiceValue":5,"ChoiceName":"interbedded sedimentary","ChoiceLabel":"Interbedded sedimentary rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":88,"ChoiceValue":6,"ChoiceName":"limestone-sandstone-shale","ChoiceLabel":"Limestone-sandstone-shale fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":87,"ChoiceValue":7,"ChoiceName":"limestone-sandstone","ChoiceLabel":"Limestone-sandstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":89,"ChoiceValue":8,"ChoiceName":"limestone-shale","ChoiceLabel":"Limestone-shale fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":90,"ChoiceValue":9,"ChoiceName":"limestone-siltstone","ChoiceLabel":"Limestone-siltstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":143,"ChoiceValue":10,"ChoiceName":"sandstone-shale","ChoiceLabel":"Sandstone and shale fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":144,"ChoiceValue":11,"ChoiceName":"sandstone-siltstone","ChoiceLabel":"Sandstone and siltstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":162,"ChoiceValue":12,"ChoiceName":"shale-siltstone","ChoiceLabel":"Shale-siltstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":31,"ChoiceValue":13,"ChoiceName":"conglomerate, unspecified","ChoiceLabel":"Conglomerate fragments","ChoiceObsolete":0,"ChoiceDescription":"A coarse-grained, clastic sedimentary rock composed of rounded to subangular rock fragments larger than 2 mm, commonly with a matrix of sand and finer material; cements include silica, calcium carbonate, and iron oxides. The consolidated equivalent of gravel.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":30,"ChoiceValue":14,"ChoiceName":"conglomerate, noncalcareous","ChoiceLabel":"Noncalcareous conglomerate fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":15,"ChoiceName":"conglomerate, calcareous","ChoiceLabel":"Calcareous conglomerate fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":40,"ChoiceValue":16,"ChoiceName":"ejecta-ash","ChoiceLabel":"Ejecta-ash","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":17,"ChoiceName":"acidic-ash","ChoiceLabel":"Acidic-ash","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":18,"ChoiceName":"basic-ash","ChoiceLabel":"Basic-ash","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":19,"ChoiceName":"basaltic-ash","ChoiceLabel":"Basaltic-ash","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":20,"ChoiceName":"andesitic-ash","ChoiceLabel":"Andesitic-ash","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":21,"ChoiceName":"cinders","ChoiceLabel":"Cinders","ChoiceObsolete":0,"ChoiceDescription":"Uncemented vitric, vesicular, pyroclastic material, more than 2.0 mm in at least one dimension, with an apparent specific gravity (including vesicles) of more than 1.0 and less than 2.0. Compare - ash [volcanic], block [volcanic], lapilli, tephra.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":130,"ChoiceValue":22,"ChoiceName":"pumice","ChoiceLabel":"Pumice fragments","ChoiceObsolete":0,"ChoiceDescription":"A light-colored, vesicular, glassy rock commonly having the composition of rhyolite. It commonly has a specific gravity of < 1.0 and is thereby sufficiently buoyant to float on water.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":154,"ChoiceValue":23,"ChoiceName":"scoria","ChoiceLabel":"Scoria fragments","ChoiceObsolete":0,"ChoiceDescription":"Vesicular, cindery crust or bomb-sized fragments of such material on the surface of andesitic or basaltic lava, the vesicular nature of which is due to the escape of volcanic gases before solidification; it is usually heavier, darker, and more crystalline than pumice. Synonym - cinder.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":186,"ChoiceValue":24,"ChoiceName":"volcanic bombs","ChoiceLabel":"Volcanic bombs","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":161,"ChoiceValue":25,"ChoiceName":"shale, unspecified","ChoiceLabel":"Shale fragments","ChoiceObsolete":0,"ChoiceDescription":"Sedimentary rock formed by induration of a clay, silty clay, or silty clay loam deposit and having the tendency to split into thin layers, i.e., fissility.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":160,"ChoiceValue":26,"ChoiceName":"shale, noncalcareous","ChoiceLabel":"Noncalcareous shale fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":158,"ChoiceValue":27,"ChoiceName":"shale, calcareous","ChoiceLabel":"Calcareous shale fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":159,"ChoiceValue":28,"ChoiceName":"shale, clayey","ChoiceLabel":"Clayey shale fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":72,"ChoiceValue":29,"ChoiceName":"igneous, unspecified","ChoiceLabel":"Igneous rock fragments","ChoiceObsolete":0,"ChoiceDescription":"Rock formed by solidification from a molten or partially molten state; major varieties include plutonic and volcanic rocks. Examples: andesite, basalt, granite. Compare - intrusive, extrusive.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":68,"ChoiceValue":30,"ChoiceName":"igneous, coarse crystal","ChoiceLabel":"Coarse crystal igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":67,"ChoiceValue":31,"ChoiceName":"igneous, basic","ChoiceLabel":"Basic igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":70,"ChoiceValue":32,"ChoiceName":"igneous, intermediate","ChoiceLabel":"Intermediate igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":54,"ChoiceValue":33,"ChoiceName":"granite","ChoiceLabel":"Granite fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":69,"ChoiceValue":34,"ChoiceName":"igneous, fine crystal","ChoiceLabel":"Fine crystal igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":35,"ChoiceName":"basalt","ChoiceLabel":"Basalt fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":36,"ChoiceName":"andesite","ChoiceLabel":"Andesite fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":66,"ChoiceValue":37,"ChoiceName":"igneous, acid","ChoiceLabel":"Acid igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":71,"ChoiceValue":38,"ChoiceName":"igneous, ultrabasic","ChoiceLabel":"Ultrabasic igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":86,"ChoiceValue":39,"ChoiceName":"limestone, unspecified","ChoiceLabel":"Limestone fragments","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock consisting chiefly (more than 50 percent) of calcium carbonate, primarily in the form of calcite. 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Nearly all such rocks are crystalline. 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{"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":96,"ChoiceValue":160,"ChoiceName":"metamorphic, foliated","ChoiceLabel":"Foliated metamorphic rock fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":161,"ChoiceName":"block lava","ChoiceLabel":"Block lava fragments","ChoiceObsolete":0,"ChoiceDescription":"Lava having a surface of angular blocks; it is similar to `a`a lava but the fragments are larger and more regular in shape, somewhat smoother, and less vesicular. 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Bauxite originates in tropical and subtropical environments as highly weathered residue from carbonate or silicate rocks and can occur in concretionary, earthy, pisolitic or oolitic forms. SW & GG","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":84,"ChoiceValue":179,"ChoiceName":"limestone, coral","ChoiceLabel":"Coral limestone fragments","ChoiceObsolete":0,"ChoiceDescription":"An informal term for massive limestone composed primarily of coral and coral fragments commonly associated with marine islands or coral reefs in tropical or subtropical waters. Compare - coral island. 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Siltite differs from siltstone, mudstone, or shale in that it exhibits very low to low grade metamorphic or diagenetic layer silicate and feldspar alteration to sericite, chlorite, and albite (subgreenschist to greenschist metamorphic facies) (Maxwell, 1973; Kidder, 1987).","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":148,"ChoiceValue":185,"ChoiceName":"schist, biotite","ChoiceLabel":"Biotite schist fragments","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily biotite.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":151,"ChoiceValue":186,"ChoiceName":"schist, muscovite","ChoiceLabel":"Muscovite schist fragments","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily muscovite.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":102,"ChoiceValue":187,"ChoiceName":"mica","ChoiceLabel":"Mica fragments","ChoiceObsolete":0,"ChoiceDescription":"A group of monoclinic phyllosilicate minerals with perfect basal cleavage that splits into thin elastic laminae and range from colorless to black. Large crystals of mica are referred to as a mica book.","ColumnPhysicalName":"osdfragkind","ColumnLogicalName":"osd_fragment_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":91,"ChoiceValue":188,"ChoiceName":"limonite","ChoiceLabel":"Limonite","ChoiceObsolete":0,"ChoiceDescription":"A general 'field' term for various brown to yellowish brown, amorphous- to- cryptocrystalline hydrous ferric oxides that are an undetermined mixture of goethite, hematite, and lepidocrocite formed by weathering and iron oxidation from iron-bearing, rocks and minerals. 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It has a harsh, rough feel and is used to polish metals and stones.","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":49,"ChoiceValue":169,"ChoiceName":"gneiss, hornblende","ChoiceLabel":"Hornblende gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":100,"ChoiceValue":170,"ChoiceName":"metasiltstone","ChoiceLabel":"Metasiltstone fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":50,"ChoiceValue":171,"ChoiceName":"gneiss, migmatitic","ChoiceLabel":"Migmatitic gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":51,"ChoiceValue":172,"ChoiceName":"gneiss, muscovite-biotite","ChoiceLabel":"Muscovite-biotite gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":149,"ChoiceValue":173,"ChoiceName":"schist, graphitic","ChoiceLabel":"Graphitic schist fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":170,"ChoiceValue":174,"ChoiceName":"slate, sulfidic","ChoiceLabel":"Sulfidic slate fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":47,"ChoiceValue":175,"ChoiceName":"gneiss, biotite","ChoiceLabel":"Biotite gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":48,"ChoiceValue":176,"ChoiceName":"gneiss, granodioritic","ChoiceLabel":"Granodioritic gneiss fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":55,"ChoiceValue":177,"ChoiceName":"granitoid","ChoiceLabel":"Granitoid fragments","ChoiceObsolete":0,"ChoiceDescription":"a) In the IUGS classification, a preliminary term for (for field use) for a plutonic rock with Q (quartz) between 20 and 40 (%). b) A general term for all phaneritic igneous rocks (mineral crystals visible unaided and all about the same size) dominated by quartz and feldspars.","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":178,"ChoiceName":"bauxite","ChoiceLabel":"Bauxite fragments","ChoiceObsolete":0,"ChoiceDescription":"An off-white to dark red brown weathered detritus or rock composed of aluminum oxides (mainly gibbsite with some boehmite and diaspore), iron hydroxides, silica, silt, and especially clay minerals. Bauxite originates in tropical and subtropical environments as highly weathered residue from carbonate or silicate rocks and can occur in concretionary, earthy, pisolitic or oolitic forms. SW & GG","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":84,"ChoiceValue":179,"ChoiceName":"limestone, coral","ChoiceLabel":"Coral limestone fragments","ChoiceObsolete":0,"ChoiceDescription":"An informal term for massive limestone composed primarily of coral and coral fragments commonly associated with marine islands or coral reefs in tropical or subtropical waters. Compare - coral island. SW","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":180,"ChoiceName":"anhydrite, rock","ChoiceLabel":"Rock anhydrite fragments","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed chiefly of mineral anhydrite (anhydrous CaSO4); The rock is generally massive, cryptocrystalline, and may exhibit rhythmic sedimentation (rhymites). Compare - rock gypsum, rock halite. SW","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":63,"ChoiceValue":181,"ChoiceName":"halite, rock","ChoiceLabel":"Rock halite fragments","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed primarily of halite (NaCl). SW","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":80,"ChoiceValue":182,"ChoiceName":"lignite","ChoiceLabel":"Lignite fragments","ChoiceObsolete":0,"ChoiceDescription":"A brownish-black carbon-rich deposit that is a metamorphic intermediate between peat and sub-bituminous coal . Dry lignite typically contains 60-70 % carbon. SW & GG","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":115,"ChoiceValue":183,"ChoiceName":"novaculite","ChoiceLabel":"Novaculite","ChoiceObsolete":0,"ChoiceDescription":"A dense, extremely finely grained, even-textured, siliceous, sedimentary rock similar to chert. It is hard, white to grayish-black in color, translucent on thin edges, has a dull to waxy luster, and displays smooth conchoidal fracture when broken. \r\n\r\nNovaculite principally occurs in the Marathon Uplift of Texas and Ouachita Mountains of Arkansas and Oklahoma where it forms erosion resistant ridges. Novaculite appears to form from chert recrystallization with microcrystalline quartz dominant over cryptocrystalline chalcedony. At the Ouachita Mountains type occurrence, novaculite formed by low-grade, thermal metamorphism of bedded chert. Novaculite is commercially quarried as a whetstone or oilstone. Compare - chert. GG & SW","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":165,"ChoiceValue":184,"ChoiceName":"siltite","ChoiceLabel":"Siltite fragments","ChoiceObsolete":0,"ChoiceDescription":"A compact, weakly metamorphosed rock formed by alteration of siltstone, mudstone, or silty shale. Siltite is more indurated than mudstone or shale and lacks either shale fissility or slate-like cleavage. Siltite differs from argillite in that silt-size grains (0.002 to 0.062 mm) rather than clay-size (<0.002 mm) dominate the matrix. Siltite differs from siltstone, mudstone, or shale in that it exhibits very low to low grade metamorphic or diagenetic layer silicate and feldspar alteration to sericite, chlorite, and albite (subgreenschist to greenschist metamorphic facies) (Maxwell, 1973; Kidder, 1987).","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":148,"ChoiceValue":185,"ChoiceName":"schist, biotite","ChoiceLabel":"Biotite schist fragments","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily biotite.","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":151,"ChoiceValue":186,"ChoiceName":"schist, muscovite","ChoiceLabel":"Muscovite schist fragments","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily muscovite.","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":102,"ChoiceValue":187,"ChoiceName":"mica","ChoiceLabel":"Mica fragments","ChoiceObsolete":0,"ChoiceDescription":"A group of monoclinic phyllosilicate minerals with perfect basal cleavage that splits into thin elastic laminae and range from colorless to black. Large crystals of mica are referred to as a mica book.","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":91,"ChoiceValue":188,"ChoiceName":"limonite","ChoiceLabel":"Limonite","ChoiceObsolete":0,"ChoiceDescription":"A general 'field' term for various brown to yellowish brown, amorphous- to- cryptocrystalline hydrous ferric oxides that are an undetermined mixture of goethite, hematite, and lepidocrocite formed by weathering and iron oxidation from iron-bearing, rocks and minerals. SW & GG","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":152,"ChoiceValue":189,"ChoiceName":"schist, sericite","ChoiceLabel":"Sericite schist","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily sericite. A fine-grained muscovite","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":61,"ChoiceValue":190,"ChoiceName":"gypsum crystals","ChoiceLabel":"Gypsum crystal fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":41,"ChoiceValue":191,"ChoiceName":"fanglomerate","ChoiceLabel":"Fanglomerate fragments","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":34,"ChoiceValue":192,"ChoiceName":"diatomite fragments","ChoiceLabel":"Diatomite fragments","ChoiceObsolete":0,"ChoiceDescription":"A light-colored, soft, siliceous sedimentary rock (generally consolidated) consisting chiefly of opaline diatom frustules deposited in a lacustrine or marine environment. Diatomite has a number of uses owing to its high surface area, absorptive capacity, and relative chemical stability but the term is generally reserved for deposits of actual or potential commercial value.","ColumnPhysicalName":"osdsfragkind","ColumnLogicalName":"osd_surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":142,"ChoiceValue":1,"ChoiceName":"sandstone, unspecified","ChoiceLabel":"Sandstone fragments","ChoiceObsolete":0,"ChoiceDescription":"Sedimentary rock containing dominantly sand-size clastic particles.","ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":141,"ChoiceValue":2,"ChoiceName":"sandstone, noncalcareous","ChoiceLabel":"Noncalcareous sandstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":3,"ChoiceName":"arkose","ChoiceLabel":"Arkose fragments","ChoiceObsolete":0,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":139,"ChoiceValue":4,"ChoiceName":"sandstone, calcareous","ChoiceLabel":"Calcareous sandstone fragments","ChoiceObsolete":0,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":74,"ChoiceValue":5,"ChoiceName":"interbedded sedimentary","ChoiceLabel":"Interbedded sedimentary rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":88,"ChoiceValue":6,"ChoiceName":"limestone-sandstone-shale","ChoiceLabel":"Limestone-sandstone-shale fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":87,"ChoiceValue":7,"ChoiceName":"limestone-sandstone","ChoiceLabel":"Limestone-sandstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":89,"ChoiceValue":8,"ChoiceName":"limestone-shale","ChoiceLabel":"Limestone-shale fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":90,"ChoiceValue":9,"ChoiceName":"limestone-siltstone","ChoiceLabel":"Limestone-siltstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":143,"ChoiceValue":10,"ChoiceName":"sandstone-shale","ChoiceLabel":"Sandstone and shale fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":144,"ChoiceValue":11,"ChoiceName":"sandstone-siltstone","ChoiceLabel":"Sandstone and siltstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":162,"ChoiceValue":12,"ChoiceName":"shale-siltstone","ChoiceLabel":"Shale-siltstone fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":31,"ChoiceValue":13,"ChoiceName":"conglomerate, unspecified","ChoiceLabel":"Conglomerate fragments","ChoiceObsolete":0,"ChoiceDescription":"A coarse-grained, clastic sedimentary rock composed of rounded to subangular rock fragments larger than 2 mm, commonly with a matrix of sand and finer material; cements include silica, calcium carbonate, and iron oxides. The consolidated equivalent of gravel.","ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":30,"ChoiceValue":14,"ChoiceName":"conglomerate, noncalcareous","ChoiceLabel":"Noncalcareous conglomerate fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":15,"ChoiceName":"conglomerate, calcareous","ChoiceLabel":"Calcareous conglomerate fragments","ChoiceObsolete":0,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":40,"ChoiceValue":16,"ChoiceName":"ejecta-ash","ChoiceLabel":"Ejecta-ash","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":17,"ChoiceName":"acidic-ash","ChoiceLabel":"Acidic-ash","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":18,"ChoiceName":"basic-ash","ChoiceLabel":"Basic-ash","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":19,"ChoiceName":"basaltic-ash","ChoiceLabel":"Basaltic-ash","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":20,"ChoiceName":"andesitic-ash","ChoiceLabel":"Andesitic-ash","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":21,"ChoiceName":"cinders","ChoiceLabel":"Cinders","ChoiceObsolete":0,"ChoiceDescription":"Uncemented vitric, vesicular, pyroclastic material, more than 2.0 mm in at least one dimension, with an apparent specific gravity (including vesicles) of more than 1.0 and less than 2.0. Compare - ash [volcanic], block [volcanic], lapilli, tephra.","ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":130,"ChoiceValue":22,"ChoiceName":"pumice","ChoiceLabel":"Pumice fragments","ChoiceObsolete":0,"ChoiceDescription":"A light-colored, vesicular, glassy rock commonly having the composition of rhyolite. It commonly has a specific gravity of < 1.0 and is thereby sufficiently buoyant to float on water.","ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":154,"ChoiceValue":23,"ChoiceName":"scoria","ChoiceLabel":"Scoria fragments","ChoiceObsolete":0,"ChoiceDescription":"Vesicular, cindery crust or bomb-sized fragments of such material on the surface of andesitic or basaltic lava, the vesicular nature of which is due to the escape of volcanic gases before solidification; it is usually heavier, darker, and more crystalline than pumice. Synonym - cinder.","ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":186,"ChoiceValue":24,"ChoiceName":"volcanic bombs","ChoiceLabel":"Volcanic bombs","ChoiceObsolete":0,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":161,"ChoiceValue":25,"ChoiceName":"shale, unspecified","ChoiceLabel":"Shale fragments","ChoiceObsolete":0,"ChoiceDescription":"Sedimentary rock formed by induration of a clay, silty clay, or silty clay loam deposit and having the tendency to split into thin layers, i.e., fissility.","ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":160,"ChoiceValue":26,"ChoiceName":"shale, noncalcareous","ChoiceLabel":"Noncalcareous shale fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":158,"ChoiceValue":27,"ChoiceName":"shale, calcareous","ChoiceLabel":"Calcareous shale fragments","ChoiceObsolete":0,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":159,"ChoiceValue":28,"ChoiceName":"shale, clayey","ChoiceLabel":"Clayey shale fragments","ChoiceObsolete":0,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":72,"ChoiceValue":29,"ChoiceName":"igneous, unspecified","ChoiceLabel":"Igneous rock fragments","ChoiceObsolete":0,"ChoiceDescription":"Rock formed by solidification from a molten or partially molten state; major varieties include plutonic and volcanic rocks. Examples: andesite, basalt, granite. Compare - intrusive, extrusive.","ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":68,"ChoiceValue":30,"ChoiceName":"igneous, coarse crystal","ChoiceLabel":"Coarse crystal igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":67,"ChoiceValue":31,"ChoiceName":"igneous, basic","ChoiceLabel":"Basic igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":70,"ChoiceValue":32,"ChoiceName":"igneous, intermediate","ChoiceLabel":"Intermediate igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":54,"ChoiceValue":33,"ChoiceName":"granite","ChoiceLabel":"Granite fragments","ChoiceObsolete":0,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":69,"ChoiceValue":34,"ChoiceName":"igneous, fine crystal","ChoiceLabel":"Fine crystal igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":35,"ChoiceName":"basalt","ChoiceLabel":"Basalt fragments","ChoiceObsolete":0,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":36,"ChoiceName":"andesite","ChoiceLabel":"Andesite fragments","ChoiceObsolete":0,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":66,"ChoiceValue":37,"ChoiceName":"igneous, acid","ChoiceLabel":"Acid igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":71,"ChoiceValue":38,"ChoiceName":"igneous, ultrabasic","ChoiceLabel":"Ultrabasic igneous rock fragments","ChoiceObsolete":1,"ColumnPhysicalName":"sfragkind","ColumnLogicalName":"surface_frag_kind"} {"DomainID":152,"DomainName":"fragment_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":86,"ChoiceValue":39,"ChoiceName":"limestone, unspecified","ChoiceLabel":"Limestone fragments","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock consisting chiefly (more than 50 percent) of calcium carbonate, primarily in the form of calcite. 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{"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":1,"ChoiceName":"angular","ChoiceLabel":"Angular","ChoiceObsolete":0,"ChoiceDescription":"Strongly developed faces with sharp edges (SSM).","ColumnPhysicalName":"osdhuartrnd","ColumnLogicalName":"osd_human_artifact_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":2,"ChoiceName":"subangular","ChoiceLabel":"Subangular","ChoiceObsolete":0,"ChoiceDescription":"Detectable flat faces with slightly-rounded corners.","ColumnPhysicalName":"osdhuartrnd","ColumnLogicalName":"osd_human_artifact_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":3,"ChoiceName":"subrounded","ChoiceLabel":"Subrounded","ChoiceObsolete":0,"ChoiceDescription":"Detectable flat faces with well-rounded corners (SSM).","ColumnPhysicalName":"osdhuartrnd","ColumnLogicalName":"osd_human_artifact_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":4,"ChoiceName":"rounded","ChoiceLabel":"Rounded","ChoiceObsolete":0,"ChoiceDescription":"Flat faces absent or nearly absent with all corners rounded (SSM).","ColumnPhysicalName":"osdhuartrnd","ColumnLogicalName":"osd_human_artifact_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":5,"ChoiceName":"well rounded","ChoiceLabel":"Well rounded","ChoiceObsolete":0,"ChoiceDescription":"Flat faces absent with all corners rounded.","ColumnPhysicalName":"osdhuartrnd","ColumnLogicalName":"osd_human_artifact_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":6,"ChoiceName":"very angular","ChoiceLabel":"Very angular","ChoiceObsolete":0,"ChoiceDescription":"Strongly developed faces with very sharp, broken edges.","ColumnPhysicalName":"osdhuartrnd","ColumnLogicalName":"osd_human_artifact_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":1,"ChoiceName":"angular","ChoiceLabel":"Angular","ChoiceObsolete":0,"ChoiceDescription":"Strongly developed faces with sharp edges (SSM).","ColumnPhysicalName":"osdsfraground","ColumnLogicalName":"osd_surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":2,"ChoiceName":"subangular","ChoiceLabel":"Subangular","ChoiceObsolete":0,"ChoiceDescription":"Detectable flat faces with slightly-rounded corners.","ColumnPhysicalName":"osdsfraground","ColumnLogicalName":"osd_surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":3,"ChoiceName":"subrounded","ChoiceLabel":"Subrounded","ChoiceObsolete":0,"ChoiceDescription":"Detectable flat faces with well-rounded corners (SSM).","ColumnPhysicalName":"osdsfraground","ColumnLogicalName":"osd_surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":4,"ChoiceName":"rounded","ChoiceLabel":"Rounded","ChoiceObsolete":0,"ChoiceDescription":"Flat faces absent or nearly absent with all corners rounded (SSM).","ColumnPhysicalName":"osdsfraground","ColumnLogicalName":"osd_surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":5,"ChoiceName":"well rounded","ChoiceLabel":"Well rounded","ChoiceObsolete":0,"ChoiceDescription":"Flat faces absent with all corners rounded.","ColumnPhysicalName":"osdsfraground","ColumnLogicalName":"osd_surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":6,"ChoiceName":"very angular","ChoiceLabel":"Very angular","ChoiceObsolete":0,"ChoiceDescription":"Strongly developed faces with very sharp, broken edges.","ColumnPhysicalName":"osdsfraground","ColumnLogicalName":"osd_surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":1,"ChoiceName":"angular","ChoiceLabel":"Angular","ChoiceObsolete":0,"ChoiceDescription":"Strongly developed faces with sharp edges (SSM).","ColumnPhysicalName":"sfraground","ColumnLogicalName":"surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":2,"ChoiceName":"subangular","ChoiceLabel":"Subangular","ChoiceObsolete":0,"ChoiceDescription":"Detectable flat faces with slightly-rounded corners.","ColumnPhysicalName":"sfraground","ColumnLogicalName":"surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":3,"ChoiceName":"subrounded","ChoiceLabel":"Subrounded","ChoiceObsolete":0,"ChoiceDescription":"Detectable flat faces with well-rounded corners (SSM).","ColumnPhysicalName":"sfraground","ColumnLogicalName":"surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":4,"ChoiceName":"rounded","ChoiceLabel":"Rounded","ChoiceObsolete":0,"ChoiceDescription":"Flat faces absent or nearly absent with all corners rounded (SSM).","ColumnPhysicalName":"sfraground","ColumnLogicalName":"surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":5,"ChoiceName":"well rounded","ChoiceLabel":"Well rounded","ChoiceObsolete":0,"ChoiceDescription":"Flat faces absent with all corners rounded.","ColumnPhysicalName":"sfraground","ColumnLogicalName":"surface_frag_roundness"} {"DomainID":153,"DomainName":"fragment_roundness","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":6,"ChoiceName":"very angular","ChoiceLabel":"Very angular","ChoiceObsolete":0,"ChoiceDescription":"Strongly developed faces with very sharp, broken edges.","ColumnPhysicalName":"sfraground","ColumnLogicalName":"surface_frag_roundness"} {"DomainID":154,"DomainName":"fragment_shape","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"flat","ChoiceLabel":"Flat","ChoiceObsolete":0,"ColumnPhysicalName":"fragshp","ColumnLogicalName":"fragment_shape"} {"DomainID":154,"DomainName":"fragment_shape","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"nonflat","ChoiceLabel":"Nonflat","ChoiceObsolete":0,"ColumnPhysicalName":"fragshp","ColumnLogicalName":"fragment_shape"} {"DomainID":154,"DomainName":"fragment_shape","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"flat","ChoiceLabel":"Flat","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragshp","ColumnLogicalName":"osd_fragment_shape"} {"DomainID":154,"DomainName":"fragment_shape","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"nonflat","ChoiceLabel":"Nonflat","ChoiceObsolete":0,"ColumnPhysicalName":"osdfragshp","ColumnLogicalName":"osd_fragment_shape"} {"DomainID":154,"DomainName":"fragment_shape","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"flat","ChoiceLabel":"Flat","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragshp","ColumnLogicalName":"osd_surface_frag_shape"} {"DomainID":154,"DomainName":"fragment_shape","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"nonflat","ChoiceLabel":"Nonflat","ChoiceObsolete":0,"ColumnPhysicalName":"osdsfragshp","ColumnLogicalName":"osd_surface_frag_shape"} {"DomainID":154,"DomainName":"fragment_shape","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"flat","ChoiceLabel":"Flat","ChoiceObsolete":0,"ColumnPhysicalName":"sfragshp","ColumnLogicalName":"surface_frag_shape"} {"DomainID":154,"DomainName":"fragment_shape","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"nonflat","ChoiceLabel":"Nonflat","ChoiceObsolete":0,"ColumnPhysicalName":"sfragshp","ColumnLogicalName":"surface_frag_shape"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"a","ChoiceLabel":"a","ChoiceObsolete":0,"ChoiceDescription":"Highly decomposed organic matter. This symbol is used with O to indicate the most highly decomposed organic materials, which have a fiber content of less than 17 percent (by volume) after rubbing.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"b","ChoiceLabel":"b","ChoiceObsolete":0,"ChoiceDescription":"Buried genetic horizon. This symbol is used in mineral soils to indicate identifiable buried horizons with major genetic features that were developed before burial. Genetic horizons may or may not have formed in the overlying material, which may be either like or unlike the assumed parent material of the buried soil. This symbol is not used in organic soils, nor is it used to separate an organic layer from a mineral layer.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"c","ChoiceLabel":"c","ChoiceObsolete":0,"ChoiceDescription":"Concretions or nodules. This symbol indicates a significant accumulation of concretions or nodules. Cementation is required. The cementing agent commonly is iron, aluminum, manganese, or titanium. It cannot be silica, dolomite, calcite, or more soluble salts.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":4,"ChoiceName":"d","ChoiceLabel":"d","ChoiceObsolete":0,"ChoiceDescription":"Physical root restriction. This symbol indicates noncemented, root-restricting layers in naturally occurring or human-made sediments or materials. Examples are dense basal till, plowpans, and other mechanically compacted zones.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":5,"ChoiceName":"e","ChoiceLabel":"e","ChoiceObsolete":0,"ChoiceDescription":"Organic material of intermediate decomposition. This symbol is used with O to indicate organic materials of intermediate decomposition. The fiber content of these materials is 17 to 40 percent (by volume) after rubbing.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":6,"ChoiceName":"f","ChoiceLabel":"f","ChoiceObsolete":0,"ChoiceDescription":"Frozen soil or water. This symbol indicates that a horizon or layer contains permanent ice. The symbol is not used for seasonally frozen layers or for dry permafrost.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":7,"ChoiceName":"g","ChoiceLabel":"g","ChoiceObsolete":0,"ChoiceDescription":"Strong gleying. This symbol indicates either that iron has been reduced and removed during soil formation or that saturation with stagnant water has preserved it in a reduced state. Most of the affected layers have chroma of 2 or less, and many have redox concentrations. The low chroma can represent either the color of reduced iron or the color of uncoated sand and silt particles from which iron has been removed. The symbol g is not used for materials of low chroma that have no history of wetness, such as some shales or E horizons. If g is used with B, pedogenic change in addition to gleying is implied. If no other pedogenic change besides gleying has taken place, the horizon is designated Cg.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":8,"ChoiceName":"h","ChoiceLabel":"h","ChoiceObsolete":0,"ChoiceDescription":"Illuvial accumulation of organic matter. This symbol is used with B to indicate the accumulation of illuvial, amorphous, dispersible complexes of organic matter and sesquioxides if the sesquioxide component is dominated by aluminum but is present only in very small quantities. The organo-sesquioxide material coats sand and silt particles. In some horizons these coatings have coalesced, filled pores, and cemented the horizon. The symbol h is also used in combination with s as \"Bhs\" if the amount of the sesquioxide component is significant but the color value and chroma, moist, of the horizon are 3 or less.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":9,"ChoiceName":"i","ChoiceLabel":"i","ChoiceObsolete":0,"ChoiceDescription":"Slightly decomposed organic material. This symbol is used with O to indicate the least decomposed of the organic materials. The fiber content of these materials is 40 percent or more (by volume) after rubbing.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":10,"ChoiceName":"k","ChoiceLabel":"k","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of secondary carbonates. This symbol indicates an accumulation of visible pedogenic calcium carbonate (less than 50 percent, by volume). Carbonate accumulations occur as carbonate filaments, coatings, masses, nodules, disseminated carbonate, or other forms.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":11,"ChoiceName":"m","ChoiceLabel":"m","ChoiceObsolete":0,"ChoiceDescription":"Cementation or induration. This symbol indicates continuous or nearly continuous cementation. It is used only for horizons that are more than 90 percent cemented, although they may be fractured. The cemented layer is physically root-restrictive. The predominant cementing agent (or the two dominant ones) may be indicated by adding defined letter suffixes, singly or in pairs. The horizon suffix kkm (and less commonly km) indicates cementation by carbonates; qm, cementation by silica; sm, cementation by iron; yym, cementation by gypsum; kqm, cementation by carbonates and silica; and zm, cementation by salts more soluble than gypsum.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":12,"ChoiceName":"n","ChoiceLabel":"n","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of sodium. This symbol indicates an accumulation of exchangeable sodium.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":13,"ChoiceName":"o","ChoiceLabel":"o","ChoiceObsolete":0,"ChoiceDescription":"This symbol indicates a residual accumulation of sesquioxides.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":14,"ChoiceName":"p","ChoiceLabel":"p","ChoiceObsolete":0,"ChoiceDescription":"Tillage or other disturbance. This symbol indicates a disturbance of the surface layer by mechanical means, pasturing, or similar uses. A disturbed organic horizon is designated Op. A disturbed mineral horizon is designated Ap even though it is clearly a former E, B, or C horizon.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":15,"ChoiceName":"q","ChoiceLabel":"q","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of silica. This symbol indicates an accumulation of secondary silica.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":16,"ChoiceName":"r","ChoiceLabel":"r","ChoiceObsolete":0,"ChoiceDescription":"Weathered or soft bedrock. This symbol is used with C to indicate layers of bedrock that are moderately cemented or less cemented. Examples are weathered igneous rock and partly consolidated sandstone, siltstone, or shale. The excavation difficulty is low to high.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":25,"ChoiceValue":17,"ChoiceName":"s","ChoiceLabel":"s","ChoiceObsolete":0,"ChoiceDescription":"Illuvial accumulation of sesquioxides and organic matter. This symbol is used with B to indicate an accumulation of illuvial, amorphous, dispersible complexes of organic matter and sesquioxides if both the organic matter and sesquioxide components are significant and if either the color value or chroma, moist, of the horizon is 4 or more. The symbol is also used in combination with h as \"Bhs\" if both the organic matter and sesquioxide components are significant and if the color value and chroma, moist, are 3 or less.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":27,"ChoiceValue":18,"ChoiceName":"ss","ChoiceLabel":"ss","ChoiceObsolete":0,"ChoiceDescription":"Presence of slickensides. This symbol indicates the presence of slickensides. Slickensides result directly from the swelling of clay minerals and shear failure, commonly at angles of 20 to 60 degrees above horizontal. They are indicators that other vertic characteristics, such as wedge-shaped peds and surface cracks, may be present.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":28,"ChoiceValue":19,"ChoiceName":"t","ChoiceLabel":"t","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of silicate clay. This symbol indicates an accumulation of silicate clay that has either formed and subsequently been translocated within the horizon or has been moved into the horizon by illuviation, or both. At least some part of the horizon should show evidence of clay accumulation either as coatings on surfaces of peds or in pores, or as lamellae or as bridges between mineral grains.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":30,"ChoiceValue":20,"ChoiceName":"v","ChoiceLabel":"v","ChoiceObsolete":0,"ChoiceDescription":"Plinthite. This symbol indicates the presence of iron-rich, humus-poor, reddish material that is firm or very firm when moist and is less than strongly cemented. It hardens irreversibly when exposed to the atmosphere and to repeated wetting and drying.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":31,"ChoiceValue":21,"ChoiceName":"w","ChoiceLabel":"w","ChoiceObsolete":0,"ChoiceDescription":"Development of color or structure. This symbol is used only with B to indicate the development of color or structure, or both, with little or no apparent illuvial accumulation of material. It should not be used to indicate a transitional horizon.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":32,"ChoiceValue":22,"ChoiceName":"x","ChoiceLabel":"x","ChoiceObsolete":0,"ChoiceDescription":"Fragipan character. This symbol indicates a genetically developed layer that has a combination of firmness, brittleness, and commonly a higher bulk density than adjacent layers. Some part of the layer is physically root-restrictive.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":33,"ChoiceValue":23,"ChoiceName":"y","ChoiceLabel":"y","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of gypsum. This symbol indicates a gypsum accumulation. The suffix y is used when the horizon fabric is dominated by soil particles or minerals other than gypsum. Gypsum is present in amounts that do not significantly obscure or disrupt other features of the horizon.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":35,"ChoiceValue":24,"ChoiceName":"z","ChoiceLabel":"z","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of salts more soluble than gypsum. This symbol indicates an accumulation of salts that are more soluble than gypsum.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":25,"ChoiceName":"j","ChoiceLabel":"j","ChoiceObsolete":0,"ChoiceDescription":"Indicates an accumulation of jarosite. Jarosite is a potassium (ferric) iron hydroxy sulfate mineral (KFe3(SO4)2(OH)6) that is commonly an alteration product of pyrite that has been exposed to an oxidizing environment. Jarosite has hue of 2.5Y or yellower and normally has chroma of 6 or more, although chroma as low as 3 or 4 have been reported. It forms in preference to iron (hydr)oxides in active acid sulfate soils at pH of 3.5 or less and can be stable in post-active acid sulfate soils for long periods of time at higher pH.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":26,"ChoiceName":"jj","ChoiceLabel":"jj","ChoiceObsolete":0,"ChoiceDescription":"Evidence of cyroturbation. Evidence of cryoturbation includes irregular and broken horizon boundaries, sorted rock fragments, and organic soil materials occurring as bodies and broken layers within and/or between mineral soil layers. The organic bodies and layers are most commonly at the contact between the active layer and the permafrost.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":27,"ChoiceName":"ff","ChoiceLabel":"ff","ChoiceObsolete":0,"ChoiceDescription":"Dry permafrost. Used in layers or horizons that are colder than 0 degrees C, but do not contain ice. It is not used for layers or horizons that have seasonal temperatures below 0 degrees C. The f suffix is used for layers or horizons that contain permanent ice.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":28,"ChoiceName":"ca","ChoiceLabel":"ca","ChoiceObsolete":1,"ChoiceDescription":"An accumulation of carbonates.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":29,"ChoiceName":"co","ChoiceLabel":"co","ChoiceObsolete":0,"ChoiceDescription":"Coprogenous Earth. This symbol, used only with L, indicates a limnic layer of coprogenous earth (or sedimentary peat).","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":30,"ChoiceName":"ma","ChoiceLabel":"ma","ChoiceObsolete":0,"ChoiceDescription":"Marl. This symbol, used only with L, indicates a limnic layer of marl.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":31,"ChoiceName":"di","ChoiceLabel":"di","ChoiceObsolete":0,"ChoiceDescription":"Diatomaceous earth. This symbol, used only with L, indicates a limnic layer of diatomaceous earth.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":32,"ChoiceName":"kk","ChoiceLabel":"kk","ChoiceObsolete":0,"ChoiceDescription":"Engulfment of horizon by secondary carbonates. This symbol indicates major accumulations of pedogenic calcium carbonate. The suffix kk is used when the soil fabric is plugged with fine grained pedogenic carbonate (50 percent or more, by volume) that occurs as an essentially continuous medium. The suffix corresponds to the stage III plugged horizon or higher of the carbonate morphogenetic stages (Gile et al., 1966).","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":33,"ChoiceName":"u","ChoiceLabel":"u","ChoiceObsolete":0,"ChoiceDescription":"Presence of human-manufactured materials (artifacts). This symbol indicates the presence of manufactured artifacts that have been created or modified by humans, usually for a practical purpose in habitation, manufacturing, excavation, or construction activities. Examples of artifacts are processed wood products, liquid petroleum products, coal combustion by-products, asphalt, fibers and fabrics, bricks, cinder blocks, concrete, plastic, glass, rubber, paper, cardboard, iron and steel, altered metals and minerals, sanitary and medical waste, garbage, and landfill waste.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":34,"ChoiceValue":34,"ChoiceName":"yy","ChoiceLabel":"yy","ChoiceObsolete":0,"ChoiceDescription":"Dominance of horizon by gypsum. This symbol indicates a horizon that is dominated by the presence of gypsum. The gypsum content may be due to an accumulation of secondary gypsum, the transformation of primary gypsum inherited from parent material, or other processes. Suffix yy is used when the horizon fabric has such an abundance of gypsum (generally 50 percent or more, by volume) that pedogenic and/or lithologic features are obscured or disrupted by growth of gypsum crystals. Colors associated with horizons that use suffix yy are typically highly whitened with value of 7 through 9.5 and chroma of 2 or less.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":35,"ChoiceName":"se","ChoiceLabel":"se","ChoiceObsolete":0,"ChoiceDescription":"This symbol indicates the presence of sulfides in mineral or organic horizons. Horizons with sulfides typically have dark colors (e.g. value 4, chroma 2). These horizons typically form in soils associated with coastal environments that are permanently saturated or submerged (i.e., tidal marshes or estuaries). Soil materials which have sulfidization actively occurring emanate hydrogen sulfide gas which is detectable by its odor (Fanning and Fanning, 1989, or Fanning et al., 2002). Sulfides may also occur in upland environments that have a source of sulfur to form sulfides. Soils in such environments are often of geologic origin and may not produce a hydrogen sulfide odor. Examples include soils formed in parent materials derived from coal deposits such as lignite or soils formed in coastal plain deposits such as glauconite that have not been oxidized because of thick layers of overburden.","ColumnPhysicalName":"desgnsuffix","ColumnLogicalName":"horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"a","ChoiceLabel":"a","ChoiceObsolete":0,"ChoiceDescription":"Highly decomposed organic matter. This symbol is used with O to indicate the most highly decomposed organic materials, which have a fiber content of less than 17 percent (by volume) after rubbing.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"b","ChoiceLabel":"b","ChoiceObsolete":0,"ChoiceDescription":"Buried genetic horizon. This symbol is used in mineral soils to indicate identifiable buried horizons with major genetic features that were developed before burial. Genetic horizons may or may not have formed in the overlying material, which may be either like or unlike the assumed parent material of the buried soil. This symbol is not used in organic soils, nor is it used to separate an organic layer from a mineral layer.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"c","ChoiceLabel":"c","ChoiceObsolete":0,"ChoiceDescription":"Concretions or nodules. This symbol indicates a significant accumulation of concretions or nodules. Cementation is required. The cementing agent commonly is iron, aluminum, manganese, or titanium. It cannot be silica, dolomite, calcite, or more soluble salts.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":4,"ChoiceName":"d","ChoiceLabel":"d","ChoiceObsolete":0,"ChoiceDescription":"Physical root restriction. This symbol indicates noncemented, root-restricting layers in naturally occurring or human-made sediments or materials. Examples are dense basal till, plowpans, and other mechanically compacted zones.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":5,"ChoiceName":"e","ChoiceLabel":"e","ChoiceObsolete":0,"ChoiceDescription":"Organic material of intermediate decomposition. This symbol is used with O to indicate organic materials of intermediate decomposition. The fiber content of these materials is 17 to 40 percent (by volume) after rubbing.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":6,"ChoiceName":"f","ChoiceLabel":"f","ChoiceObsolete":0,"ChoiceDescription":"Frozen soil or water. This symbol indicates that a horizon or layer contains permanent ice. The symbol is not used for seasonally frozen layers or for dry permafrost.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":7,"ChoiceName":"g","ChoiceLabel":"g","ChoiceObsolete":0,"ChoiceDescription":"Strong gleying. This symbol indicates either that iron has been reduced and removed during soil formation or that saturation with stagnant water has preserved it in a reduced state. Most of the affected layers have chroma of 2 or less, and many have redox concentrations. The low chroma can represent either the color of reduced iron or the color of uncoated sand and silt particles from which iron has been removed. The symbol g is not used for materials of low chroma that have no history of wetness, such as some shales or E horizons. If g is used with B, pedogenic change in addition to gleying is implied. If no other pedogenic change besides gleying has taken place, the horizon is designated Cg.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":8,"ChoiceName":"h","ChoiceLabel":"h","ChoiceObsolete":0,"ChoiceDescription":"Illuvial accumulation of organic matter. This symbol is used with B to indicate the accumulation of illuvial, amorphous, dispersible complexes of organic matter and sesquioxides if the sesquioxide component is dominated by aluminum but is present only in very small quantities. The organo-sesquioxide material coats sand and silt particles. In some horizons these coatings have coalesced, filled pores, and cemented the horizon. The symbol h is also used in combination with s as \"Bhs\" if the amount of the sesquioxide component is significant but the color value and chroma, moist, of the horizon are 3 or less.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":9,"ChoiceName":"i","ChoiceLabel":"i","ChoiceObsolete":0,"ChoiceDescription":"Slightly decomposed organic material. This symbol is used with O to indicate the least decomposed of the organic materials. The fiber content of these materials is 40 percent or more (by volume) after rubbing.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":10,"ChoiceName":"k","ChoiceLabel":"k","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of secondary carbonates. This symbol indicates an accumulation of visible pedogenic calcium carbonate (less than 50 percent, by volume). Carbonate accumulations occur as carbonate filaments, coatings, masses, nodules, disseminated carbonate, or other forms.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":11,"ChoiceName":"m","ChoiceLabel":"m","ChoiceObsolete":0,"ChoiceDescription":"Cementation or induration. This symbol indicates continuous or nearly continuous cementation. It is used only for horizons that are more than 90 percent cemented, although they may be fractured. The cemented layer is physically root-restrictive. The predominant cementing agent (or the two dominant ones) may be indicated by adding defined letter suffixes, singly or in pairs. The horizon suffix kkm (and less commonly km) indicates cementation by carbonates; qm, cementation by silica; sm, cementation by iron; yym, cementation by gypsum; kqm, cementation by carbonates and silica; and zm, cementation by salts more soluble than gypsum.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":12,"ChoiceName":"n","ChoiceLabel":"n","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of sodium. This symbol indicates an accumulation of exchangeable sodium.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":13,"ChoiceName":"o","ChoiceLabel":"o","ChoiceObsolete":0,"ChoiceDescription":"This symbol indicates a residual accumulation of sesquioxides.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":14,"ChoiceName":"p","ChoiceLabel":"p","ChoiceObsolete":0,"ChoiceDescription":"Tillage or other disturbance. This symbol indicates a disturbance of the surface layer by mechanical means, pasturing, or similar uses. A disturbed organic horizon is designated Op. A disturbed mineral horizon is designated Ap even though it is clearly a former E, B, or C horizon.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":15,"ChoiceName":"q","ChoiceLabel":"q","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of silica. This symbol indicates an accumulation of secondary silica.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":16,"ChoiceName":"r","ChoiceLabel":"r","ChoiceObsolete":0,"ChoiceDescription":"Weathered or soft bedrock. This symbol is used with C to indicate layers of bedrock that are moderately cemented or less cemented. Examples are weathered igneous rock and partly consolidated sandstone, siltstone, or shale. The excavation difficulty is low to high.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":25,"ChoiceValue":17,"ChoiceName":"s","ChoiceLabel":"s","ChoiceObsolete":0,"ChoiceDescription":"Illuvial accumulation of sesquioxides and organic matter. This symbol is used with B to indicate an accumulation of illuvial, amorphous, dispersible complexes of organic matter and sesquioxides if both the organic matter and sesquioxide components are significant and if either the color value or chroma, moist, of the horizon is 4 or more. The symbol is also used in combination with h as \"Bhs\" if both the organic matter and sesquioxide components are significant and if the color value and chroma, moist, are 3 or less.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":27,"ChoiceValue":18,"ChoiceName":"ss","ChoiceLabel":"ss","ChoiceObsolete":0,"ChoiceDescription":"Presence of slickensides. This symbol indicates the presence of slickensides. Slickensides result directly from the swelling of clay minerals and shear failure, commonly at angles of 20 to 60 degrees above horizontal. They are indicators that other vertic characteristics, such as wedge-shaped peds and surface cracks, may be present.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":28,"ChoiceValue":19,"ChoiceName":"t","ChoiceLabel":"t","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of silicate clay. This symbol indicates an accumulation of silicate clay that has either formed and subsequently been translocated within the horizon or has been moved into the horizon by illuviation, or both. At least some part of the horizon should show evidence of clay accumulation either as coatings on surfaces of peds or in pores, or as lamellae or as bridges between mineral grains.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":30,"ChoiceValue":20,"ChoiceName":"v","ChoiceLabel":"v","ChoiceObsolete":0,"ChoiceDescription":"Plinthite. This symbol indicates the presence of iron-rich, humus-poor, reddish material that is firm or very firm when moist and is less than strongly cemented. It hardens irreversibly when exposed to the atmosphere and to repeated wetting and drying.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":31,"ChoiceValue":21,"ChoiceName":"w","ChoiceLabel":"w","ChoiceObsolete":0,"ChoiceDescription":"Development of color or structure. This symbol is used only with B to indicate the development of color or structure, or both, with little or no apparent illuvial accumulation of material. It should not be used to indicate a transitional horizon.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":32,"ChoiceValue":22,"ChoiceName":"x","ChoiceLabel":"x","ChoiceObsolete":0,"ChoiceDescription":"Fragipan character. This symbol indicates a genetically developed layer that has a combination of firmness, brittleness, and commonly a higher bulk density than adjacent layers. Some part of the layer is physically root-restrictive.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":33,"ChoiceValue":23,"ChoiceName":"y","ChoiceLabel":"y","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of gypsum. This symbol indicates a gypsum accumulation. The suffix y is used when the horizon fabric is dominated by soil particles or minerals other than gypsum. Gypsum is present in amounts that do not significantly obscure or disrupt other features of the horizon.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":35,"ChoiceValue":24,"ChoiceName":"z","ChoiceLabel":"z","ChoiceObsolete":0,"ChoiceDescription":"Accumulation of salts more soluble than gypsum. This symbol indicates an accumulation of salts that are more soluble than gypsum.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":25,"ChoiceName":"j","ChoiceLabel":"j","ChoiceObsolete":0,"ChoiceDescription":"Indicates an accumulation of jarosite. Jarosite is a potassium (ferric) iron hydroxy sulfate mineral (KFe3(SO4)2(OH)6) that is commonly an alteration product of pyrite that has been exposed to an oxidizing environment. Jarosite has hue of 2.5Y or yellower and normally has chroma of 6 or more, although chroma as low as 3 or 4 have been reported. It forms in preference to iron (hydr)oxides in active acid sulfate soils at pH of 3.5 or less and can be stable in post-active acid sulfate soils for long periods of time at higher pH.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":26,"ChoiceName":"jj","ChoiceLabel":"jj","ChoiceObsolete":0,"ChoiceDescription":"Evidence of cyroturbation. Evidence of cryoturbation includes irregular and broken horizon boundaries, sorted rock fragments, and organic soil materials occurring as bodies and broken layers within and/or between mineral soil layers. The organic bodies and layers are most commonly at the contact between the active layer and the permafrost.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":27,"ChoiceName":"ff","ChoiceLabel":"ff","ChoiceObsolete":0,"ChoiceDescription":"Dry permafrost. Used in layers or horizons that are colder than 0 degrees C, but do not contain ice. It is not used for layers or horizons that have seasonal temperatures below 0 degrees C. The f suffix is used for layers or horizons that contain permanent ice.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":28,"ChoiceName":"ca","ChoiceLabel":"ca","ChoiceObsolete":1,"ChoiceDescription":"An accumulation of carbonates.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":29,"ChoiceName":"co","ChoiceLabel":"co","ChoiceObsolete":0,"ChoiceDescription":"Coprogenous Earth. This symbol, used only with L, indicates a limnic layer of coprogenous earth (or sedimentary peat).","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":30,"ChoiceName":"ma","ChoiceLabel":"ma","ChoiceObsolete":0,"ChoiceDescription":"Marl. This symbol, used only with L, indicates a limnic layer of marl.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":31,"ChoiceName":"di","ChoiceLabel":"di","ChoiceObsolete":0,"ChoiceDescription":"Diatomaceous earth. This symbol, used only with L, indicates a limnic layer of diatomaceous earth.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":32,"ChoiceName":"kk","ChoiceLabel":"kk","ChoiceObsolete":0,"ChoiceDescription":"Engulfment of horizon by secondary carbonates. This symbol indicates major accumulations of pedogenic calcium carbonate. The suffix kk is used when the soil fabric is plugged with fine grained pedogenic carbonate (50 percent or more, by volume) that occurs as an essentially continuous medium. The suffix corresponds to the stage III plugged horizon or higher of the carbonate morphogenetic stages (Gile et al., 1966).","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":33,"ChoiceName":"u","ChoiceLabel":"u","ChoiceObsolete":0,"ChoiceDescription":"Presence of human-manufactured materials (artifacts). This symbol indicates the presence of manufactured artifacts that have been created or modified by humans, usually for a practical purpose in habitation, manufacturing, excavation, or construction activities. Examples of artifacts are processed wood products, liquid petroleum products, coal combustion by-products, asphalt, fibers and fabrics, bricks, cinder blocks, concrete, plastic, glass, rubber, paper, cardboard, iron and steel, altered metals and minerals, sanitary and medical waste, garbage, and landfill waste.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":34,"ChoiceValue":34,"ChoiceName":"yy","ChoiceLabel":"yy","ChoiceObsolete":0,"ChoiceDescription":"Dominance of horizon by gypsum. This symbol indicates a horizon that is dominated by the presence of gypsum. The gypsum content may be due to an accumulation of secondary gypsum, the transformation of primary gypsum inherited from parent material, or other processes. Suffix yy is used when the horizon fabric has such an abundance of gypsum (generally 50 percent or more, by volume) that pedogenic and/or lithologic features are obscured or disrupted by growth of gypsum crystals. Colors associated with horizons that use suffix yy are typically highly whitened with value of 7 through 9.5 and chroma of 2 or less.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":155,"DomainName":"horz_desgn_letter_suffix","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":35,"ChoiceName":"se","ChoiceLabel":"se","ChoiceObsolete":0,"ChoiceDescription":"This symbol indicates the presence of sulfides in mineral or organic horizons. Horizons with sulfides typically have dark colors (e.g. value 4, chroma 2). These horizons typically form in soils associated with coastal environments that are permanently saturated or submerged (i.e., tidal marshes or estuaries). Soil materials which have sulfidization actively occurring emanate hydrogen sulfide gas which is detectable by its odor (Fanning and Fanning, 1989, or Fanning et al., 2002). Sulfides may also occur in upland environments that have a source of sulfur to form sulfides. Soils in such environments are often of geologic origin and may not produce a hydrogen sulfide odor. Examples include soils formed in parent materials derived from coal deposits such as lignite or soils formed in coastal plain deposits such as glauconite that have not been oxidized because of thick layers of overburden.","ColumnPhysicalName":"osdhorzdesignlettersuffix","ColumnLogicalName":"osd_horz_desgn_letter_suffix"} {"DomainID":163,"DomainName":"soil_slippage_potential","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"low","ChoiceLabel":"Low","ChoiceObsolete":0,"ChoiceDescription":"Low potential of slippage.","ColumnPhysicalName":"soilslippot","ColumnLogicalName":"soil_slippage_potential"} {"DomainID":163,"DomainName":"soil_slippage_potential","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"moderately low","ChoiceLabel":"Moderately low","ChoiceObsolete":1,"ChoiceDescription":"Moderately low hazzard of slippage.","ColumnPhysicalName":"soilslippot","ColumnLogicalName":"soil_slippage_potential"} {"DomainID":163,"DomainName":"soil_slippage_potential","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"medium","ChoiceLabel":"Medium","ChoiceObsolete":0,"ChoiceDescription":"Medium potential of slippage.","ColumnPhysicalName":"soilslippot","ColumnLogicalName":"soil_slippage_potential"} {"DomainID":163,"DomainName":"soil_slippage_potential","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderately high","ChoiceLabel":"Moderately high","ChoiceObsolete":1,"ChoiceDescription":"Moderately high hazard of slippage.","ColumnPhysicalName":"soilslippot","ColumnLogicalName":"soil_slippage_potential"} {"DomainID":163,"DomainName":"soil_slippage_potential","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"high","ChoiceLabel":"High","ChoiceObsolete":0,"ChoiceDescription":"High potential of slippage.","ColumnPhysicalName":"soilslippot","ColumnLogicalName":"soil_slippage_potential"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"very brief","ChoiceLabel":"Very brief (4 to 48 hours)","ChoiceObsolete":0,"ChoiceDescription":"4 hours to 48 hours","ColumnPhysicalName":"coponddurcl","ColumnLogicalName":"comp_ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"brief","ChoiceLabel":"Brief (2 to 7 days)","ChoiceObsolete":0,"ChoiceDescription":"2 days to 7 days","ColumnPhysicalName":"coponddurcl","ColumnLogicalName":"comp_ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"long","ChoiceLabel":"Long (7 to 30 days)","ChoiceObsolete":0,"ChoiceDescription":"7 days to 30 days","ColumnPhysicalName":"coponddurcl","ColumnLogicalName":"comp_ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"very long","ChoiceLabel":"Very long (more than 30 days)","ChoiceObsolete":0,"ChoiceDescription":"More than 30 days","ColumnPhysicalName":"coponddurcl","ColumnLogicalName":"comp_ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"very brief","ChoiceLabel":"Very brief (4 to 48 hours)","ChoiceObsolete":0,"ChoiceDescription":"4 hours to 48 hours","ColumnPhysicalName":"osdponddurcl","ColumnLogicalName":"osd_ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"brief","ChoiceLabel":"Brief (2 to 7 days)","ChoiceObsolete":0,"ChoiceDescription":"2 days to 7 days","ColumnPhysicalName":"osdponddurcl","ColumnLogicalName":"osd_ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"long","ChoiceLabel":"Long (7 to 30 days)","ChoiceObsolete":0,"ChoiceDescription":"7 days to 30 days","ColumnPhysicalName":"osdponddurcl","ColumnLogicalName":"osd_ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"very long","ChoiceLabel":"Very long (more than 30 days)","ChoiceObsolete":0,"ChoiceDescription":"More than 30 days","ColumnPhysicalName":"osdponddurcl","ColumnLogicalName":"osd_ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"very brief","ChoiceLabel":"Very brief (4 to 48 hours)","ChoiceObsolete":0,"ChoiceDescription":"4 hours to 48 hours","ColumnPhysicalName":"ponddurcl","ColumnLogicalName":"ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"brief","ChoiceLabel":"Brief (2 to 7 days)","ChoiceObsolete":0,"ChoiceDescription":"2 days to 7 days","ColumnPhysicalName":"ponddurcl","ColumnLogicalName":"ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"long","ChoiceLabel":"Long (7 to 30 days)","ChoiceObsolete":0,"ChoiceDescription":"7 days to 30 days","ColumnPhysicalName":"ponddurcl","ColumnLogicalName":"ponding_duration_class"} {"DomainID":167,"DomainName":"ponding_duration_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"very long","ChoiceLabel":"Very long (more than 30 days)","ChoiceObsolete":0,"ChoiceDescription":"More than 30 days","ColumnPhysicalName":"ponddurcl","ColumnLogicalName":"ponding_duration_class"} {"DomainID":168,"DomainName":"pore_continuity_vertical","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":1,"ChoiceName":"high","ChoiceLabel":"High","ChoiceObsolete":0,"ChoiceDescription":"=>10 cm vertical distance.","ColumnPhysicalName":"osdporecont","ColumnLogicalName":"osd_pore_continuity_vertical"} {"DomainID":168,"DomainName":"pore_continuity_vertical","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":2,"ChoiceName":"low","ChoiceLabel":"Low","ChoiceObsolete":0,"ChoiceDescription":"<1 cm vertical distance","ColumnPhysicalName":"osdporecont","ColumnLogicalName":"osd_pore_continuity_vertical"} {"DomainID":168,"DomainName":"pore_continuity_vertical","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"1 to <10 cm vertical 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{"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":89,"ChoiceValue":68,"ChoiceName":"sy","ChoiceLabel":"slaty","ChoiceObsolete":1,"ColumnPhysicalName":"osdtexmod","ColumnLogicalName":"osd_texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":90,"ChoiceValue":69,"ChoiceName":"syv","ChoiceLabel":"Very slaty","ChoiceObsolete":1,"ColumnPhysicalName":"osdtexmod","ColumnLogicalName":"osd_texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":91,"ChoiceValue":70,"ChoiceName":"syx","ChoiceLabel":"Extremely slaty","ChoiceObsolete":1,"ColumnPhysicalName":"osdtexmod","ColumnLogicalName":"osd_texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":1,"ChoiceValue":71,"ChoiceName":"art","ChoiceLabel":"Artifactual","ChoiceObsolete":0,"ChoiceDescription":"15 to 35 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{"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":31,"ChoiceValue":10,"ChoiceName":"fl","ChoiceLabel":"Flaggy","ChoiceObsolete":0,"ChoiceDescription":"Flaggy","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":33,"ChoiceValue":11,"ChoiceName":"flv","ChoiceLabel":"Very flaggy","ChoiceObsolete":0,"ChoiceDescription":"Very flaggy","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":35,"ChoiceValue":12,"ChoiceName":"flx","ChoiceLabel":"Extremely flaggy","ChoiceObsolete":0,"ChoiceDescription":"Extremely flaggy","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} 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{"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":41,"ChoiceValue":16,"ChoiceName":"grm","ChoiceLabel":"Medium gravelly","ChoiceObsolete":0,"ChoiceDescription":"Medium gravelly","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":42,"ChoiceValue":17,"ChoiceName":"grv","ChoiceLabel":"Very gravelly","ChoiceObsolete":0,"ChoiceDescription":"Very gravelly","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":44,"ChoiceValue":18,"ChoiceName":"grx","ChoiceLabel":"Extremely gravelly","ChoiceObsolete":0,"ChoiceDescription":"Extremely gravelly","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":55,"ChoiceValue":19,"ChoiceName":"mk","ChoiceLabel":"Mucky","ChoiceObsolete":0,"ChoiceDescription":"Mucky is used to modify near surface horizons of mineral soils that are saturated with water for 30 or more cumulative days in normal years (or are artificially drained). 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{"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":62,"ChoiceValue":32,"ChoiceName":"pcb","ChoiceLabel":"Paracobbly","ChoiceObsolete":0,"ChoiceDescription":"Paracobbly","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":63,"ChoiceValue":33,"ChoiceName":"pcbv","ChoiceLabel":"Very paracobbly","ChoiceObsolete":0,"ChoiceDescription":"Very paracobbly","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":64,"ChoiceValue":34,"ChoiceName":"pcbx","ChoiceLabel":"Extremely paracobbly","ChoiceObsolete":0,"ChoiceDescription":"Extremely paracobbly","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":65,"ChoiceValue":35,"ChoiceName":"pcn","ChoiceLabel":"Parachannery","ChoiceObsolete":0,"ChoiceDescription":"Parachannery","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":66,"ChoiceValue":36,"ChoiceName":"pcnv","ChoiceLabel":"Very parachannery","ChoiceObsolete":0,"ChoiceDescription":"Very parachannery","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":67,"ChoiceValue":37,"ChoiceName":"pcnx","ChoiceLabel":"Extremely parachannery","ChoiceObsolete":0,"ChoiceDescription":"Extremely parachannery","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} 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{"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":80,"ChoiceValue":66,"ChoiceName":"shv","ChoiceLabel":"Very shaly","ChoiceObsolete":1,"ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":81,"ChoiceValue":67,"ChoiceName":"shx","ChoiceLabel":"Extremely shaly","ChoiceObsolete":1,"ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":89,"ChoiceValue":68,"ChoiceName":"sy","ChoiceLabel":"slaty","ChoiceObsolete":1,"ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":90,"ChoiceValue":69,"ChoiceName":"syv","ChoiceLabel":"Very 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The total of shell fragments plus artifacts is 15 to less than 35 percent, by volume. Shells and shell-size artifacts dominate fraction => 2 mm.","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":98,"ChoiceValue":98,"ChoiceName":"shfvart","ChoiceLabel":"Very shelly-artifactual","ChoiceObsolete":0,"ChoiceDescription":"Horizon contains a combination of shell fragments and artifacts which are discrete (=> 2mm), cohesive, and persistent. The total of shell fragments plus artifacts is 35 to less than 60 percent, by volume. Shells and shell-size artifacts dominate fraction => 2 mm.","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":190,"DomainName":"texture_modifier","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":99,"ChoiceValue":99,"ChoiceName":"shfeart","ChoiceLabel":"Extremely shelly-artifactual","ChoiceObsolete":0,"ChoiceDescription":"Horizon contains a combination of shell fragments and artifacts which are discrete (=> 2mm), cohesive, and persistent. The total of shell fragments plus artifacts is 60 to less than 90 percent, by volume. Shells and shell-size artifacts dominate fraction => 2 mm.","ColumnPhysicalName":"texmod","ColumnLogicalName":"texture_modifier"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":5,"ChoiceValue":1,"ChoiceName":"cl-ml","ChoiceLabel":"CL-ML","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. 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It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":38,"ChoiceValue":8,"ChoiceName":"sw-sc","ChoiceLabel":"SW-SC","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":39,"ChoiceValue":9,"ChoiceName":"sw-sm","ChoiceLabel":"SW-SM","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. 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It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":15,"ChoiceValue":11,"ChoiceName":"gw-gc","ChoiceLabel":"GW-GC","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":1,"ChoiceValue":12,"ChoiceName":"ch","ChoiceLabel":"CH","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays (liquid limit is 50% or more), Fat Clay. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":2,"ChoiceValue":13,"ChoiceName":"cl","ChoiceLabel":"CL","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays (liquid limit is less than 50%), Lean Clay. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":8,"ChoiceValue":14,"ChoiceName":"gc","ChoiceLabel":"GC","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Gravels, gravel with fines, Clayey Gravel. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":10,"ChoiceValue":15,"ChoiceName":"gm","ChoiceLabel":"GM","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Gravels, Gravels with fines, Silty Gravel. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":11,"ChoiceValue":16,"ChoiceName":"gp","ChoiceLabel":"GP","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Gravels, clean gravels, Poorly Graded Gravel. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":14,"ChoiceValue":17,"ChoiceName":"gw","ChoiceLabel":"GW","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Gravels, clean gravels, Well-Graded Gravel. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":17,"ChoiceValue":18,"ChoiceName":"mh","ChoiceLabel":"MH","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays, (liquid limit is 50% or more), Elastic Silt. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":22,"ChoiceValue":19,"ChoiceName":"ml","ChoiceLabel":"ML","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays, (liquid limit is less than 50%), Silt. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":27,"ChoiceValue":20,"ChoiceName":"oh","ChoiceLabel":"OH","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays, (liquid limit is 50% or more), Organic Clay or Organic Silt. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":29,"ChoiceValue":21,"ChoiceName":"ol","ChoiceLabel":"OL","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays (liquid limit is less than 50%), Organic Clay or Organic Silt. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":30,"ChoiceValue":22,"ChoiceName":"pt","ChoiceLabel":"PT","ChoiceObsolete":0,"ChoiceDescription":"Highly organic soils, Peat. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":31,"ChoiceValue":23,"ChoiceName":"sc","ChoiceLabel":"SC","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Sands, sands with fines, Clayey Sand. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":33,"ChoiceValue":24,"ChoiceName":"sm","ChoiceLabel":"SM","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Sands, Sands with fines, Silty Sand. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":34,"ChoiceValue":25,"ChoiceName":"sp","ChoiceLabel":"SP","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Sands, Clean Sands, Poorly Graded Sand. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":37,"ChoiceValue":26,"ChoiceName":"sw","ChoiceLabel":"SW","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Sands, Clean Sands, Well-graded Sand. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":3,"ChoiceValue":27,"ChoiceName":"cl-a","ChoiceLabel":"CL-A (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":4,"ChoiceValue":28,"ChoiceName":"cl-k","ChoiceLabel":"CL-K (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":6,"ChoiceValue":29,"ChoiceName":"cl-o","ChoiceLabel":"CL-O (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":7,"ChoiceValue":30,"ChoiceName":"cl-t","ChoiceLabel":"CL-T (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":18,"ChoiceValue":31,"ChoiceName":"mh-a","ChoiceLabel":"MH-A (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":19,"ChoiceValue":32,"ChoiceName":"mh-k","ChoiceLabel":"MH-K (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":20,"ChoiceValue":33,"ChoiceName":"mh-o","ChoiceLabel":"MH-O (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":21,"ChoiceValue":34,"ChoiceName":"mh-t","ChoiceLabel":"MH-T (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":23,"ChoiceValue":35,"ChoiceName":"ml-a","ChoiceLabel":"ML-A (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":24,"ChoiceValue":36,"ChoiceName":"ml-k","ChoiceLabel":"ML-K (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":25,"ChoiceValue":37,"ChoiceName":"ml-o","ChoiceLabel":"ML-O (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":26,"ChoiceValue":38,"ChoiceName":"ml-t","ChoiceLabel":"ML-T (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":28,"ChoiceValue":39,"ChoiceName":"oh-t","ChoiceLabel":"OH-T (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"osdunifiedcl","ColumnLogicalName":"osd_unified_soil_class"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":5,"ChoiceValue":1,"ChoiceName":"cl-ml","ChoiceLabel":"CL-ML","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":9,"ChoiceValue":2,"ChoiceName":"gc-gm","ChoiceLabel":"GC-GM","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":12,"ChoiceValue":3,"ChoiceName":"gp-gc","ChoiceLabel":"GP-GC","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":13,"ChoiceValue":4,"ChoiceName":"gp-gm","ChoiceLabel":"GP-GM","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":32,"ChoiceValue":5,"ChoiceName":"sc-sm","ChoiceLabel":"SC-SM","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":35,"ChoiceValue":6,"ChoiceName":"sp-sc","ChoiceLabel":"SP-SC","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":36,"ChoiceValue":7,"ChoiceName":"sp-sm","ChoiceLabel":"SP-SM","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":38,"ChoiceValue":8,"ChoiceName":"sw-sc","ChoiceLabel":"SW-SC","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":39,"ChoiceValue":9,"ChoiceName":"sw-sm","ChoiceLabel":"SW-SM","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":16,"ChoiceValue":10,"ChoiceName":"gw-gm","ChoiceLabel":"GW-GM","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":15,"ChoiceValue":11,"ChoiceName":"gw-gc","ChoiceLabel":"GW-GC","ChoiceObsolete":0,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":1,"ChoiceValue":12,"ChoiceName":"ch","ChoiceLabel":"CH","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays (liquid limit is 50% or more), Fat Clay. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":2,"ChoiceValue":13,"ChoiceName":"cl","ChoiceLabel":"CL","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays (liquid limit is less than 50%), Lean Clay. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":8,"ChoiceValue":14,"ChoiceName":"gc","ChoiceLabel":"GC","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Gravels, gravel with fines, Clayey Gravel. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":10,"ChoiceValue":15,"ChoiceName":"gm","ChoiceLabel":"GM","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Gravels, Gravels with fines, Silty Gravel. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":11,"ChoiceValue":16,"ChoiceName":"gp","ChoiceLabel":"GP","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Gravels, clean gravels, Poorly Graded Gravel. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":14,"ChoiceValue":17,"ChoiceName":"gw","ChoiceLabel":"GW","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Gravels, clean gravels, Well-Graded Gravel. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":17,"ChoiceValue":18,"ChoiceName":"mh","ChoiceLabel":"MH","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays, (liquid limit is 50% or more), Elastic Silt. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":22,"ChoiceValue":19,"ChoiceName":"ml","ChoiceLabel":"ML","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays, (liquid limit is less than 50%), Silt. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":27,"ChoiceValue":20,"ChoiceName":"oh","ChoiceLabel":"OH","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays, (liquid limit is 50% or more), Organic Clay or Organic Silt. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":29,"ChoiceValue":21,"ChoiceName":"ol","ChoiceLabel":"OL","ChoiceObsolete":0,"ChoiceDescription":"FINE-GRAINED SOILS, Silts and clays (liquid limit is less than 50%), Organic Clay or Organic Silt. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":30,"ChoiceValue":22,"ChoiceName":"pt","ChoiceLabel":"PT","ChoiceObsolete":0,"ChoiceDescription":"Highly organic soils, Peat. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":31,"ChoiceValue":23,"ChoiceName":"sc","ChoiceLabel":"SC","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Sands, sands with fines, Clayey Sand. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":33,"ChoiceValue":24,"ChoiceName":"sm","ChoiceLabel":"SM","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Sands, Sands with fines, Silty Sand. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":34,"ChoiceValue":25,"ChoiceName":"sp","ChoiceLabel":"SP","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Sands, Clean Sands, Poorly Graded Sand. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":37,"ChoiceValue":26,"ChoiceName":"sw","ChoiceLabel":"SW","ChoiceObsolete":0,"ChoiceDescription":"COARSE-GRAINED SOILS, Sands, Clean Sands, Well-graded Sand. Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle size distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic matter (ASTM test D 2487, in ASTM, 1984).","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":3,"ChoiceValue":27,"ChoiceName":"cl-a","ChoiceLabel":"CL-A (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":4,"ChoiceValue":28,"ChoiceName":"cl-k","ChoiceLabel":"CL-K (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":6,"ChoiceValue":29,"ChoiceName":"cl-o","ChoiceLabel":"CL-O (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":7,"ChoiceValue":30,"ChoiceName":"cl-t","ChoiceLabel":"CL-T (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":18,"ChoiceValue":31,"ChoiceName":"mh-a","ChoiceLabel":"MH-A (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":19,"ChoiceValue":32,"ChoiceName":"mh-k","ChoiceLabel":"MH-K (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":20,"ChoiceValue":33,"ChoiceName":"mh-o","ChoiceLabel":"MH-O (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":21,"ChoiceValue":34,"ChoiceName":"mh-t","ChoiceLabel":"MH-T (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":23,"ChoiceValue":35,"ChoiceName":"ml-a","ChoiceLabel":"ML-A (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":24,"ChoiceValue":36,"ChoiceName":"ml-k","ChoiceLabel":"ML-K (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":25,"ChoiceValue":37,"ChoiceName":"ml-o","ChoiceLabel":"ML-O (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":26,"ChoiceValue":38,"ChoiceName":"ml-t","ChoiceLabel":"ML-T (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":191,"DomainName":"unified_soil_classification","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":28,"ChoiceValue":39,"ChoiceName":"oh-t","ChoiceLabel":"OH-T (proposed)","ChoiceObsolete":1,"ChoiceDescription":"Reference: This is a classification of soil material designed for general construction purposes. It is dependent on the particle \r\nsize distribution of the <75 mm, the liquid limit, and the plasticity index and on whether the soil material is high in organic \r\nmatter (ASTM test D 2487, in ASTM, 1984). \r\n\r\nThis subclass is based on research by H. H. Sato and proposed in: Sato, H. H. 1971. Interpretation of Index Properties of the Unified Classification System for Hawaiian Soils. Unpublished Master of Science thesis. University of Hawaii. \r\n\r\nAs proposed, this subclass is only to be used in the islands of the state of Hawaii and islands included in the Pacific Island Area. As of 10 Jun 2016 this subclass is under review.","ColumnPhysicalName":"unifiedcl","ColumnLogicalName":"unified_soil_classification"} {"DomainID":192,"DomainName":"terms_used_in_lieu_of_texture","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":3,"ChoiceValue":1,"ChoiceName":"ashy","ChoiceLabel":"Ashy","ChoiceObsolete":1,"ChoiceDescription":"Ashy","ColumnPhysicalName":"legacyterminlieu","ColumnLogicalName":"legacy_term_in_lieu_of_texture"} {"DomainID":192,"DomainName":"terms_used_in_lieu_of_texture","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":1,"ChoiceValue":2,"ChoiceName":"apum","ChoiceLabel":"Ashy-pumiceous","ChoiceObsolete":1,"ChoiceDescription":"Ashy-pumiceous","ColumnPhysicalName":"legacyterminlieu","ColumnLogicalName":"legacy_term_in_lieu_of_texture"} 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{"DomainID":192,"DomainName":"terms_used_in_lieu_of_texture","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":10,"ChoiceValue":6,"ChoiceName":"cind","ChoiceLabel":"Cinders","ChoiceObsolete":1,"ChoiceDescription":"Cindery","ColumnPhysicalName":"legacyterminlieu","ColumnLogicalName":"legacy_term_in_lieu_of_texture"} {"DomainID":192,"DomainName":"terms_used_in_lieu_of_texture","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":12,"ChoiceValue":7,"ChoiceName":"cndy","ChoiceLabel":"Cindery","ChoiceObsolete":1,"ChoiceDescription":"Cindery","ColumnPhysicalName":"legacyterminlieu","ColumnLogicalName":"legacy_term_in_lieu_of_texture"} {"DomainID":192,"DomainName":"terms_used_in_lieu_of_texture","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":14,"ChoiceValue":8,"ChoiceName":"cpf","ChoiceLabel":"Consolidated permafrost (ice rich)","ChoiceObsolete":1,"ChoiceDescription":"Consolidated permafrost (ice 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{"DomainID":192,"DomainName":"terms_used_in_lieu_of_texture","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":19,"ChoiceValue":11,"ChoiceName":"frag","ChoiceLabel":"Fragmental material","ChoiceObsolete":1,"ChoiceDescription":"Fragmental material","ColumnPhysicalName":"legacyterminlieu","ColumnLogicalName":"legacy_term_in_lieu_of_texture"} {"DomainID":192,"DomainName":"terms_used_in_lieu_of_texture","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":20,"ChoiceValue":12,"ChoiceName":"gr","ChoiceLabel":"Gravel","ChoiceObsolete":0,"ChoiceDescription":"Gravel","ColumnPhysicalName":"legacyterminlieu","ColumnLogicalName":"legacy_term_in_lieu_of_texture"} {"DomainID":192,"DomainName":"terms_used_in_lieu_of_texture","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":21,"ChoiceValue":13,"ChoiceName":"gyp","ChoiceLabel":"Gypsiferous material","ChoiceObsolete":1,"ChoiceDescription":"Material that contains 15 to < 40 percent by weight 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The deposits are stratified and may occur in the form of outwash plains, valley trains, deltas, kames, eskers, and kame terraces.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":46,"ChoiceValue":99,"ChoiceName":"glaciolacustrine deposits","ChoiceLabel":"Glaciolacustrine deposits","ChoiceObsolete":0,"ChoiceDescription":"Material ranging from fine clay to sand derived from glaciers and deposited in glacial lakes by water originating mainly from the melting of glacial ice. Many are bedded or laminated with varves or rhythmites.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":47,"ChoiceValue":100,"ChoiceName":"glaciomarine deposits","ChoiceLabel":"Glaciomarine deposits","ChoiceObsolete":0,"ChoiceDescription":"Glacially eroded, terrestrially derived sediments (clay, silt, sand, and gravel) that accumulated on the ocean floor. Sediments may be accumulated as an ice-contact deposit, by fluvial transport, ice-rafting, or eolian transport.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":67,"ChoiceValue":101,"ChoiceName":"lacustrine deposits","ChoiceLabel":"Lacustrine deposits","ChoiceObsolete":0,"ChoiceDescription":"Clastic sediments and chemical precipitates deposited in lakes.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":82,"ChoiceValue":102,"ChoiceName":"loess","ChoiceLabel":"Loess","ChoiceObsolete":0,"ChoiceDescription":"Material transported and deposited by wind and consisting predominantly of silt size.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":83,"ChoiceValue":103,"ChoiceName":"loess, calcareous","ChoiceLabel":"Calcareous loess","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":87,"ChoiceValue":104,"ChoiceName":"marine deposits","ChoiceLabel":"Marine deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":89,"ChoiceValue":105,"ChoiceName":"mass movement deposits","ChoiceLabel":"Mass movement deposits","ChoiceObsolete":0,"ChoiceDescription":"Sediment resulting from the dislodgement and downslope transport of soil and rock material as a unit under direct gravitational stress. The process includes slow displacements such as creep and solifluction, and rapid movements such as landslides, rock slides, and falls, earthflows, debris flows, and avalanches. Agents of fluid transport (water, ice, air) may play an important, if subordinate role in the process.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":91,"ChoiceValue":106,"ChoiceName":"mine spoil or earthy fill","ChoiceLabel":"Mine spoil or earthy fill","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":102,"ChoiceValue":107,"ChoiceName":"organic, grassy material","ChoiceLabel":"Grassy organic material","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":107,"ChoiceValue":108,"ChoiceName":"outwash","ChoiceLabel":"Outwash","ChoiceObsolete":0,"ChoiceDescription":"(a) Stratified detritus (chiefly sand and gravel) removed or \"washed out\" from a glacier by melt-water streams and deposited in front of or beyond the end moraine or the margin of an active glacier. The coarser material is deposited nearer to the ice.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":111,"ChoiceValue":109,"ChoiceName":"pedisediment","ChoiceLabel":"Pedisediment","ChoiceObsolete":0,"ChoiceDescription":"A layer of sediment, eroded from the shoulder and back slope of an erosional slope, that lies on and is, or was, being transported across a pediment.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":117,"ChoiceValue":110,"ChoiceName":"residuum","ChoiceLabel":"Residuum","ChoiceObsolete":0,"ChoiceDescription":"Unconsolidated, weathered, or partly weathered mineral material that accumulates by disintegration of bedrock in place.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":150,"ChoiceValue":111,"ChoiceName":"slope alluvium","ChoiceLabel":"Slope alluvium","ChoiceObsolete":0,"ChoiceDescription":"Sediment gradually transported on mountain or hill slopes primarily by alluvial processes and characterized by particle sorting. In a profile sequence, sediments may be distinguished by differences in size and/or specific gravity of coarse fragments and may be separated by stone lines. Sorting of rounded or subrounded pebbles or cobbles and burnished peds distinguish these materials from unsorted colluvial deposits.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":158,"ChoiceValue":112,"ChoiceName":"tephra","ChoiceLabel":"Tephra","ChoiceObsolete":0,"ChoiceDescription":"A collective term for all clastic volcanic materials that are ejected from a vent during an eruption and transported through the air, including ash [volcanic], blocks [volcanic], cinders, lapilli, scoria, and pumice. Tephra is a general term which, unlike many volcaniclastic terms, does not denote properties of composition, visicularity, or grain size.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":159,"ChoiceValue":113,"ChoiceName":"till, ablation","ChoiceLabel":"Ablation till","ChoiceObsolete":0,"ChoiceDescription":"A general term for loose, relatively permeable material deposited during the downwasting of nearly static glacial ice, either contained within or accumulated on the surface of the glacier.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":160,"ChoiceValue":114,"ChoiceName":"till, basal","ChoiceLabel":"Basal till","ChoiceObsolete":0,"ChoiceDescription":"Unconsolidated material of mixed composition deposited at the base (bottom) of a glacier [ The term emphaizes the e.g. subglacial till. Types of basal till include lodgment, melt-out, and flow till.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":161,"ChoiceValue":115,"ChoiceName":"till, flow","ChoiceLabel":"Flow till","ChoiceObsolete":0,"ChoiceDescription":"A till, commonly supraglacial, that is modified and transported by plastic mass flow; also spelled flow till. Compare - ablation till, basal till, lodgment till, mass-movement till, slump-till, supraglacial melt-out till.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":162,"ChoiceValue":116,"ChoiceName":"till, lodgment","ChoiceLabel":"Lodgment till","ChoiceObsolete":0,"ChoiceDescription":"A basal till commonly characterized by compact, fissile (\"platy\") structure and containing coarse fragments oriented with their long axes generally parallel to the direction of ice movement.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":163,"ChoiceValue":117,"ChoiceName":"till, melt-out","ChoiceLabel":"Melt-out till","ChoiceObsolete":0,"ChoiceDescription":"Till derived from slow melting of debris-rich stagnant ice buried beneath sufficient overburden to inhibit deformation under gravity, thus preserving structures derived from the parent ice.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":164,"ChoiceValue":118,"ChoiceName":"till, slump","ChoiceLabel":"Slump till","ChoiceObsolete":1,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":166,"ChoiceValue":119,"ChoiceName":"till, supraglacial","ChoiceLabel":"Supraglacial till","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":168,"ChoiceValue":120,"ChoiceName":"till, unspecified","ChoiceLabel":"Till","ChoiceObsolete":0,"ChoiceDescription":"Dominantly unsorted and unstratified drift, generally unconsolidated and deposited directly by a glacier without subsequent reworking by meltwater, and consisting of a heterogeneous mixture of clay, silt, sand, gravel, stones, and boulders; rock fragments of various lithologies are imbedded within a finer matrix that can range from clay to sandy loam. Compare - ablation till, basal till, flowtill, lodgment till, drift, moraine.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":179,"ChoiceValue":121,"ChoiceName":"valley side alluvium","ChoiceLabel":"Valley side alluvium","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":156,"ChoiceValue":122,"ChoiceName":"supraglacial debris-flow","ChoiceLabel":"Supraglacial debris-flow","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":167,"ChoiceValue":123,"ChoiceName":"till, supraglacial meltout","ChoiceLabel":"Supraglacial meltout till","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":124,"ChoiceName":"backswamp deposits","ChoiceLabel":"Backswamp deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":108,"ChoiceValue":125,"ChoiceName":"overbank deposits","ChoiceLabel":"Overbank deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":101,"ChoiceValue":126,"ChoiceName":"mudflow deposits","ChoiceLabel":"Mudflow deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":127,"ChoiceName":"block glide deposits","ChoiceLabel":"Block glide deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":128,"ChoiceName":"creep deposits","ChoiceLabel":"Creep deposits","ChoiceObsolete":0,"ChoiceDescription":"Sediment resulting from slow mass movement of earth material down slopes, caused by gravity but facilitated by saturation with water and alternate freezing and thawing.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":129,"ChoiceName":"debris avalanche deposits","ChoiceLabel":"Debris avalanche deposits","ChoiceObsolete":0,"ChoiceDescription":"Sediment resulting from the very rapid and usually sudden sliding and flow of incoherent, unsorted mixtures of soil and weathered bedrock.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":130,"ChoiceName":"debris flow deposits","ChoiceLabel":"Debris flow deposits","ChoiceObsolete":0,"ChoiceDescription":"Sediment resulting from a mass movement of rock fragments, soil, mud, more than half of the particles being larger than sand size.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":27,"ChoiceValue":131,"ChoiceName":"debris slide deposits","ChoiceLabel":"Debris slide deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":37,"ChoiceValue":132,"ChoiceName":"earthflow deposits","ChoiceLabel":"Earthflow deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":71,"ChoiceValue":133,"ChoiceName":"lateral spread deposits","ChoiceLabel":"Lateral spread deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":121,"ChoiceValue":134,"ChoiceName":"rockfall deposits","ChoiceLabel":"Rockfall deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":120,"ChoiceValue":135,"ChoiceName":"rockfall avalanche deposits","ChoiceLabel":"Rockfall avalanche deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":125,"ChoiceValue":136,"ChoiceName":"rotational slide deposits","ChoiceLabel":"Rotational slide deposits","ChoiceObsolete":0,"ChoiceDescription":"An accumlation of sediment resulting from a mass movement and a process characterized by a slide in which shearing takes place on a well defined, curved shear surface, concave upward, producing a backward rotation in the displaced mass.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":137,"ChoiceValue":137,"ChoiceName":"scree","ChoiceLabel":"Scree","ChoiceObsolete":0,"ChoiceDescription":"A collective term for an accumulation of coarse rock debris or a sheet of coarse debris mantling a slope. Scree is not a synonym of talus, as scree includes loose, coarse fragment material on slopes without cliffs.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":152,"ChoiceValue":138,"ChoiceName":"soil fall deposits","ChoiceLabel":"Soil fall deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":157,"ChoiceValue":139,"ChoiceName":"talus","ChoiceLabel":"Talus","ChoiceObsolete":0,"ChoiceDescription":"Rock fragments of any size or shape (usually coarse and angular) derived from and lying at the base of a cliff or very steep rock slope. The accumulated mass of such loose broken rock formed chiefly by falling, rolling, or sliding.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":169,"ChoiceValue":140,"ChoiceName":"topple deposits","ChoiceLabel":"Topple deposits","ChoiceObsolete":0,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":53,"ChoiceValue":141,"ChoiceName":"grus","ChoiceLabel":"Grus","ChoiceObsolete":0,"ChoiceDescription":"The fragmental products of in situ granular disintegration of granite and granitic rocks, dominated by inter-crystal disintegration.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":132,"ChoiceValue":142,"ChoiceName":"saprolite","ChoiceLabel":"Saprolite","ChoiceObsolete":0,"ChoiceDescription":"- (Provisional definition) Soft, friable, isovolumetrically weathered bedrock that retains the fabric and structure of the parent rock (Colman and Dethier, 1986) exhibiting extensive inter-crystal and intra-crystal weathering. \r\n\r\nIn pedology, saprolite was formerly applied to any unconsolidated residual material underlying the soil and grading to hard bedrock below.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":39,"ChoiceValue":143,"ChoiceName":"eolian sands","ChoiceLabel":"Eolian sands","ChoiceObsolete":0,"ChoiceDescription":"Material transported and deposited by the wind, dominated by particles of sand-size (0.05-2 mm).","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":84,"ChoiceValue":144,"ChoiceName":"loess, noncalcareous","ChoiceLabel":"Noncalcareous loess","ChoiceObsolete":0,"ChoiceDescription":"Noncalcareous material transported and deposited by wind and consisting predominantly of silt size (0.002-0.05 mm).","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":110,"ChoiceValue":145,"ChoiceName":"parna","ChoiceLabel":"Parna","ChoiceObsolete":0,"ChoiceDescription":"A term used, especially in southeast Australia, for silt and sand-sized aggregates of eolian clay occurring in sheets.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":69,"ChoiceValue":146,"ChoiceName":"lahar deposits","ChoiceLabel":"Lahar deposits","ChoiceObsolete":0,"ChoiceDescription":"Unconsolidated volcaniclastic material emplaced as mudflows on or near the flanks of a volcano.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":70,"ChoiceValue":147,"ChoiceName":"lapilli","ChoiceLabel":"Lapilli","ChoiceObsolete":0,"ChoiceDescription":"Non or slightly vesicular pyroclastics, 2.0 to 76 mm in at least one dimension, with an apparent specific gravity of 2.0 or more.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":148,"ChoiceName":"ash flow (pyroclastic)","ChoiceLabel":"Ash flow","ChoiceObsolete":0,"ChoiceDescription":"A highly heated mixture of volcanic gases and ash, traveling down the flank of a volcano or along the surface of the ground; produced by the explosive disintegration of viscous lava in a volcanic crater, or by the explosive emission of gas-charged ash from a fissure or group of fissures. The solid materials contained in a typical ash flow are generally unsorted and ordinarily include volcanic dust, pumice, scoria, and blocks in addition to ash.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":153,"ChoiceValue":149,"ChoiceName":"solid rock","ChoiceLabel":"Solid rock","ChoiceObsolete":1,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":178,"ChoiceValue":150,"ChoiceName":"unconsolidated sediments","ChoiceLabel":"Unconsolidated sediments","ChoiceObsolete":1,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":154,"ChoiceValue":151,"ChoiceName":"solifluctate","ChoiceLabel":"Solifluctate","ChoiceObsolete":1,"ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":165,"ChoiceValue":152,"ChoiceName":"till, subglacial","ChoiceLabel":"Subglacial till","ChoiceObsolete":0,"ChoiceDescription":"Till deposited in or by the bottom parts of a glacier or ice sheet; types include lodgement till, subglacial flow till; synonym (not preferred; obsolete): basal till. SW & GM","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":153,"ChoiceName":"complex landslide deposits","ChoiceLabel":"Complex landslide deposits","ChoiceObsolete":0,"ChoiceDescription":"A category of mass movement processes, associated sediments (complex landslide deposit) or resultant landforms characterized by a composite of several mass movement processes none of which dominates or leaves a prevailing landform. Numerous types of complex landslides can be specified by naming the constituent processes evident (e.g. a complex earth spread - earth flow landslide). Compare - fall, topple, slide, lateral spread, flow, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":25,"ChoiceValue":154,"ChoiceName":"debris fall deposits","ChoiceLabel":"Debris fall deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (debris fall deposit) or resultant landform characterized by a rapid type of fall involving the relatively free, downslope movement or collapse of detached, unconsolidated material which falls freely through the air (lacks an underlying slip face); sediments have substantial proportions of both fine earth and coarse fragments; common along undercut stream banks. Compare - rock fall, soil fall, landslide. SW","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":28,"ChoiceValue":155,"ChoiceName":"debris spread deposits","ChoiceLabel":"Debris spread deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (debris spread deposit) or resultant landforms characterized by a very rapid type of spread dominated by lateral movement in a soil and rock mass resulting from liquefaction or plastic flow of underlying materials that may be extruded out between intact units; sediments have substantial proportions of both fine earth and coarse fragments. Compare - earth spread, rock spread, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":156,"ChoiceName":"debris topple deposits","ChoiceLabel":"Debris topple deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (debris topple deposit) or resultant landform characterized by a localized, very rapid type of topple in which large blocks of soil and rock material literally fall over, rotating outward over a low pivot point; sediments have substantial proportions of both fine earth and coarse fragments. Portions of the original material may remain intact, although reoriented, within the resulting debris pile. Compare - earth topple, rock topple, landslide. SW","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":35,"ChoiceValue":157,"ChoiceName":"earth spread deposits","ChoiceLabel":"Earth spread deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (earth spread deposit) or resultant landforms characterized by a very rapid type of spread dominated by lateral movement in a soil mass resulting from liquefaction or plastic flow of underlying materials that may be extruded out between intact units. Compare - debris spread, rock spread, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":36,"ChoiceValue":158,"ChoiceName":"earth topple deposits","ChoiceLabel":"Earth topple deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (earth topple deposit) or resultant landform characterized by a localized, very rapid type of topple in which large blocks of soil material literally fall over, rotating outward over a low pivot point; sediments < 2 mm predominate. Portions of the original material may remain intact, although reoriented, within the resulting deposit. Compare - debris topple, rock topple, landslide. SW","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":41,"ChoiceValue":159,"ChoiceName":"fall deposits","ChoiceLabel":"Fall deposits","ChoiceObsolete":0,"ChoiceDescription":"(a) A category of mass movement processes, associated sediments (fall deposit), or resultant landforms (e.g., rockfall, debris fall, soil fall) characterized by very rapid movement of a mass of rock or earth that travels mostly through the air by free fall, leaping, bounding, or rolling, with little or no interaction between one moving unit and another. Compare - topple, slide, lateral spread, flow, complex landslide, landslide. SW & DV; (b) The mass of material moved by a fall. GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":42,"ChoiceValue":160,"ChoiceName":"flow deposits","ChoiceLabel":"Flow deposits","ChoiceObsolete":0,"ChoiceDescription":"A category of mass movement processes, associated sediments (flow deposit) and landforms characterized by slow to very rapid downslope movement of unconsolidated material which, whether saturated or comparatively dry, behaves much as a viscous fluid as it moves. Types of flows can be specified based on the dominant particle size of sediments [i.e. debris flow (e.g., lahar), earth flow (creep, mudflow), rock fragment flow (e.g., rockfall avalanche), debris avalanche]. Compare - fall, topple, slide, lateral spread, complex landslide, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":52,"ChoiceValue":161,"ChoiceName":"greensands","ChoiceLabel":"Greensands","ChoiceObsolete":0,"ChoiceDescription":"a) An unconsolidated, near-shore marine sediment containing substantial amounts of dark greenish glauconite pellets, often mingled with clay or sand (quartz may form the dominant constituent); prominent in Cretaceous and Tertiary coastal plain strata of New Jersey, Delaware and Maryland; has been commercially mined for potassium fertilizer. The term is loosely applied to any glauconitic sediment. b) (Not Preferred - use glauconitic sandstone) A sandstone consisting of greensand that is commonly poorly cemented, and has a greenish color when unweathered but an orange or yellow color when weathered. Compare - glauconite pellets. SW","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":118,"ChoiceValue":162,"ChoiceName":"rock spread deposits","ChoiceLabel":"Rock spread deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rock spread deposit) or resultant landforms characterized by a very rapid type of spread dominated by lateral movement in a rock mass resulting from liquefaction or plastic flow of underlying materials that may be extruded out between intact units; rock bodies predominate. Compare - debris spread, earth spread, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":119,"ChoiceValue":163,"ChoiceName":"rock topple deposits","ChoiceLabel":"Rock topple deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rock topple deposit) or resultant landform characterized by a localized, very rapid type of fall in which large blocks of rock material literally fall over, rotating outward over a low pivot point; rock bodies predominate (little fine earth). Portions of the original material may remain intact, although reoriented, within the resulting deposit. Compare - earth topple, debris topple, landslide. SW","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":122,"ChoiceValue":164,"ChoiceName":"rotational debris slide deposits","ChoiceLabel":"Rotational debris slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rotational debris slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions of which remain largely intact and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass; sediments have substantial proportions of both fine earth and coarse fragments. The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare - rotational earth slide, rotational rock slide, translational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":123,"ChoiceValue":165,"ChoiceName":"rotational earth slide deposits","ChoiceLabel":"Rotational earth slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rotational earth slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions of which remain largely intact and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass; sediments predominantly fine earth (< 2 mm). The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare - rotational debris slide, rotational rock slide, translational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":124,"ChoiceValue":166,"ChoiceName":"rotational rock slide deposits","ChoiceLabel":"Rotational rock slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rotational rock slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely consolidated rock bodies, portions of which remain largely intact but reoriented, and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass. The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare - rotational debris slide, rotational earth slide, translational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":126,"ChoiceValue":167,"ChoiceName":"sand flow deposits","ChoiceLabel":"Sand flow deposits","ChoiceObsolete":0,"ChoiceDescription":"A flow of wet sand, as along banks of noncohesive clean sand that is subject to scour and to repeated fluctuations in pore-water pressure due to rise and fall of the tide. GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":149,"ChoiceValue":168,"ChoiceName":"slide deposits","ChoiceLabel":"Slide deposits","ChoiceObsolete":0,"ChoiceDescription":"A category of mass movement processes, associated sediments (slide deposit) or resultant landforms (e.g., rotational slide, translational slide, and snowslide) characterized by a failure of earth, snow, or rock under shear stress along one or several surfaces that are either visible or may reasonably be inferred. The moving mass may or may not be greatly deformed, and movement may be rotational (rotational slide) or planar (translational slide). A slide can result from lateral erosion, lateral pressure, weight of overlying material, accumulation of moisture, earthquakes, expansion owing to freeze-thaw of water in cracks, regional tilting, undermining, fire, and human agencies. Compare -fall, topple, lateral spread, flow, complex landslide. SW & DV (b) The track of bare rock or furrowed earth left by a slide. (c) The mass of material moved in or deposited by a slide. Compare - fall, flow, complex landslide, landslide. SW & GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":151,"ChoiceValue":169,"ChoiceName":"slump block","ChoiceLabel":"Slump block","ChoiceObsolete":0,"ChoiceDescription":"TheA mass of material torn away as a coherent unit during a landslide; a largely intact but displaced and commonly reoriented body of rock or soil. SW & GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":155,"ChoiceValue":170,"ChoiceName":"solifluction deposits","ChoiceLabel":"Solifluction deposits","ChoiceObsolete":0,"ChoiceDescription":"A deposit of nonsorted, water-saturated, locally derived earthy material that is moving or has moved downslope, en masse, caused by the melting of seasonal frost or permafrost.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":173,"ChoiceValue":171,"ChoiceName":"translational slide deposits","ChoiceLabel":"Translational slide deposits","ChoiceObsolete":0,"ChoiceDescription":"A category of mass movement processes, associated sediments (translational slide deposit) or resultant landforms characterized by the extremely slow to moderately rapid downslope displacement of comparatively dry soil-rock material on a surface (slip face) that is roughly parallel to the general ground surface, in contrast to falls topples, and rotational slides. The term includes such diverse slide types as translational debris slides, translational earth slide, translational rock slide, block glides, and slab or flake slides. . Compare - rotational slide, slide, landslide. SW, DV, GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":170,"ChoiceValue":172,"ChoiceName":"translational debris slide deposits","ChoiceLabel":"Translational debris slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (translational debris slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions or blocks of which remain largely intact and in which movement occurs along a well-defined, planar slip face roughly parallel to the ground surface and resulting in lateral displacement but no rotation of the displaced mass; sediments have substantial proportions of both fine earth and coarse fragments. The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare - translational earth slide, translational rock slide, rotational slide lateral spread, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":171,"ChoiceValue":173,"ChoiceName":"translational earth slide deposits","ChoiceLabel":"Translational earth slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (translational earth slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions or blocks of which remain largely intact and in which movement occurs along a well-defined, planar slip face roughly parallel to the ground surface and resulting in lateral displacement but no rotation of the displaced mass; sediments predominantly fine earth (< 2 mm). The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare translational debris slide, translational rock slide, rotational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":172,"ChoiceValue":174,"ChoiceName":"translational rock slide deposits","ChoiceLabel":"Translational rock slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (translational rock slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely consolidated rock bodies, portions or blocks of which remain largely intact and in which movement occurs along a well-defined, planar slip face roughly parallel to the ground surface and resulting in lateral displacement but no rotation of the displaced mass; sediments predominantly fine earth (< 2 mm). The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare translational debris slide, translational earth slide, rotational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":114,"ChoiceValue":175,"ChoiceName":"pyroclastic flow","ChoiceLabel":"Pyroclastic flow","ChoiceObsolete":0,"ChoiceDescription":"A fast density current of pyroclastic material, usually very hot, composed of a mixture of gasses and a variety of pyroclastic particles (ash, pumice, scoria, lava fragments, etc.); produced by the explosive disintegration of viscous lava in a volcanic crater or by the explosive emission of gas-charged ash from a fissure and which tends to follow topographic lows (e.g. valleys) as it moves; used in a more general sense than ash flow. Compare - pyroclastic surge, ash flow, nue ardente, lahar. SW, SN, GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":115,"ChoiceValue":176,"ChoiceName":"pyroclastic surge","ChoiceLabel":"Pyroclastic surge","ChoiceObsolete":0,"ChoiceDescription":"A low density, dilute, turbulent pyroclastic flow, usually very hot, composed of a generally unsorted mixture of gases, ash, pumice and dense rock fragments that travels across the ground at high speed and less constrained by topography than a pyroclastic flow; several types of pyroclastic surges can be specified (e.g. base surge, ash-cloud-surge). Compare - pyroclastic flow. SW, SN, GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":43,"ChoiceValue":177,"ChoiceName":"fluviomarine deposits","ChoiceLabel":"Fluviomarine deposits","ChoiceObsolete":0,"ChoiceDescription":"Stratified materials (clay, silt, sand, or gravel) formed by both marine and fluvial processes, resulting from sea level flucuations and stream migration (i.e. materials originally deposited in a nearshore environment and subsequently reworked by fluvial processes as sea level fell, or vice versa as sea level rose).","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":92,"ChoiceValue":178,"ChoiceName":"mine spoil, coal extraction","ChoiceLabel":"Coal extraction mine spoil","ChoiceObsolete":0,"ChoiceDescription":"Randomly mixed, earthy materials artificially deposited as a result of either surficial or underground coal mining activities.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":93,"ChoiceValue":179,"ChoiceName":"mine spoil, metal ore extraction","ChoiceLabel":"Metal ore extraction mine spoil","ChoiceObsolete":0,"ChoiceDescription":"Randomly mixed, earthy materials artificially deposited as a result of either surficial or underground metal-ore mining activities.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":33,"ChoiceValue":180,"ChoiceName":"dredge spoils","ChoiceLabel":"Dredge spoils","ChoiceObsolete":0,"ChoiceDescription":"Unconsolidated, randomly mixed sediments extracted and deposited during dredging and dumping activities (e.g. adjoining the Intracoastal Waterway). Dredge spoils lie unconformably upon natural, undisturbed soil or regolith and can form anthropogenic landforms (e.g. dredge spoil bank).","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":68,"ChoiceValue":181,"ChoiceName":"lagoonal deposits","ChoiceLabel":"Lagoonal deposits","ChoiceObsolete":0,"ChoiceDescription":"Sand, silt or clay-sized sediments transported and deposited by wind, currents, and storm washover in the relatively low-energy, brackish to saline, shallow waters of a lagoon. Compare - marine deposit.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":182,"ChoiceName":"coastal marl","ChoiceLabel":"Coastal marl","ChoiceObsolete":0,"ChoiceDescription":"An earthy, unconsolidated deposit of gray to buff-colored mud of low bulk density (dry) composed primarily of very fine, almost pure calcium carbonate formed in subaqueous settings that span freshwater lacustrine conditions (e.g. Florida Everglades) to saline intertidal settings (e.g. Florida Keys) formed by the chemical action of algal mats and organic detritus (periphyton); other marl varieties associated with different environments (e.g. freshwater marl, glauconitic marl) also occur. Coastal marl can be quite pure or it can be finely disseminated throughout living root mats (e.g. mangrove roots) and / or organic soil layers. Compare marl, freshwater marl.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":44,"ChoiceValue":183,"ChoiceName":"freshwater marl","ChoiceLabel":"Freshwater marl","ChoiceObsolete":0,"ChoiceDescription":"A soft, grayish to white, earthy or powdery, usually impure calcium carbonate precipitated on the bottoms of present-day freshwater lakes and ponds largely through the chemical action of algal mats and organic detritus, or forming deposits that underlie marshes, swamps, and bogs that occupy the sites of former (glacial) lakes. The calcium carbonate may range from 90% to less than 30%. Freshwater marl is usually gray; it has been used as a fertilizer for acid soils deficient in lime. Syn.: bog lime. Compare marl, coastal marl.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":55,"ChoiceValue":184,"ChoiceName":"human-transported material","ChoiceLabel":"Human-transported material","ChoiceObsolete":0,"ChoiceDescription":"Organic or mineral soil material (or any other material that can function as a soil material) that has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. There has been little or no subsequent reworking by wind, gravity, water, or ice. Human transported materials are most commonly associated with building sites, mining or dredging operations, land fills, or other similar activities that result in the formation of a constructional anthropogenic landform.","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":185,"ChoiceName":"bauxite","ChoiceLabel":"Bauxite","ChoiceObsolete":0,"ChoiceDescription":"An off-white to dark red brown weathered detritus or rock composed of aluminum oxides (mainly gibbsite with some boehmite and diaspore), iron hydroxides, silica, silt, and especially clay minerals. Bauxite originates in tropical and subtropical environments as highly weathered residue from carbonate or silicate rocks and can occur in concretionary, earthy, pisolitic or oolitic forms. SW & GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":54,"ChoiceValue":186,"ChoiceName":"gypsite","ChoiceLabel":"Gypsite","ChoiceObsolete":0,"ChoiceDescription":"An earthy gypsum (CaSO4.2H2O) variety that contains various quantities (i.e. < 50%) of soil material, silicate clay minerals and sometimes other salts (e.g. NaCl); found only in arid or semi-arid regions as secondary precipitation concentrations or efflorescence associated with rock gypsum or gypsum-bearing strata. Compare rock gypsum, rock anhydrite. SW & GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":81,"ChoiceValue":187,"ChoiceName":"limonite","ChoiceLabel":"Limonite","ChoiceObsolete":0,"ChoiceDescription":"A general 'field' term for various brown to yellowish brown, amorphous- to- cryptocrystalline hydrous ferric oxides that are an undetermined mixture of goethite, hematite, and lepidocrocite formed by weathering and iron oxidation from iron-bearing, rocks and minerals. SW & GG","ColumnPhysicalName":"osdpmkind","ColumnLogicalName":"osd_parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":127,"ChoiceValue":1,"ChoiceName":"sandstone","ChoiceLabel":"sandstone","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":129,"ChoiceValue":2,"ChoiceName":"sandstone-noncalcareous","ChoiceLabel":"sandstone-noncalcareous","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"arkosic-sandstone","ChoiceLabel":"arkosic-sandstone","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":128,"ChoiceValue":4,"ChoiceName":"sandstone-calcareous","ChoiceLabel":"sandstone-calcareous","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":66,"ChoiceValue":5,"ChoiceName":"interbedded sedimentary","ChoiceLabel":"interbedded sedimentary","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":78,"ChoiceValue":6,"ChoiceName":"limestone-sandstone-shale","ChoiceLabel":"limestone-sandstone-shale","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":77,"ChoiceValue":7,"ChoiceName":"limestone-sandstone","ChoiceLabel":"limestone-sandstone","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":79,"ChoiceValue":8,"ChoiceName":"limestone-shale","ChoiceLabel":"limestone-shale","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":80,"ChoiceValue":9,"ChoiceName":"limestone-siltstone","ChoiceLabel":"limestone-siltstone","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":130,"ChoiceValue":10,"ChoiceName":"sandstone-shale","ChoiceLabel":"sandstone-shale","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":131,"ChoiceValue":11,"ChoiceName":"sandstone-siltstone","ChoiceLabel":"sandstone-siltstone","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":144,"ChoiceValue":12,"ChoiceName":"shale-siltstone","ChoiceLabel":"shale-siltstone","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":13,"ChoiceName":"conglomerate","ChoiceLabel":"conglomerate","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":14,"ChoiceName":"conglomerate-noncalcareous","ChoiceLabel":"conglomerate-noncalcareous","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":15,"ChoiceName":"conglomerate-calcareous","ChoiceLabel":"conglomerate-calcareous","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":180,"ChoiceValue":16,"ChoiceName":"volcanic ash","ChoiceLabel":"Volcanic ash","ChoiceObsolete":0,"ChoiceDescription":"Unconsolidated, pyroclastic material less than 2 mm in all dimensions.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":181,"ChoiceValue":17,"ChoiceName":"volcanic ash, acidic","ChoiceLabel":"Acidic volcanic ash","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":184,"ChoiceValue":18,"ChoiceName":"volcanic ash, basic","ChoiceLabel":"Basic volcanic ash","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":183,"ChoiceValue":19,"ChoiceName":"volcanic ash, basaltic","ChoiceLabel":"Basaltic volcanic ash","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":182,"ChoiceValue":20,"ChoiceName":"volcanic ash, andesitic","ChoiceLabel":"Andesitic volcanic ash","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":21,"ChoiceName":"cinders","ChoiceLabel":"Cinders","ChoiceObsolete":0,"ChoiceDescription":"Uncemented vitric, vesicular, pyroclastic material, more than 2.0 mm in at least one dimension, with an apparent specific gravity (including vesicles) of more than 1.0 and less than 2.0.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":112,"ChoiceValue":22,"ChoiceName":"pumice","ChoiceLabel":"Pumice","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":136,"ChoiceValue":23,"ChoiceName":"scoria","ChoiceLabel":"Scoria","ChoiceObsolete":0,"ChoiceDescription":"Vesicular, cindery crust or bomb-sized fragments of such material on the surface of andesitic or basaltic lava, the vesicular nature of which is due to the escape of volcanic gases before solidification; it is usually heavier, darker, and more crystalline than pumice. Synonym - cinder.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":185,"ChoiceValue":24,"ChoiceName":"volcanic bombs","ChoiceLabel":"Volcanic bombs","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":140,"ChoiceValue":25,"ChoiceName":"shale","ChoiceLabel":"shale","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":143,"ChoiceValue":26,"ChoiceName":"shale-noncalcareous","ChoiceLabel":"shale-noncalcareous","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":141,"ChoiceValue":27,"ChoiceName":"shale-calcareous","ChoiceLabel":"shale-calcareous","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":142,"ChoiceValue":28,"ChoiceName":"shale-clay","ChoiceLabel":"shale-clay","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":56,"ChoiceValue":29,"ChoiceName":"igneous","ChoiceLabel":"igneous","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":61,"ChoiceValue":30,"ChoiceName":"igneous-coarse (or 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Tephra is a general term which, unlike many volcaniclastic terms, does not denote properties of composition, visicularity, or grain size.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":159,"ChoiceValue":113,"ChoiceName":"till, ablation","ChoiceLabel":"Ablation till","ChoiceObsolete":0,"ChoiceDescription":"A general term for loose, relatively permeable material deposited during the downwasting of nearly static glacial ice, either contained within or accumulated on the surface of the glacier.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":160,"ChoiceValue":114,"ChoiceName":"till, basal","ChoiceLabel":"Basal till","ChoiceObsolete":0,"ChoiceDescription":"Unconsolidated material of mixed composition deposited at the base (bottom) of a glacier [ The term emphaizes the e.g. subglacial till. Types of basal till include lodgment, melt-out, and flow till.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":161,"ChoiceValue":115,"ChoiceName":"till, flow","ChoiceLabel":"Flow till","ChoiceObsolete":0,"ChoiceDescription":"A till, commonly supraglacial, that is modified and transported by plastic mass flow; also spelled flow till. Compare - ablation till, basal till, lodgment till, mass-movement till, slump-till, supraglacial melt-out till.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":162,"ChoiceValue":116,"ChoiceName":"till, lodgment","ChoiceLabel":"Lodgment till","ChoiceObsolete":0,"ChoiceDescription":"A basal till commonly characterized by compact, fissile (\"platy\") structure and containing coarse fragments oriented with their long axes generally parallel to the direction of ice movement.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":163,"ChoiceValue":117,"ChoiceName":"till, melt-out","ChoiceLabel":"Melt-out till","ChoiceObsolete":0,"ChoiceDescription":"Till derived from slow melting of debris-rich stagnant ice buried beneath sufficient overburden to inhibit deformation under gravity, thus preserving structures derived from the parent ice.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":164,"ChoiceValue":118,"ChoiceName":"till, slump","ChoiceLabel":"Slump till","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":166,"ChoiceValue":119,"ChoiceName":"till, supraglacial","ChoiceLabel":"Supraglacial till","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":168,"ChoiceValue":120,"ChoiceName":"till, unspecified","ChoiceLabel":"Till","ChoiceObsolete":0,"ChoiceDescription":"Dominantly unsorted and unstratified drift, generally unconsolidated and deposited directly by a glacier without subsequent reworking by meltwater, and consisting of a heterogeneous mixture of clay, silt, sand, gravel, stones, and boulders; rock fragments of various lithologies are imbedded within a finer matrix that can range from clay to sandy loam. Compare - ablation till, basal till, flowtill, lodgment till, drift, moraine.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":179,"ChoiceValue":121,"ChoiceName":"valley side alluvium","ChoiceLabel":"Valley side alluvium","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":156,"ChoiceValue":122,"ChoiceName":"supraglacial debris-flow","ChoiceLabel":"Supraglacial debris-flow","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":167,"ChoiceValue":123,"ChoiceName":"till, supraglacial meltout","ChoiceLabel":"Supraglacial meltout till","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":124,"ChoiceName":"backswamp deposits","ChoiceLabel":"Backswamp deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":108,"ChoiceValue":125,"ChoiceName":"overbank deposits","ChoiceLabel":"Overbank deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":101,"ChoiceValue":126,"ChoiceName":"mudflow deposits","ChoiceLabel":"Mudflow deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":127,"ChoiceName":"block glide deposits","ChoiceLabel":"Block glide deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":128,"ChoiceName":"creep deposits","ChoiceLabel":"Creep deposits","ChoiceObsolete":0,"ChoiceDescription":"Sediment resulting from slow mass movement of earth material down slopes, caused by gravity but facilitated by saturation with water and alternate freezing and thawing.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":129,"ChoiceName":"debris avalanche deposits","ChoiceLabel":"Debris avalanche deposits","ChoiceObsolete":0,"ChoiceDescription":"Sediment resulting from the very rapid and usually sudden sliding and flow of incoherent, unsorted mixtures of soil and weathered bedrock.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":130,"ChoiceName":"debris flow deposits","ChoiceLabel":"Debris flow deposits","ChoiceObsolete":0,"ChoiceDescription":"Sediment resulting from a mass movement of rock fragments, soil, mud, more than half of the particles being larger than sand size.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":27,"ChoiceValue":131,"ChoiceName":"debris slide deposits","ChoiceLabel":"Debris slide deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":37,"ChoiceValue":132,"ChoiceName":"earthflow deposits","ChoiceLabel":"Earthflow deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":71,"ChoiceValue":133,"ChoiceName":"lateral spread deposits","ChoiceLabel":"Lateral spread deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":121,"ChoiceValue":134,"ChoiceName":"rockfall deposits","ChoiceLabel":"Rockfall deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":120,"ChoiceValue":135,"ChoiceName":"rockfall avalanche deposits","ChoiceLabel":"Rockfall avalanche deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":125,"ChoiceValue":136,"ChoiceName":"rotational slide deposits","ChoiceLabel":"Rotational slide deposits","ChoiceObsolete":0,"ChoiceDescription":"An accumlation of sediment resulting from a mass movement and a process characterized by a slide in which shearing takes place on a well defined, curved shear surface, concave upward, producing a backward rotation in the displaced mass.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":137,"ChoiceValue":137,"ChoiceName":"scree","ChoiceLabel":"Scree","ChoiceObsolete":0,"ChoiceDescription":"A collective term for an accumulation of coarse rock debris or a sheet of coarse debris mantling a slope. Scree is not a synonym of talus, as scree includes loose, coarse fragment material on slopes without cliffs.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":152,"ChoiceValue":138,"ChoiceName":"soil fall deposits","ChoiceLabel":"Soil fall deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":157,"ChoiceValue":139,"ChoiceName":"talus","ChoiceLabel":"Talus","ChoiceObsolete":0,"ChoiceDescription":"Rock fragments of any size or shape (usually coarse and angular) derived from and lying at the base of a cliff or very steep rock slope. The accumulated mass of such loose broken rock formed chiefly by falling, rolling, or sliding.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":169,"ChoiceValue":140,"ChoiceName":"topple deposits","ChoiceLabel":"Topple deposits","ChoiceObsolete":0,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":53,"ChoiceValue":141,"ChoiceName":"grus","ChoiceLabel":"Grus","ChoiceObsolete":0,"ChoiceDescription":"The fragmental products of in situ granular disintegration of granite and granitic rocks, dominated by inter-crystal disintegration.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":132,"ChoiceValue":142,"ChoiceName":"saprolite","ChoiceLabel":"Saprolite","ChoiceObsolete":0,"ChoiceDescription":"- (Provisional definition) Soft, friable, isovolumetrically weathered bedrock that retains the fabric and structure of the parent rock (Colman and Dethier, 1986) exhibiting extensive inter-crystal and intra-crystal weathering. \r\n\r\nIn pedology, saprolite was formerly applied to any unconsolidated residual material underlying the soil and grading to hard bedrock below.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":39,"ChoiceValue":143,"ChoiceName":"eolian sands","ChoiceLabel":"Eolian sands","ChoiceObsolete":0,"ChoiceDescription":"Material transported and deposited by the wind, dominated by particles of sand-size (0.05-2 mm).","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":84,"ChoiceValue":144,"ChoiceName":"loess, noncalcareous","ChoiceLabel":"Noncalcareous loess","ChoiceObsolete":0,"ChoiceDescription":"Noncalcareous material transported and deposited by wind and consisting predominantly of silt size (0.002-0.05 mm).","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":110,"ChoiceValue":145,"ChoiceName":"parna","ChoiceLabel":"Parna","ChoiceObsolete":0,"ChoiceDescription":"A term used, especially in southeast Australia, for silt and sand-sized aggregates of eolian clay occurring in sheets.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":69,"ChoiceValue":146,"ChoiceName":"lahar deposits","ChoiceLabel":"Lahar deposits","ChoiceObsolete":0,"ChoiceDescription":"Unconsolidated volcaniclastic material emplaced as mudflows on or near the flanks of a volcano.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":70,"ChoiceValue":147,"ChoiceName":"lapilli","ChoiceLabel":"Lapilli","ChoiceObsolete":0,"ChoiceDescription":"Non or slightly vesicular pyroclastics, 2.0 to 76 mm in at least one dimension, with an apparent specific gravity of 2.0 or more.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":148,"ChoiceName":"ash flow (pyroclastic)","ChoiceLabel":"Ash flow","ChoiceObsolete":0,"ChoiceDescription":"A highly heated mixture of volcanic gases and ash, traveling down the flank of a volcano or along the surface of the ground; produced by the explosive disintegration of viscous lava in a volcanic crater, or by the explosive emission of gas-charged ash from a fissure or group of fissures. The solid materials contained in a typical ash flow are generally unsorted and ordinarily include volcanic dust, pumice, scoria, and blocks in addition to ash.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":153,"ChoiceValue":149,"ChoiceName":"solid rock","ChoiceLabel":"Solid rock","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":178,"ChoiceValue":150,"ChoiceName":"unconsolidated sediments","ChoiceLabel":"Unconsolidated sediments","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":154,"ChoiceValue":151,"ChoiceName":"solifluctate","ChoiceLabel":"Solifluctate","ChoiceObsolete":1,"ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":165,"ChoiceValue":152,"ChoiceName":"till, subglacial","ChoiceLabel":"Subglacial till","ChoiceObsolete":0,"ChoiceDescription":"Till deposited in or by the bottom parts of a glacier or ice sheet; types include lodgement till, subglacial flow till; synonym (not preferred; obsolete): basal till. SW & GM","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":153,"ChoiceName":"complex landslide deposits","ChoiceLabel":"Complex landslide deposits","ChoiceObsolete":0,"ChoiceDescription":"A category of mass movement processes, associated sediments (complex landslide deposit) or resultant landforms characterized by a composite of several mass movement processes none of which dominates or leaves a prevailing landform. Numerous types of complex landslides can be specified by naming the constituent processes evident (e.g. a complex earth spread - earth flow landslide). Compare - fall, topple, slide, lateral spread, flow, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":25,"ChoiceValue":154,"ChoiceName":"debris fall deposits","ChoiceLabel":"Debris fall deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (debris fall deposit) or resultant landform characterized by a rapid type of fall involving the relatively free, downslope movement or collapse of detached, unconsolidated material which falls freely through the air (lacks an underlying slip face); sediments have substantial proportions of both fine earth and coarse fragments; common along undercut stream banks. Compare - rock fall, soil fall, landslide. SW","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":28,"ChoiceValue":155,"ChoiceName":"debris spread deposits","ChoiceLabel":"Debris spread deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (debris spread deposit) or resultant landforms characterized by a very rapid type of spread dominated by lateral movement in a soil and rock mass resulting from liquefaction or plastic flow of underlying materials that may be extruded out between intact units; sediments have substantial proportions of both fine earth and coarse fragments. Compare - earth spread, rock spread, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":156,"ChoiceName":"debris topple deposits","ChoiceLabel":"Debris topple deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (debris topple deposit) or resultant landform characterized by a localized, very rapid type of topple in which large blocks of soil and rock material literally fall over, rotating outward over a low pivot point; sediments have substantial proportions of both fine earth and coarse fragments. Portions of the original material may remain intact, although reoriented, within the resulting debris pile. Compare - earth topple, rock topple, landslide. SW","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":35,"ChoiceValue":157,"ChoiceName":"earth spread deposits","ChoiceLabel":"Earth spread deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (earth spread deposit) or resultant landforms characterized by a very rapid type of spread dominated by lateral movement in a soil mass resulting from liquefaction or plastic flow of underlying materials that may be extruded out between intact units. Compare - debris spread, rock spread, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":36,"ChoiceValue":158,"ChoiceName":"earth topple deposits","ChoiceLabel":"Earth topple deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (earth topple deposit) or resultant landform characterized by a localized, very rapid type of topple in which large blocks of soil material literally fall over, rotating outward over a low pivot point; sediments < 2 mm predominate. Portions of the original material may remain intact, although reoriented, within the resulting deposit. Compare - debris topple, rock topple, landslide. SW","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":41,"ChoiceValue":159,"ChoiceName":"fall deposits","ChoiceLabel":"Fall deposits","ChoiceObsolete":0,"ChoiceDescription":"(a) A category of mass movement processes, associated sediments (fall deposit), or resultant landforms (e.g., rockfall, debris fall, soil fall) characterized by very rapid movement of a mass of rock or earth that travels mostly through the air by free fall, leaping, bounding, or rolling, with little or no interaction between one moving unit and another. Compare - topple, slide, lateral spread, flow, complex landslide, landslide. SW & DV; (b) The mass of material moved by a fall. GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":42,"ChoiceValue":160,"ChoiceName":"flow deposits","ChoiceLabel":"Flow deposits","ChoiceObsolete":0,"ChoiceDescription":"A category of mass movement processes, associated sediments (flow deposit) and landforms characterized by slow to very rapid downslope movement of unconsolidated material which, whether saturated or comparatively dry, behaves much as a viscous fluid as it moves. Types of flows can be specified based on the dominant particle size of sediments [i.e. debris flow (e.g., lahar), earth flow (creep, mudflow), rock fragment flow (e.g., rockfall avalanche), debris avalanche]. Compare - fall, topple, slide, lateral spread, complex landslide, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":52,"ChoiceValue":161,"ChoiceName":"greensands","ChoiceLabel":"Greensands","ChoiceObsolete":0,"ChoiceDescription":"a) An unconsolidated, near-shore marine sediment containing substantial amounts of dark greenish glauconite pellets, often mingled with clay or sand (quartz may form the dominant constituent); prominent in Cretaceous and Tertiary coastal plain strata of New Jersey, Delaware and Maryland; has been commercially mined for potassium fertilizer. The term is loosely applied to any glauconitic sediment. b) (Not Preferred - use glauconitic sandstone) A sandstone consisting of greensand that is commonly poorly cemented, and has a greenish color when unweathered but an orange or yellow color when weathered. Compare - glauconite pellets. SW","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":118,"ChoiceValue":162,"ChoiceName":"rock spread deposits","ChoiceLabel":"Rock spread deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rock spread deposit) or resultant landforms characterized by a very rapid type of spread dominated by lateral movement in a rock mass resulting from liquefaction or plastic flow of underlying materials that may be extruded out between intact units; rock bodies predominate. Compare - debris spread, earth spread, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":119,"ChoiceValue":163,"ChoiceName":"rock topple deposits","ChoiceLabel":"Rock topple deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rock topple deposit) or resultant landform characterized by a localized, very rapid type of fall in which large blocks of rock material literally fall over, rotating outward over a low pivot point; rock bodies predominate (little fine earth). Portions of the original material may remain intact, although reoriented, within the resulting deposit. Compare - earth topple, debris topple, landslide. SW","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":122,"ChoiceValue":164,"ChoiceName":"rotational debris slide deposits","ChoiceLabel":"Rotational debris slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rotational debris slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions of which remain largely intact and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass; sediments have substantial proportions of both fine earth and coarse fragments. The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare - rotational earth slide, rotational rock slide, translational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":123,"ChoiceValue":165,"ChoiceName":"rotational earth slide deposits","ChoiceLabel":"Rotational earth slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rotational earth slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions of which remain largely intact and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass; sediments predominantly fine earth (< 2 mm). The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare - rotational debris slide, rotational rock slide, translational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":124,"ChoiceValue":166,"ChoiceName":"rotational rock slide deposits","ChoiceLabel":"Rotational rock slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (rotational rock slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely consolidated rock bodies, portions of which remain largely intact but reoriented, and in which movement occurs along a well-defined, concave shear surface and resulting in a backward rotation of the displaced mass. The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare - rotational debris slide, rotational earth slide, translational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":126,"ChoiceValue":167,"ChoiceName":"sand flow deposits","ChoiceLabel":"Sand flow deposits","ChoiceObsolete":0,"ChoiceDescription":"A flow of wet sand, as along banks of noncohesive clean sand that is subject to scour and to repeated fluctuations in pore-water pressure due to rise and fall of the tide. GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":149,"ChoiceValue":168,"ChoiceName":"slide deposits","ChoiceLabel":"Slide deposits","ChoiceObsolete":0,"ChoiceDescription":"A category of mass movement processes, associated sediments (slide deposit) or resultant landforms (e.g., rotational slide, translational slide, and snowslide) characterized by a failure of earth, snow, or rock under shear stress along one or several surfaces that are either visible or may reasonably be inferred. The moving mass may or may not be greatly deformed, and movement may be rotational (rotational slide) or planar (translational slide). A slide can result from lateral erosion, lateral pressure, weight of overlying material, accumulation of moisture, earthquakes, expansion owing to freeze-thaw of water in cracks, regional tilting, undermining, fire, and human agencies. Compare -fall, topple, lateral spread, flow, complex landslide. SW & DV (b) The track of bare rock or furrowed earth left by a slide. (c) The mass of material moved in or deposited by a slide. Compare - fall, flow, complex landslide, landslide. SW & GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":151,"ChoiceValue":169,"ChoiceName":"slump block","ChoiceLabel":"Slump block","ChoiceObsolete":0,"ChoiceDescription":"TheA mass of material torn away as a coherent unit during a landslide; a largely intact but displaced and commonly reoriented body of rock or soil. SW & GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":155,"ChoiceValue":170,"ChoiceName":"solifluction deposits","ChoiceLabel":"Solifluction deposits","ChoiceObsolete":0,"ChoiceDescription":"A deposit of nonsorted, water-saturated, locally derived earthy material that is moving or has moved downslope, en masse, caused by the melting of seasonal frost or permafrost.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":173,"ChoiceValue":171,"ChoiceName":"translational slide deposits","ChoiceLabel":"Translational slide deposits","ChoiceObsolete":0,"ChoiceDescription":"A category of mass movement processes, associated sediments (translational slide deposit) or resultant landforms characterized by the extremely slow to moderately rapid downslope displacement of comparatively dry soil-rock material on a surface (slip face) that is roughly parallel to the general ground surface, in contrast to falls topples, and rotational slides. The term includes such diverse slide types as translational debris slides, translational earth slide, translational rock slide, block glides, and slab or flake slides. . Compare - rotational slide, slide, landslide. SW, DV, GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":170,"ChoiceValue":172,"ChoiceName":"translational debris slide deposits","ChoiceLabel":"Translational debris slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (translational debris slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions or blocks of which remain largely intact and in which movement occurs along a well-defined, planar slip face roughly parallel to the ground surface and resulting in lateral displacement but no rotation of the displaced mass; sediments have substantial proportions of both fine earth and coarse fragments. The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare - translational earth slide, translational rock slide, rotational slide lateral spread, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":171,"ChoiceValue":173,"ChoiceName":"translational earth slide deposits","ChoiceLabel":"Translational earth slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (translational earth slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely unconsolidated earthy material, portions or blocks of which remain largely intact and in which movement occurs along a well-defined, planar slip face roughly parallel to the ground surface and resulting in lateral displacement but no rotation of the displaced mass; sediments predominantly fine earth (< 2 mm). The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare translational debris slide, translational rock slide, rotational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":172,"ChoiceValue":174,"ChoiceName":"translational rock slide deposits","ChoiceLabel":"Translational rock slide deposits","ChoiceObsolete":0,"ChoiceDescription":"The process, associated sediments (translational rock slide deposit) or resultant landform characterized by an extremely slow to moderately rapid type of slide, composed of comparatively dry and largely consolidated rock bodies, portions or blocks of which remain largely intact and in which movement occurs along a well-defined, planar slip face roughly parallel to the ground surface and resulting in lateral displacement but no rotation of the displaced mass; sediments predominantly fine earth (< 2 mm). The landform may be single, successive (repeated up and down slope), or multiple (as the number of slide components increase). Compare translational debris slide, translational earth slide, rotational slide, lateral spread, landslide. SW & DV","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":114,"ChoiceValue":175,"ChoiceName":"pyroclastic flow","ChoiceLabel":"Pyroclastic flow","ChoiceObsolete":0,"ChoiceDescription":"A fast density current of pyroclastic material, usually very hot, composed of a mixture of gasses and a variety of pyroclastic particles (ash, pumice, scoria, lava fragments, etc.); produced by the explosive disintegration of viscous lava in a volcanic crater or by the explosive emission of gas-charged ash from a fissure and which tends to follow topographic lows (e.g. valleys) as it moves; used in a more general sense than ash flow. Compare - pyroclastic surge, ash flow, nue ardente, lahar. SW, SN, GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":115,"ChoiceValue":176,"ChoiceName":"pyroclastic surge","ChoiceLabel":"Pyroclastic surge","ChoiceObsolete":0,"ChoiceDescription":"A low density, dilute, turbulent pyroclastic flow, usually very hot, composed of a generally unsorted mixture of gases, ash, pumice and dense rock fragments that travels across the ground at high speed and less constrained by topography than a pyroclastic flow; several types of pyroclastic surges can be specified (e.g. base surge, ash-cloud-surge). Compare - pyroclastic flow. SW, SN, GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":43,"ChoiceValue":177,"ChoiceName":"fluviomarine deposits","ChoiceLabel":"Fluviomarine deposits","ChoiceObsolete":0,"ChoiceDescription":"Stratified materials (clay, silt, sand, or gravel) formed by both marine and fluvial processes, resulting from sea level flucuations and stream migration (i.e. materials originally deposited in a nearshore environment and subsequently reworked by fluvial processes as sea level fell, or vice versa as sea level rose).","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":92,"ChoiceValue":178,"ChoiceName":"mine spoil, coal extraction","ChoiceLabel":"Coal extraction mine spoil","ChoiceObsolete":0,"ChoiceDescription":"Randomly mixed, earthy materials artificially deposited as a result of either surficial or underground coal mining activities.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":93,"ChoiceValue":179,"ChoiceName":"mine spoil, metal ore extraction","ChoiceLabel":"Metal ore extraction mine spoil","ChoiceObsolete":0,"ChoiceDescription":"Randomly mixed, earthy materials artificially deposited as a result of either surficial or underground metal-ore mining activities.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":33,"ChoiceValue":180,"ChoiceName":"dredge spoils","ChoiceLabel":"Dredge spoils","ChoiceObsolete":0,"ChoiceDescription":"Unconsolidated, randomly mixed sediments extracted and deposited during dredging and dumping activities (e.g. adjoining the Intracoastal Waterway). Dredge spoils lie unconformably upon natural, undisturbed soil or regolith and can form anthropogenic landforms (e.g. dredge spoil bank).","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":68,"ChoiceValue":181,"ChoiceName":"lagoonal deposits","ChoiceLabel":"Lagoonal deposits","ChoiceObsolete":0,"ChoiceDescription":"Sand, silt or clay-sized sediments transported and deposited by wind, currents, and storm washover in the relatively low-energy, brackish to saline, shallow waters of a lagoon. Compare - marine deposit.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":182,"ChoiceName":"coastal marl","ChoiceLabel":"Coastal marl","ChoiceObsolete":0,"ChoiceDescription":"An earthy, unconsolidated deposit of gray to buff-colored mud of low bulk density (dry) composed primarily of very fine, almost pure calcium carbonate formed in subaqueous settings that span freshwater lacustrine conditions (e.g. Florida Everglades) to saline intertidal settings (e.g. Florida Keys) formed by the chemical action of algal mats and organic detritus (periphyton); other marl varieties associated with different environments (e.g. freshwater marl, glauconitic marl) also occur. Coastal marl can be quite pure or it can be finely disseminated throughout living root mats (e.g. mangrove roots) and / or organic soil layers. Compare marl, freshwater marl.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":44,"ChoiceValue":183,"ChoiceName":"freshwater marl","ChoiceLabel":"Freshwater marl","ChoiceObsolete":0,"ChoiceDescription":"A soft, grayish to white, earthy or powdery, usually impure calcium carbonate precipitated on the bottoms of present-day freshwater lakes and ponds largely through the chemical action of algal mats and organic detritus, or forming deposits that underlie marshes, swamps, and bogs that occupy the sites of former (glacial) lakes. The calcium carbonate may range from 90% to less than 30%. Freshwater marl is usually gray; it has been used as a fertilizer for acid soils deficient in lime. Syn.: bog lime. Compare marl, coastal marl.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":55,"ChoiceValue":184,"ChoiceName":"human-transported material","ChoiceLabel":"Human-transported material","ChoiceObsolete":0,"ChoiceDescription":"Organic or mineral soil material (or any other material that can function as a soil material) that has been moved horizontally onto a pedon from a source area outside of that pedon by directed human activity, usually with the aid of machinery. There has been little or no subsequent reworking by wind, gravity, water, or ice. Human transported materials are most commonly associated with building sites, mining or dredging operations, land fills, or other similar activities that result in the formation of a constructional anthropogenic landform.","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":185,"ChoiceName":"bauxite","ChoiceLabel":"Bauxite","ChoiceObsolete":0,"ChoiceDescription":"An off-white to dark red brown weathered detritus or rock composed of aluminum oxides (mainly gibbsite with some boehmite and diaspore), iron hydroxides, silica, silt, and especially clay minerals. Bauxite originates in tropical and subtropical environments as highly weathered residue from carbonate or silicate rocks and can occur in concretionary, earthy, pisolitic or oolitic forms. SW & GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":54,"ChoiceValue":186,"ChoiceName":"gypsite","ChoiceLabel":"Gypsite","ChoiceObsolete":0,"ChoiceDescription":"An earthy gypsum (CaSO4.2H2O) variety that contains various quantities (i.e. < 50%) of soil material, silicate clay minerals and sometimes other salts (e.g. NaCl); found only in arid or semi-arid regions as secondary precipitation concentrations or efflorescence associated with rock gypsum or gypsum-bearing strata. Compare rock gypsum, rock anhydrite. SW & GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":515,"DomainName":"parent_material_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":81,"ChoiceValue":187,"ChoiceName":"limonite","ChoiceLabel":"Limonite","ChoiceObsolete":0,"ChoiceDescription":"A general 'field' term for various brown to yellowish brown, amorphous- to- cryptocrystalline hydrous ferric oxides that are an undetermined mixture of goethite, hematite, and lepidocrocite formed by weathering and iron oxidation from iron-bearing, rocks and minerals. SW & GG","ColumnPhysicalName":"pmkind","ColumnLogicalName":"parent_material_kind"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"clayey","ChoiceLabel":"Clayey","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is clay, sandy clay, or silty clay.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"coarse-loamy","ChoiceLabel":"Coarse-loamy","ChoiceObsolete":0,"ChoiceDescription":"The material contains less than 18 percent clay and 15 percent or more particles that are 0.1 to 75.0 mm in size. The soil texture class is loamy very fine sand, very fine sand, or finer.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"coarse-silty","ChoiceLabel":"Coarse-silty","ChoiceObsolete":0,"ChoiceDescription":"The material contains less than 18 percent clay and less than 15 percent particles that are 0.1 to 75.0 mm in size.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"fine-loamy","ChoiceLabel":"Fine-loamy","ChoiceObsolete":0,"ChoiceDescription":"The material contains 18 to 35 percent clay and 15 percent or more particles that are 0.1 to 75.0 mm in size.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"fine-silty","ChoiceLabel":"Fine-silty","ChoiceObsolete":0,"ChoiceDescription":"The material contains 18 to 35 percent clay and less than 15 percent particles that are 0.1 to 75.0 mm in size.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"gravelly","ChoiceLabel":"Gravelly","ChoiceObsolete":0,"ChoiceDescription":"The material contains 15 percent or more rock fragments.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"loamy","ChoiceLabel":"Loamy","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sandy loam, sandy clay loam, clay loam, silt, silt loam, or silty clay loam.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"sandy","ChoiceLabel":"Sandy","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sand or loamy sand.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"sandy and gravelly","ChoiceLabel":"Sandy and gravelly","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class contains sand or loamy sand, and the material contains 15 percent or more rock fragments.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"sandy and silty","ChoiceLabel":"Sandy and silty","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sand or loamy sand and silt or silt loam.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"silty","ChoiceLabel":"Silty","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is silt or silt loam.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"silty and clayey","ChoiceLabel":"Silty and clayey","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is silt or silt loam and clay, sandy clay, or silty clay.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"sandy and loamy","ChoiceLabel":"Sandy and loamy","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sand or loamy sand and sandy loam, sandy clay loam, clay loam, silt, silt loam, or silty clay loam.","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"loamy and clayey","ChoiceLabel":"Loamy and clayey","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sandy loam, sandy clay loam, clay loam, silt, silt loam, or silty clay loam and clay, sandy clay, or silty clay.\r\n","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"sandy and clayey","ChoiceLabel":"Sandy and clayey","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sand or loamy sand and clay, sandy clay, or silty clay.\r\n","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"coarse textured","ChoiceLabel":"Coarse textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is sands (coarse sand, sand, fine sand, very fine sand);loamy sands(loamy coarse sand, loamy sand, loamy fine sand, loamy very fine sand). SSM table 3.1","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"moderately coarse textured","ChoiceLabel":"Moderately coarse textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is coarse sandy loam, sandy loam, fine sandy loam. From table 3.1 SSM","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"medium textured","ChoiceLabel":"Medium textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is very fine sandy loam, loam, silt loam, silt. From table 3.1 SSM\r\n","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"moderately fine textured","ChoiceLabel":"Moderately fine textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is clay loam, sandy clay loam, silty clay loam. From table 3.1 SSM\r\n","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":20,"ChoiceName":"fine textured","ChoiceLabel":"Fine textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is sandy clay, silty clay, clay. From table 3.1 SSM","ColumnPhysicalName":"osdpmmodifier","ColumnLogicalName":"osd_parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"clayey","ChoiceLabel":"Clayey","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is clay, sandy clay, or silty clay.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"coarse-loamy","ChoiceLabel":"Coarse-loamy","ChoiceObsolete":0,"ChoiceDescription":"The material contains less than 18 percent clay and 15 percent or more particles that are 0.1 to 75.0 mm in size. The soil texture class is loamy very fine sand, very fine sand, or finer.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"coarse-silty","ChoiceLabel":"Coarse-silty","ChoiceObsolete":0,"ChoiceDescription":"The material contains less than 18 percent clay and less than 15 percent particles that are 0.1 to 75.0 mm in size.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"fine-loamy","ChoiceLabel":"Fine-loamy","ChoiceObsolete":0,"ChoiceDescription":"The material contains 18 to 35 percent clay and 15 percent or more particles that are 0.1 to 75.0 mm in size.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"fine-silty","ChoiceLabel":"Fine-silty","ChoiceObsolete":0,"ChoiceDescription":"The material contains 18 to 35 percent clay and less than 15 percent particles that are 0.1 to 75.0 mm in size.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"gravelly","ChoiceLabel":"Gravelly","ChoiceObsolete":0,"ChoiceDescription":"The material contains 15 percent or more rock fragments.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"loamy","ChoiceLabel":"Loamy","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sandy loam, sandy clay loam, clay loam, silt, silt loam, or silty clay loam.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"sandy","ChoiceLabel":"Sandy","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sand or loamy sand.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"sandy and gravelly","ChoiceLabel":"Sandy and gravelly","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class contains sand or loamy sand, and the material contains 15 percent or more rock fragments.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"sandy and silty","ChoiceLabel":"Sandy and silty","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sand or loamy sand and silt or silt loam.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"silty","ChoiceLabel":"Silty","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is silt or silt loam.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"silty and clayey","ChoiceLabel":"Silty and clayey","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is silt or silt loam and clay, sandy clay, or silty clay.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"sandy and loamy","ChoiceLabel":"Sandy and loamy","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sand or loamy sand and sandy loam, sandy clay loam, clay loam, silt, silt loam, or silty clay loam.","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"loamy and clayey","ChoiceLabel":"Loamy and clayey","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sandy loam, sandy clay loam, clay loam, silt, silt loam, or silty clay loam and clay, sandy clay, or silty clay.\r\n","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"sandy and clayey","ChoiceLabel":"Sandy and clayey","ChoiceObsolete":0,"ChoiceDescription":"The soil texture class is sand or loamy sand and clay, sandy clay, or silty clay.\r\n","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"coarse textured","ChoiceLabel":"Coarse textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is sands (coarse sand, sand, fine sand, very fine sand);loamy sands(loamy coarse sand, loamy sand, loamy fine sand, loamy very fine sand). SSM table 3.1","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"moderately coarse textured","ChoiceLabel":"Moderately coarse textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is coarse sandy loam, sandy loam, fine sandy loam. From table 3.1 SSM","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"medium textured","ChoiceLabel":"Medium textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is very fine sandy loam, loam, silt loam, silt. From table 3.1 SSM\r\n","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"moderately fine textured","ChoiceLabel":"Moderately fine textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is clay loam, sandy clay loam, silty clay loam. From table 3.1 SSM\r\n","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":516,"DomainName":"parent_material_modifier","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":20,"ChoiceName":"fine textured","ChoiceLabel":"Fine textured","ChoiceObsolete":0,"ChoiceDescription":"The soil texture is sandy clay, silty clay, clay. From table 3.1 SSM","ColumnPhysicalName":"pmmodifier","ColumnLogicalName":"parent_material_modifier"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":114,"ChoiceValue":1,"ChoiceName":"sandstone, unspecified","ChoiceLabel":"Sandstone","ChoiceObsolete":0,"ChoiceDescription":"Sedimentary rock containing dominantly sand-size clastic particles.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":113,"ChoiceValue":2,"ChoiceName":"sandstone, noncalcareous","ChoiceLabel":"Noncalcareous sandstone","ChoiceObsolete":1,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":3,"ChoiceName":"arkose","ChoiceLabel":"Arkose","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":111,"ChoiceValue":4,"ChoiceName":"sandstone, calcareous","ChoiceLabel":"Calcareous sandstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":62,"ChoiceValue":5,"ChoiceName":"interbedded sedimentary","ChoiceLabel":"Interbedded sedimentary rock","ChoiceObsolete":1,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":72,"ChoiceValue":6,"ChoiceName":"limestone, sandstone, and shale","ChoiceLabel":"Limestone, sandstone, and shale","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":64,"ChoiceValue":7,"ChoiceName":"limestone and sandstone","ChoiceLabel":"Limestone and sandstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":65,"ChoiceValue":8,"ChoiceName":"limestone and shale","ChoiceLabel":"Limestone and shale","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":66,"ChoiceValue":9,"ChoiceName":"limestone and siltstone","ChoiceLabel":"Limestone and siltstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":109,"ChoiceValue":10,"ChoiceName":"sandstone and shale","ChoiceLabel":"Sandstone and shale","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":110,"ChoiceValue":11,"ChoiceName":"sandstone and siltstone","ChoiceLabel":"Sandstone and siltstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":127,"ChoiceValue":12,"ChoiceName":"shale and siltstone","ChoiceLabel":"Shale and siltstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":13,"ChoiceName":"conglomerate, unspecified","ChoiceLabel":"Conglomerate","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":25,"ChoiceValue":14,"ChoiceName":"conglomerate, noncalcareous","ChoiceLabel":"Noncalcareous conglomerate","ChoiceObsolete":1,"ChoiceDescription":"A coarse-grained, clastic sedimentary rock composed of rounded to subangular rock fragments larger than 2 mm, commonly with a matrix of sand and finer material; cements include silica, calcium carbonate, and iron oxides. 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Compare - scoria, tephra.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":124,"ChoiceValue":23,"ChoiceName":"scoria","ChoiceLabel":"Scoria","ChoiceObsolete":0,"ChoiceDescription":"Vesicular, cindery crust or bomb-sized fragments of such material on the surface of andesitic or basaltic lava, the vesicular nature of which is due to the escape of volcanic gases before solidification; it is usually heavier, darker, and more crystalline than pumice. Synonym - cinder. 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Compare - intrusive, extrusive, metamorphic rock, sedimentary.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":56,"ChoiceValue":30,"ChoiceName":"igneous, coarse crystal","ChoiceLabel":"Coarse igneous crystal","ChoiceObsolete":1,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":55,"ChoiceValue":31,"ChoiceName":"igneous, basic","ChoiceLabel":"Basic igneous rock","ChoiceObsolete":1,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":58,"ChoiceValue":32,"ChoiceName":"igneous, intermediate","ChoiceLabel":"Intermediate igneous rock","ChoiceObsolete":1,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":44,"ChoiceValue":33,"ChoiceName":"granite","ChoiceLabel":"Granite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":57,"ChoiceValue":34,"ChoiceName":"igneous, fine crystal","ChoiceLabel":"Fine igneous crystal","ChoiceObsolete":1,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":35,"ChoiceName":"basalt","ChoiceLabel":"Basalt","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":36,"ChoiceName":"andesite","ChoiceLabel":"Andesite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":54,"ChoiceValue":37,"ChoiceName":"igneous, acid","ChoiceLabel":"Acid igneous rock","ChoiceObsolete":1,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":59,"ChoiceValue":38,"ChoiceName":"igneous, ultrabasic","ChoiceLabel":"Ultrabasic igneous rock","ChoiceObsolete":1,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":73,"ChoiceValue":39,"ChoiceName":"limestone, unspecified","ChoiceLabel":"Limestone","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock consisting chiefly (more than 50 percent) of calcium carbonate, primarily in the form of calcite. 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{"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":49,"ChoiceValue":88,"ChoiceName":"graywacke","ChoiceLabel":"Graywacke","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":51,"ChoiceValue":89,"ChoiceName":"gypsum, rock","ChoiceLabel":"Rock gypsum","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed primarily of mineral gypsum (CaSO4.2H2O). The rock is generally massive, ranges from coarse crystalline to fine granular, may show disturbed bedding due to hydration expansion of parent anhydrite (anhydrous CaSO4), and may exhibit rhythmic sedimentation (rhymites). Compare - gypsite. GG","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":128,"ChoiceValue":90,"ChoiceName":"shale, acid","ChoiceLabel":"Acid shale","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":101,"ChoiceValue":91,"ChoiceName":"porcellanite","ChoiceLabel":"Porcellanite","ChoiceObsolete":0,"ChoiceDescription":"An indurated or baked clay or shale with a dull, light-colored, cherty appearance, often found in the roof or floor of a burned-out coal seam.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":27,"ChoiceValue":92,"ChoiceName":"dacite","ChoiceLabel":"Dacite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":63,"ChoiceValue":93,"ChoiceName":"latite","ChoiceLabel":"Latite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":144,"ChoiceValue":94,"ChoiceName":"trachyte","ChoiceLabel":"Trachyte","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":28,"ChoiceValue":95,"ChoiceName":"diabase","ChoiceLabel":"Diabase","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":46,"ChoiceValue":96,"ChoiceName":"granodiorite","ChoiceLabel":"Granodiorite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":91,"ChoiceValue":97,"ChoiceName":"monzonite","ChoiceLabel":"Monzonite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":98,"ChoiceValue":98,"ChoiceName":"peridotite","ChoiceLabel":"Peridotite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":104,"ChoiceValue":99,"ChoiceName":"pyroxenite","ChoiceLabel":"Pyroxenite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":140,"ChoiceValue":100,"ChoiceName":"syenite","ChoiceLabel":"Syenite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":141,"ChoiceValue":101,"ChoiceName":"syenodiorite","ChoiceLabel":"Syenodiorite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":102,"ChoiceName":"amphibolite","ChoiceLabel":"Amphibolite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":47,"ChoiceValue":103,"ChoiceName":"granofels","ChoiceLabel":"Granofels","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":50,"ChoiceValue":104,"ChoiceName":"greenstone","ChoiceLabel":"Greenstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":79,"ChoiceValue":105,"ChoiceName":"metaquartzite","ChoiceLabel":"Metaquartzite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":82,"ChoiceValue":106,"ChoiceName":"metavolcanics","ChoiceLabel":"Metavolcanics","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":93,"ChoiceValue":107,"ChoiceName":"mylonite","ChoiceLabel":"Mylonite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":108,"ChoiceName":"arenite","ChoiceLabel":"Arenite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":109,"ChoiceName":"claystone","ChoiceLabel":"Claystone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":92,"ChoiceValue":110,"ChoiceName":"mudstone","ChoiceLabel":"Mudstone","ChoiceObsolete":0,"ChoiceDescription":"a) a blocky or massive, fine-grained sedimentary rock in which the proportions of clay and silt are approximately equal b) A general term that includes clay, silt, claystone, siltstone, shale, and argillite, and that should be used only when the amounts of clay and silt are not known or cannot be precisely identified.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":111,"ChoiceName":"chert","ChoiceLabel":"Chert","ChoiceObsolete":0,"ChoiceDescription":"A hard, extremely dense or compact, dull to semivitreous, cryptocrystalline sedimentary rock, consisting dominantly of interlocking crystals of quartz less than about 30 mm in diameter; it may contain amorphous silica (opal). It sometimes contains impurities such as calcite, iron oxide, or the remains of silicious and other organisims. It has a tough, splintery to conchoidal fracture and may be white or variously colored gray, green, blue, pink, red, yellow, brown, and black. Chet occurs principally as nodular or concretionary segregations in limestones and dolomites.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":145,"ChoiceValue":112,"ChoiceName":"travertine","ChoiceLabel":"Travertine","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":147,"ChoiceValue":113,"ChoiceName":"tufa","ChoiceLabel":"Tufa","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":61,"ChoiceValue":114,"ChoiceName":"ignimbrite","ChoiceLabel":"Ignimbrite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":115,"ChoiceName":"breccia, non-volcanic","ChoiceLabel":"Non-volcanic breccia","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":48,"ChoiceValue":116,"ChoiceName":"granulite","ChoiceLabel":"Granulite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":83,"ChoiceValue":117,"ChoiceName":"migmatite","ChoiceLabel":"Migmatite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":139,"ChoiceValue":118,"ChoiceName":"soapstone","ChoiceLabel":"Soapstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":119,"ChoiceName":"argillite","ChoiceLabel":"Argillite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":96,"ChoiceValue":120,"ChoiceName":"orthoquartzite","ChoiceLabel":"Orthoquartzite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":121,"ChoiceName":"anorthosite","ChoiceLabel":"Anorthosite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":122,"ChoiceName":"breccia, non-volcanic, acidic","ChoiceLabel":"Acidic Non-volcanic breccia","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":123,"ChoiceName":"breccia, non-volcanic, basic","ChoiceLabel":"Basic Non-volcanic breccia","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":33,"ChoiceValue":124,"ChoiceName":"fanglomerate","ChoiceLabel":"Fanglomerate","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":80,"ChoiceValue":125,"ChoiceName":"metasedimentary rock, unspecified","ChoiceLabel":"Metasedimentary rock","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":120,"ChoiceValue":126,"ChoiceName":"schist, mica","ChoiceLabel":"Mica schist","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":105,"ChoiceValue":127,"ChoiceName":"quartz-diorite","ChoiceLabel":"Quartz-diorite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":107,"ChoiceValue":128,"ChoiceName":"quartz-monzonite","ChoiceLabel":"Quartz-monzonite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":142,"ChoiceValue":129,"ChoiceName":"tachylite","ChoiceLabel":"Tachylite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":143,"ChoiceValue":130,"ChoiceName":"tonalite","ChoiceLabel":"Tonalite","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":153,"ChoiceValue":131,"ChoiceName":"ultramafic, unspecified","ChoiceLabel":"Ultramafic rock","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":152,"ChoiceValue":132,"ChoiceName":"tuff, welded","ChoiceLabel":"Welded tuff","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":115,"ChoiceValue":133,"ChoiceName":"sandstone, volcanic","ChoiceLabel":"Volcanic sandstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":134,"ChoiceName":"block lava","ChoiceLabel":"Block lava","ChoiceObsolete":0,"ChoiceDescription":"Lava having a surface of angular blocks; it is similar to a'a lava but the fragments are larger and more regular in shape, somewhat smoother, and less vesicular. Compare - `a`a lava, pahoehoe lava, pillow lava.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":100,"ChoiceValue":135,"ChoiceName":"pillow lava","ChoiceLabel":"Pillow lava","ChoiceObsolete":0,"ChoiceDescription":"A general term for lava displaying pillow structure (discontinuous, close-fitting, bun-shaped or ellipsoidal masses, generally < 1 m in diameter); considered to have formed in a subaqueous environment; such lava is usually basaltic or andesitic. Compare - `a`a lava, block lava, pahoehoe lava.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":112,"ChoiceValue":136,"ChoiceName":"sandstone, glauconitic","ChoiceLabel":"Glauconitic sandstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":146,"ChoiceValue":137,"ChoiceName":"tripoli","ChoiceLabel":"Tripoli","ChoiceObsolete":0,"ChoiceDescription":"A light-colored, porous, friable, siliceous (largely chalcedonic) sedimentary rock, which occurs in powdery or earthy masses that result from the weathering of siliceous limestone. It has a harsh, rough feel and is used to polish metals and stones.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":37,"ChoiceValue":138,"ChoiceName":"gneiss, biotite","ChoiceLabel":"Biotite gneiss","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":38,"ChoiceValue":139,"ChoiceName":"gneiss, granodioritic","ChoiceLabel":"Granodioritic gneiss","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":39,"ChoiceValue":140,"ChoiceName":"gneiss, hornblende","ChoiceLabel":"Hornblende gneiss","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":81,"ChoiceValue":141,"ChoiceName":"metasiltstone","ChoiceLabel":"Metasiltstone","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":40,"ChoiceValue":142,"ChoiceName":"gneiss, migmatitic","ChoiceLabel":"Migmatitic gneiss","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":41,"ChoiceValue":143,"ChoiceName":"gneiss, muscovite-biotite","ChoiceLabel":"Muscovite-biotite gneiss","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":119,"ChoiceValue":144,"ChoiceName":"schist, graphitic","ChoiceLabel":"Graphitic schist","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":138,"ChoiceValue":145,"ChoiceName":"slate, sulfidic","ChoiceLabel":"Sulfidic slate","ChoiceObsolete":0,"ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":45,"ChoiceValue":146,"ChoiceName":"granitoid","ChoiceLabel":"Granitoid","ChoiceObsolete":0,"ChoiceDescription":"a) In the IUGS classification, a preliminary term for (for field use) for a plutonic rock with Q (quartz) between 20 and 40 (%). b) A general term for all phaneritic igneous rocks (mineral crystals visible unaided and all about the same size) dominated by quartz and feldspars.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":147,"ChoiceName":"bauxite","ChoiceLabel":"Bauxite","ChoiceObsolete":0,"ChoiceDescription":"An off-white to dark red brown weathered detritus or rock composed of aluminum oxides (mainly gibbsite with some boehmite and diaspore), iron hydroxides, silica, silt, and especially clay minerals. Bauxite originates in tropical and subtropical environments as highly weathered residue from carbonate or silicate rocks and can occur in concretionary, earthy, pisolitic or oolitic forms. SW & GG","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":70,"ChoiceValue":148,"ChoiceName":"limestone, coral","ChoiceLabel":"Coral limestone","ChoiceObsolete":0,"ChoiceDescription":"An informal term for massive limestone composed primarily of coral and coral fragments commonly associated with marine islands or coral reefs in tropical or subtropical waters. Compare - coral island. SW","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":149,"ChoiceName":"anhydrite, rock","ChoiceLabel":"Rock anhydrite","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed chiefly of mineral anhydrite (anhydrous CaSO4); The rock is generally massive, cryptocrystalline, and may exhibit rhythmic sedimentation (rhymites). Compare - rock gypsum, rock halite. SW","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":52,"ChoiceValue":150,"ChoiceName":"halite, rock","ChoiceLabel":"Rock halite","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed primarily of halite (NaCl). SW","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":94,"ChoiceValue":151,"ChoiceName":"novaculite","ChoiceLabel":"Novaculite","ChoiceObsolete":0,"ChoiceDescription":"A dense, extremely finely grained, even-textured, siliceous, sedimentary rock similar to chert. It is hard, white to grayish-black in color, translucent on thin edges, has a dull to waxy luster, and displays smooth conchoidal fracture when broken. \r\n\r\nNovaculite principally occurs in the Marathon Uplift of Texas and Ouachita Mountains of Arkansas and Oklahoma where it forms erosion resistant ridges. Novaculite appears to form from chert recrystallization with microcrystalline quartz dominant over cryptocrystalline chalcedony. At the Ouachita Mountains type occurrence, novaculite formed by low-grade, thermal metamorphism of bedded chert. Novaculite is commercially quarried as a whetstone or oilstone. Compare - chert. GG & SW","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":133,"ChoiceValue":152,"ChoiceName":"siltite","ChoiceLabel":"Siltite","ChoiceObsolete":0,"ChoiceDescription":"A compact, weakly metamorphosed rock formed by alteration of siltstone, mudstone, or silty shale. Siltite is more indurated than mudstone or shale and lacks either shale fissility or slate-like cleavage. Siltite differs from argillite in that silt-size grains (0.002 to 0.062 mm) rather than clay-size (<0.002 mm) dominate the matrix. Siltite differs from siltstone, mudstone, or shale in that it exhibits very low to low grade metamorphic or diagenetic layer silicate and feldspar alteration to sericite, chlorite, and albite (subgreenschist to greenschist metamorphic facies) (Maxwell, 1973; Kidder, 1987).","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":118,"ChoiceValue":153,"ChoiceName":"schist, biotite","ChoiceLabel":"Biotite schist","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily biotite.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":121,"ChoiceValue":154,"ChoiceName":"schist, muscovite","ChoiceLabel":"Muscovite schist","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily muscovite.","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":74,"ChoiceValue":155,"ChoiceName":"limonite","ChoiceLabel":"Limonite","ChoiceObsolete":0,"ChoiceDescription":"A general 'field' term for various brown to yellowish brown, amorphous- to- cryptocrystalline hydrous ferric oxides that are an undetermined mixture of goethite, hematite, and lepidocrocite formed by weathering and iron oxidation from iron-bearing, rocks and minerals. SW & GG","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":122,"ChoiceValue":156,"ChoiceName":"schist, sericite","ChoiceLabel":"Sericite schist","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily sericite. A fine-grained muscovite","ColumnPhysicalName":"bedrckkind","ColumnLogicalName":"bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":157,"ChoiceName":"diatomite","ChoiceLabel":"Diatomite","ChoiceObsolete":0,"ChoiceDescription":"A light-colored, soft, siliceous sedimentary rock consisting chiefly of opaline diatom frustules deposited in a lacustrine or marine environment. 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Commonly called \"volcanic ash\". 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Compare - scoria, tephra.","ColumnPhysicalName":"osdbedrckkind","ColumnLogicalName":"osd_bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":124,"ChoiceValue":23,"ChoiceName":"scoria","ChoiceLabel":"Scoria","ChoiceObsolete":0,"ChoiceDescription":"Vesicular, cindery crust or bomb-sized fragments of such material on the surface of andesitic or basaltic lava, the vesicular nature of which is due to the escape of volcanic gases before solidification; it is usually heavier, darker, and more crystalline than pumice. Synonym - cinder. 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Examples: andesite, basalt, granite. 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{"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":151,"ChoiceValue":58,"ChoiceName":"tuff, unspecified","ChoiceLabel":"Tuff","ChoiceObsolete":0,"ChoiceDescription":"A compacted deposit that is 50 percent or more volcanic ash and dust.","ColumnPhysicalName":"osdbedrckkind","ColumnLogicalName":"osd_bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":149,"ChoiceValue":59,"ChoiceName":"tuff, acidic","ChoiceLabel":"Acidic tuff","ChoiceObsolete":0,"ColumnPhysicalName":"osdbedrckkind","ColumnLogicalName":"osd_bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":150,"ChoiceValue":60,"ChoiceName":"tuff, basic","ChoiceLabel":"Basic tuff","ChoiceObsolete":0,"ColumnPhysicalName":"osdbedrckkind","ColumnLogicalName":"osd_bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":157,"ChoiceValue":61,"ChoiceName":"volcanic breccia, unspecified","ChoiceLabel":"Volcanic breccia","ChoiceObsolete":0,"ColumnPhysicalName":"osdbedrckkind","ColumnLogicalName":"osd_bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":155,"ChoiceValue":62,"ChoiceName":"volcanic breccia, acidic","ChoiceLabel":"Acidic volcanic breccia","ChoiceObsolete":0,"ColumnPhysicalName":"osdbedrckkind","ColumnLogicalName":"osd_bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":156,"ChoiceValue":63,"ChoiceName":"volcanic breccia, basic","ChoiceLabel":"Basic volcanic breccia","ChoiceObsolete":0,"ColumnPhysicalName":"osdbedrckkind","ColumnLogicalName":"osd_bedrock_kind"} 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{"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":49,"ChoiceValue":88,"ChoiceName":"graywacke","ChoiceLabel":"Graywacke","ChoiceObsolete":0,"ColumnPhysicalName":"osdbedrckkind","ColumnLogicalName":"osd_bedrock_kind"} {"DomainID":517,"DomainName":"bedrock_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":51,"ChoiceValue":89,"ChoiceName":"gypsum, rock","ChoiceLabel":"Rock gypsum","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed primarily of mineral gypsum (CaSO4.2H2O). 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Sauerwein 1983","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":135,"ChoiceValue":132,"ChoiceName":"806","ChoiceLabel":"Carmean 1971, 1972 (806)","ChoiceObsolete":0,"ChoiceDescription":"Chestnut oak Unglaciated uplands of southeastern Ohio, Eastern Kentucky, southern Indiana, southern Illinois, and southern Missouri Carmean 1971, 1972","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":130,"ChoiceValue":133,"ChoiceName":"801","ChoiceLabel":"Grane, Bower 1971 (801)","ChoiceObsolete":0,"ChoiceDescription":"Northern Red oak and Black oak, Graney, Bower 1971","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":136,"ChoiceValue":134,"ChoiceName":"807","ChoiceLabel":"Carmean 1978 (807)","ChoiceObsolete":0,"ChoiceDescription":"Upland Oaks, Carmean 1978","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":129,"ChoiceValue":135,"ChoiceName":"800","ChoiceLabel":"Gevorkiantz 1957f (800)","ChoiceObsolete":0,"ChoiceDescription":"Eastern white pine, Gevorkiantz 1957f","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":139,"ChoiceValue":136,"ChoiceName":"810","ChoiceLabel":"Olson 1959 (810)","ChoiceObsolete":0,"ChoiceDescription":"upland oaks Virginia-Carolina Piedmont and northern Appalachian Mountains, Olson 1959","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":144,"ChoiceValue":137,"ChoiceName":"860","ChoiceLabel":"Broadfoot 1963 (860)","ChoiceObsolete":0,"ChoiceDescription":"Laurel oak, Overcup oak, Swamp Chestnut oak, Water oak, Nuttall oak, Pin oak, Willow oak, Shumard's oak, Broadfoot 1963","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":137,"ChoiceValue":138,"ChoiceName":"808","ChoiceLabel":"Carmean 1971, 1972 (808)","ChoiceObsolete":0,"ChoiceDescription":"Black oak Unglaciated uplands of southeastern Ohio, Eastern Kentucky, southern Indiana, southern Illinois, and southern Missouri Carmean 1971, 1972","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":146,"ChoiceValue":139,"ChoiceName":"900","ChoiceLabel":"Kellogg 1939b (900)","ChoiceObsolete":0,"ChoiceDescription":"Black locust, entire range: Site index curves for plantation black locust, Central States region. USDA, Forest Service. Central States Forest Experiment Station Note 36. Kellogg 1939b","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":147,"ChoiceValue":140,"ChoiceName":"930","ChoiceLabel":"Lindquist, Palley 1963 (930)","ChoiceObsolete":0,"ChoiceDescription":"Redwood, Empirical yield tables for young-growth redwood. Calif. Ag. Exp. Sta. Bull. 796. Lindquist, Palley 1963","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":138,"ChoiceValue":141,"ChoiceName":"809","ChoiceLabel":"Carmean 1978 (809)","ChoiceObsolete":0,"ChoiceDescription":"American basswood, Carmean 1978","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":152,"ChoiceValue":142,"ChoiceName":"991","ChoiceLabel":"Frothingham 1915 (991)","ChoiceObsolete":0,"ChoiceDescription":"Eastern hemlock, Frothingham 1915","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":151,"ChoiceValue":143,"ChoiceName":"990","ChoiceLabel":"Barnes 1962 (990)","ChoiceObsolete":0,"ChoiceDescription":"Western hemlock, entire range, Yield of Even-Aged Stands of Western Hemlock Tech Bulletin No. 1273. Barnes 1962","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":153,"ChoiceValue":144,"ChoiceName":"995","ChoiceLabel":"Wiley 1978 (995)","ChoiceObsolete":0,"ChoiceDescription":"Western hemlock, Western WA, Site index tables for western hemlock in the Pacific Northwest. Weyerhaeuser For. Pap. 17. Wiley 1978","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":94,"ChoiceValue":145,"ChoiceName":"615","ChoiceLabel":"Biging and Wensel 1984 (615)","ChoiceObsolete":0,"ChoiceDescription":"Site Index Equations for Young Growth Mixed Conifers of Northern California. Northern Calif. Forest Yield Cooperative, University of Calif. Berkeley Research Note No. 8. Biging and Wensel 1984","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":125,"ChoiceValue":146,"ChoiceName":"780","ChoiceLabel":"Curtis, Herman, DeMars 1974 (780) (obsolete)","ChoiceObsolete":1,"ChoiceDescription":"Douglas-fir, Height Growth and Site Index for Douglas-fir in High Elevation Forests of the Oregon - Washington Cascades. Forest Science. Vol. 20, No. 4. Curtis, R.O., F.R. Herman, D.J. DeMars. 1974. (obsolete)","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":149,"ChoiceValue":147,"ChoiceName":"960","ChoiceLabel":"Gevorkiantz 1957g (960)","ChoiceObsolete":0,"ChoiceDescription":"White spruce, Gevorkiantz 1957g","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":148,"ChoiceValue":148,"ChoiceName":"935","ChoiceLabel":"Krumland, Wensel 1986 (935)","ChoiceObsolete":0,"ChoiceDescription":"A Site Index System for Redwood and Douglas-fir in California's North Coast Forest. Univ. Calif. Agric. Exp. Sta., Hilgardia 54:1-14. Wensel, L. C. and B. Krumland 1986.","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":79,"ChoiceValue":149,"ChoiceName":"525","ChoiceLabel":"Hegyi, Jelinek, Carpenter 100TA 1979 (525)","ChoiceObsolete":0,"ChoiceDescription":"Site index equations and curves for the major tree species in British Columbia. Inventory Branch, B.C. Ministry of Forests, Forest Inventory Report No. 1. Hegyi, F., J. Jelinek, and D.B. Carpenter. 1979","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":150,"ChoiceValue":150,"ChoiceName":"970","ChoiceLabel":"Kurucz 50BH, 1978 (970)","ChoiceObsolete":0,"ChoiceDescription":"Preliminary, polymorphic site index curves for western redcedar - Thuja plicata Donn - in coastal British Columbia. For. Res. Note 3. Vancouver, BC: Kurucz, J. F. 1978.","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":154,"ChoiceValue":151,"ChoiceName":"9999","ChoiceLabel":"Unknown curve","ChoiceObsolete":0,"ChoiceDescription":"Unknown","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":8,"ChoiceValue":152,"ChoiceName":"037","ChoiceLabel":"Mathiasen, Olsen, Edminster 2006 (037)","ChoiceObsolete":0,"ChoiceDescription":"Site index curves for white fir in the southwestern United States developed using a guide curve method. Western journal of applied forestry. 21(2): 87-93. Mathiasen, Robert L.; Olsen, William K.; Edminster, Carleton B. 2006.","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":88,"ChoiceValue":153,"ChoiceName":"575","ChoiceLabel":"Curtis, Diaz, Clendenen 1990 (575)","ChoiceObsolete":0,"ChoiceDescription":"Height growth and site index curves for western white pine in the Cascade Range of Washington and Oregon. Curtis, R.O., Diaz, N.M. 1990","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":89,"ChoiceValue":154,"ChoiceName":"576","ChoiceLabel":"Curtis, Diaz, Clendenen 1990 (576)","ChoiceObsolete":0,"ChoiceDescription":"Height growth and site index curves for western white pine in the Cascade Range of Washington and Oregon. Curtis, R.O., Diaz, N.M. 1990","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":155,"ChoiceValue":155,"ChoiceName":"625","ChoiceLabel":"Brickell 1970","ChoiceObsolete":0,"ChoiceDescription":"Equations and computer subroutines for estimating site quality of eight Rocky Mountain species. Res. Pap. INT-75. Ogden, UT: U.S. Department of Agriculture, Forest Service, Intermountain Forest and Range Experiment Station. Brickell, J.E. 1970","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":156,"ChoiceValue":156,"ChoiceName":"602","ChoiceLabel":"Lynch 1958 (602)","ChoiceObsolete":0,"ChoiceDescription":"Effects of stocking on site measurement and yield of second growth ponderosa pine in the inland empire. USDA For. Serv. Intermtn. For. Range Exp. Sta. Res. Pap. 56. Lynch, D. W. 1958.","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":157,"ChoiceValue":157,"ChoiceName":"460","ChoiceLabel":"Rosner 2004 (460)","ChoiceObsolete":0,"ChoiceDescription":"Growth and yield of black spruce, Picea mariana (Mill.) B.S.P., in Alaska. M.Sc. thesis, University of Alaska, Fairbanks, Alaska. Rosner, C. 2004.","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":967,"DomainName":"site_index_curves","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":158,"ChoiceValue":158,"ChoiceName":"461","ChoiceLabel":"Quenet, Manning 1990 (461)","ChoiceObsolete":0,"ChoiceDescription":"Site index equations for black spruce and white spruce in the Yukon. Forestry Canada, Pacific Forestry Centre, Victoria, BC. Information Report BC-X-317. Quenet, R.V.; Manning, G.H. 1990","ColumnPhysicalName":"siteindexbase","ColumnLogicalName":"site_index_base"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"interfluve","ChoiceLabel":"Interfluve","ChoiceObsolete":0,"ChoiceDescription":"An elevated area between two drainageways that sheds water to those drainageways.","ColumnPhysicalName":"geomposhill","ColumnLogicalName":"geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"head slope","ChoiceLabel":"Head Slope","ChoiceObsolete":0,"ChoiceDescription":"The concave surface at the head of a drainageway where the flow of water converges downward toward the center and contour lines form concave curves.","ColumnPhysicalName":"geomposhill","ColumnLogicalName":"geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"nose slope","ChoiceLabel":"Nose Slope","ChoiceObsolete":0,"ChoiceDescription":"The projecting end of an interfluve, where contour lines connecting the opposing side slopes form convex curves around the projecting end and lines perpendicular to the contours diverge downward. Overland flow of water is divergent.","ColumnPhysicalName":"geomposhill","ColumnLogicalName":"geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"side slope","ChoiceLabel":"Side Slope","ChoiceObsolete":0,"ChoiceDescription":"The slope bounding a drainageway and lying between the drainageway and the adjacent interfluve. It is generally linear along the slope width and overland flow is parallel down the slope.","ColumnPhysicalName":"geomposhill","ColumnLogicalName":"geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"base slope","ChoiceLabel":"Base Slope","ChoiceObsolete":0,"ChoiceDescription":"A geomorphic component of hills consisting of the concave to linear slope (perpendicular to the contour) which, regardless of the lateral shape is an area that forms an apron or wedge at the bottom of a hillside dominated by colluvial and slope wash processes and sediments (e.g., colluvium and slope alluvium). Distal base slope sediments commonly grade to, or interfinger with, alluvial fills, or gradually thin to form pedisediment over residuum. Compare - head slope, side slope, nose slope, interfluve, free face. SW","ColumnPhysicalName":"geomposhill","ColumnLogicalName":"geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"crest","ChoiceLabel":"Crest","ChoiceObsolete":0,"ChoiceDescription":"A geomorphic component of hills consisting of the convex slopes (perpendicular to the contour) that form the narrow, roughly linear top area of a hill, ridge, or other upland where shoulders have converged to the extent that little or no summit remains; dominated by erosion, slope wash and mass movement processes and sediments (e.g., slope alluvium, creep). Commonly, soils on crests are more similar to those on side slopes than to soils on adjacent interfluves. Compare - interfluve, head slope, side slope, nose slope. SW","ColumnPhysicalName":"geomposhill","ColumnLogicalName":"geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"free face","ChoiceLabel":"Free face","ChoiceObsolete":0,"ChoiceDescription":"The part of a hillside or mountainside consisting of an outcrop of bare rock (scarp or cliff) that sheds colluvium to slopes below and commonly stands more steeply than the angle of repose of the colluvial slope (e.g. talus slope) immediately below. SW & GG","ColumnPhysicalName":"geomposhill","ColumnLogicalName":"geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"crested hills","ChoiceLabel":"Crested hills","ChoiceObsolete":1,"ColumnPhysicalName":"geomposhill","ColumnLogicalName":"geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"interfluve","ChoiceLabel":"Interfluve","ChoiceObsolete":0,"ChoiceDescription":"An elevated area between two drainageways that sheds water to those drainageways.","ColumnPhysicalName":"osdgeomposhill","ColumnLogicalName":"osd_geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"head slope","ChoiceLabel":"Head Slope","ChoiceObsolete":0,"ChoiceDescription":"The concave surface at the head of a drainageway where the flow of water converges downward toward the center and contour lines form concave curves.","ColumnPhysicalName":"osdgeomposhill","ColumnLogicalName":"osd_geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"nose slope","ChoiceLabel":"Nose Slope","ChoiceObsolete":0,"ChoiceDescription":"The projecting end of an interfluve, where contour lines connecting the opposing side slopes form convex curves around the projecting end and lines perpendicular to the contours diverge downward. Overland flow of water is divergent.","ColumnPhysicalName":"osdgeomposhill","ColumnLogicalName":"osd_geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"side slope","ChoiceLabel":"Side Slope","ChoiceObsolete":0,"ChoiceDescription":"The slope bounding a drainageway and lying between the drainageway and the adjacent interfluve. It is generally linear along the slope width and overland flow is parallel down the slope.","ColumnPhysicalName":"osdgeomposhill","ColumnLogicalName":"osd_geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"base slope","ChoiceLabel":"Base Slope","ChoiceObsolete":0,"ChoiceDescription":"A geomorphic component of hills consisting of the concave to linear slope (perpendicular to the contour) which, regardless of the lateral shape is an area that forms an apron or wedge at the bottom of a hillside dominated by colluvial and slope wash processes and sediments (e.g., colluvium and slope alluvium). Distal base slope sediments commonly grade to, or interfinger with, alluvial fills, or gradually thin to form pedisediment over residuum. Compare - head slope, side slope, nose slope, interfluve, free face. SW","ColumnPhysicalName":"osdgeomposhill","ColumnLogicalName":"osd_geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"crest","ChoiceLabel":"Crest","ChoiceObsolete":0,"ChoiceDescription":"A geomorphic component of hills consisting of the convex slopes (perpendicular to the contour) that form the narrow, roughly linear top area of a hill, ridge, or other upland where shoulders have converged to the extent that little or no summit remains; dominated by erosion, slope wash and mass movement processes and sediments (e.g., slope alluvium, creep). Commonly, soils on crests are more similar to those on side slopes than to soils on adjacent interfluves. Compare - interfluve, head slope, side slope, nose slope. SW","ColumnPhysicalName":"osdgeomposhill","ColumnLogicalName":"osd_geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"free face","ChoiceLabel":"Free face","ChoiceObsolete":0,"ChoiceDescription":"The part of a hillside or mountainside consisting of an outcrop of bare rock (scarp or cliff) that sheds colluvium to slopes below and commonly stands more steeply than the angle of repose of the colluvial slope (e.g. talus slope) immediately below. SW & GG","ColumnPhysicalName":"osdgeomposhill","ColumnLogicalName":"osd_geomorphic_position_hills"} {"DomainID":968,"DomainName":"geomor_pos_hill","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"crested hills","ChoiceLabel":"Crested hills","ChoiceObsolete":1,"ColumnPhysicalName":"osdgeomposhill","ColumnLogicalName":"osd_geomorphic_position_hills"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"mountaintop","ChoiceLabel":"Mountaintop","ChoiceObsolete":0,"ChoiceDescription":"roughly analogous to the crest or summit); Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"geomposmntn","ColumnLogicalName":"geomorphic_position_mountains"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"mountainflank","ChoiceLabel":"Mountainflank","ChoiceObsolete":0,"ChoiceDescription":"the long slope along the sides of mountains which can be further subdivided into three portions based on the relative slope location: upper third-, middle third-, or lower third mountainflank; Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"geomposmntn","ColumnLogicalName":"geomorphic_position_mountains"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"mountainbase","ChoiceLabel":"Mountainbase","ChoiceObsolete":0,"ChoiceDescription":"colluvium / slope alluvium apron at the bottom of the mountain; Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"geomposmntn","ColumnLogicalName":"geomorphic_position_mountains"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"mountainflank, upper third","ChoiceLabel":"Upper third of mountainflank","ChoiceObsolete":0,"ChoiceDescription":"The upper third of the long slope along mountainflank. Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"geomposmntn","ColumnLogicalName":"geomorphic_position_mountains"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"mountainflank, center third","ChoiceLabel":"Center third of mountainflank","ChoiceObsolete":0,"ChoiceDescription":"The middle third of the long slope along mountainflank. Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"geomposmntn","ColumnLogicalName":"geomorphic_position_mountains"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"mountainflank, lower third","ChoiceLabel":"Lower third of mountainflank","ChoiceObsolete":0,"ChoiceDescription":"The lower third of the long slope along mountainflank. Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"geomposmntn","ColumnLogicalName":"geomorphic_position_mountains"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"free face","ChoiceLabel":"Free face","ChoiceObsolete":0,"ChoiceDescription":"The part of a hillside or mountainside consisting of an outcrop of bare rock (scarp or cliff) that sheds colluvium to slopes below and commonly stands more steeply than the angle of repose of the colluvial slope (e.g. talus slope) immediately below. References: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE. and Neuendorf, K.K.E., Mehl Jr., J.P., and Jackson, J.A. (ed.) 2005. Glossary of geology, 5th Ed. American Geological Institute, Alexandria, VA. 779 p.","ColumnPhysicalName":"geomposmntn","ColumnLogicalName":"geomorphic_position_mountains"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"mountaintop","ChoiceLabel":"Mountaintop","ChoiceObsolete":0,"ChoiceDescription":"roughly analogous to the crest or summit); Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"osdgeomposmntn","ColumnLogicalName":"osd_geomorphic_position_mts"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"mountainflank","ChoiceLabel":"Mountainflank","ChoiceObsolete":0,"ChoiceDescription":"the long slope along the sides of mountains which can be further subdivided into three portions based on the relative slope location: upper third-, middle third-, or lower third mountainflank; Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"osdgeomposmntn","ColumnLogicalName":"osd_geomorphic_position_mts"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"mountainbase","ChoiceLabel":"Mountainbase","ChoiceObsolete":0,"ChoiceDescription":"colluvium / slope alluvium apron at the bottom of the mountain; Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"osdgeomposmntn","ColumnLogicalName":"osd_geomorphic_position_mts"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"mountainflank, upper third","ChoiceLabel":"Upper third of mountainflank","ChoiceObsolete":0,"ChoiceDescription":"The upper third of the long slope along mountainflank. Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"osdgeomposmntn","ColumnLogicalName":"osd_geomorphic_position_mts"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"mountainflank, center third","ChoiceLabel":"Center third of mountainflank","ChoiceObsolete":0,"ChoiceDescription":"The middle third of the long slope along mountainflank. Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"osdgeomposmntn","ColumnLogicalName":"osd_geomorphic_position_mts"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"mountainflank, lower third","ChoiceLabel":"Lower third of mountainflank","ChoiceObsolete":0,"ChoiceDescription":"The lower third of the long slope along mountainflank. Reference: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE.","ColumnPhysicalName":"osdgeomposmntn","ColumnLogicalName":"osd_geomorphic_position_mts"} {"DomainID":969,"DomainName":"geomor_pos_mountain","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"free face","ChoiceLabel":"Free face","ChoiceObsolete":0,"ChoiceDescription":"The part of a hillside or mountainside consisting of an outcrop of bare rock (scarp or cliff) that sheds colluvium to slopes below and commonly stands more steeply than the angle of repose of the colluvial slope (e.g. talus slope) immediately below. References: Schoeneberger, P.J. and Wysocki, D.A. 2013. (personal communication), National Soil Survey Center, NRCS, Lincoln, NE. and Neuendorf, K.K.E., Mehl Jr., J.P., and Jackson, J.A. (ed.) 2005. Glossary of geology, 5th Ed. American Geological Institute, Alexandria, VA. 779 p.","ColumnPhysicalName":"osdgeomposmntn","ColumnLogicalName":"osd_geomorphic_position_mts"} {"DomainID":970,"DomainName":"geomor_pos_terrace","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"riser","ChoiceLabel":"Riser","ChoiceObsolete":0,"ChoiceDescription":"The vertical or steeply sloping surface, commonly one of a series, of natural steplike landforms, as those of a glacial stairway or of successive stream terraces.","ColumnPhysicalName":"geompostrce","ColumnLogicalName":"geomorphic_position_terraces"} {"DomainID":970,"DomainName":"geomor_pos_terrace","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"tread","ChoiceLabel":"Tread","ChoiceObsolete":0,"ChoiceDescription":"The flat or gently sloping surface of natural step-like landforms, commonly one of a series, such as successive stream terraces.","ColumnPhysicalName":"geompostrce","ColumnLogicalName":"geomorphic_position_terraces"} {"DomainID":970,"DomainName":"geomor_pos_terrace","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"riser","ChoiceLabel":"Riser","ChoiceObsolete":0,"ChoiceDescription":"The vertical or steeply sloping surface, commonly one of a series, of natural steplike landforms, as those of a glacial stairway or of successive stream terraces.","ColumnPhysicalName":"osdgeompostrce","ColumnLogicalName":"osd_geomorphic_position_terrs"} {"DomainID":970,"DomainName":"geomor_pos_terrace","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"tread","ChoiceLabel":"Tread","ChoiceObsolete":0,"ChoiceDescription":"The flat or gently sloping surface of natural step-like landforms, commonly one of a series, such as successive stream terraces.","ColumnPhysicalName":"osdgeompostrce","ColumnLogicalName":"osd_geomorphic_position_terrs"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"summit","ChoiceLabel":"Summit","ChoiceObsolete":0,"ChoiceDescription":"The topographically highest hillslope position of a hillslope profile and exhibiting a nearly level (planar or only slightly convex) surface.","ColumnPhysicalName":"hillslopeprof","ColumnLogicalName":"hillslope_profile"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"shoulder","ChoiceLabel":"Shoulder","ChoiceObsolete":0,"ChoiceDescription":"The hillslope position that forms the uppermost inclined surface near the top of a hillslope. If present, it comprises the transition zone from backslope to summit. The surface is dominantly convex in profile and erosional in origin.","ColumnPhysicalName":"hillslopeprof","ColumnLogicalName":"hillslope_profile"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"backslope","ChoiceLabel":"Backslope","ChoiceObsolete":0,"ChoiceDescription":"The hillslope profile position that forms the steepest and generally linear, middle portion of the slope. In profile, backslopes are commonly bounded by a convex shoulder above and a concave footslope below. They may or may not include cliff segments (i.e. free faces). Backslopes are commonly erosional forms produced by mass movement, colluvial action, and running water.","ColumnPhysicalName":"hillslopeprof","ColumnLogicalName":"hillslope_profile"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"footslope","ChoiceLabel":"Footslope","ChoiceObsolete":0,"ChoiceDescription":"The hillslope position that forms the inner, gently inclined surface at the base of a hillslope. In profile, footslopes are commonly concave. It is a transition zone between upslope sites of erosion and transport (shoulder, backslope) and downslope sites of deposition (toeslope).","ColumnPhysicalName":"hillslopeprof","ColumnLogicalName":"hillslope_profile"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"toeslope","ChoiceLabel":"Toeslope","ChoiceObsolete":0,"ChoiceDescription":"The hillslope position that forms the gently inclined surface at the base of a hillslope. Toeslopes in profile are commonly gentle and linear, and are constructional surfaces forming the lower part of a hill-slope continuum that grades to valley or closed-depression floors.","ColumnPhysicalName":"hillslopeprof","ColumnLogicalName":"hillslope_profile"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"summit","ChoiceLabel":"Summit","ChoiceObsolete":0,"ChoiceDescription":"The topographically highest hillslope position of a hillslope profile and exhibiting a nearly level (planar or only slightly convex) surface.","ColumnPhysicalName":"osdhillslopeprof","ColumnLogicalName":"osd_hillslope_profile"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"shoulder","ChoiceLabel":"Shoulder","ChoiceObsolete":0,"ChoiceDescription":"The hillslope position that forms the uppermost inclined surface near the top of a hillslope. If present, it comprises the transition zone from backslope to summit. The surface is dominantly convex in profile and erosional in origin.","ColumnPhysicalName":"osdhillslopeprof","ColumnLogicalName":"osd_hillslope_profile"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"backslope","ChoiceLabel":"Backslope","ChoiceObsolete":0,"ChoiceDescription":"The hillslope profile position that forms the steepest and generally linear, middle portion of the slope. In profile, backslopes are commonly bounded by a convex shoulder above and a concave footslope below. They may or may not include cliff segments (i.e. free faces). Backslopes are commonly erosional forms produced by mass movement, colluvial action, and running water.","ColumnPhysicalName":"osdhillslopeprof","ColumnLogicalName":"osd_hillslope_profile"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"footslope","ChoiceLabel":"Footslope","ChoiceObsolete":0,"ChoiceDescription":"The hillslope position that forms the inner, gently inclined surface at the base of a hillslope. In profile, footslopes are commonly concave. It is a transition zone between upslope sites of erosion and transport (shoulder, backslope) and downslope sites of deposition (toeslope).","ColumnPhysicalName":"osdhillslopeprof","ColumnLogicalName":"osd_hillslope_profile"} {"DomainID":971,"DomainName":"hillslope_profile","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"toeslope","ChoiceLabel":"Toeslope","ChoiceObsolete":0,"ChoiceDescription":"The hillslope position that forms the gently inclined surface at the base of a hillslope. Toeslopes in profile are commonly gentle and linear, and are constructional surfaces forming the lower part of a hill-slope continuum that grades to valley or closed-depression floors.","ColumnPhysicalName":"osdhillslopeprof","ColumnLogicalName":"osd_hillslope_profile"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"microhigh","ChoiceLabel":"Microhigh","ChoiceObsolete":0,"ChoiceDescription":"A generic microrelief term applied to slightly elevated areas relative to the adjacent ground surface; differences in relief range from several centimeters to several meters; cross sectional profiles can be simple or complex and generally consist of gently rounded, convex tops with gently sloping sides.","ColumnPhysicalName":"geomicrorelief","ColumnLogicalName":"geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"microlow","ChoiceLabel":"Microlow","ChoiceObsolete":0,"ChoiceDescription":"A generic microrelief term applied to slightly lower areas relative to the adjacent ground surface; differences in relief range from several centimeters to several meters; ; cross sectional profiles can be simple or complex and generally consist of subdued, concave, open or closed depressions with gently sloping sides.","ColumnPhysicalName":"geomicrorelief","ColumnLogicalName":"geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"microdepression","ChoiceLabel":"Microdepression","ChoiceObsolete":1,"ChoiceDescription":"refer to micro-low","ColumnPhysicalName":"geomicrorelief","ColumnLogicalName":"geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"microknoll","ChoiceLabel":"Microknoll","ChoiceObsolete":1,"ChoiceDescription":"refer to micro-high.","ColumnPhysicalName":"geomicrorelief","ColumnLogicalName":"geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":5,"ChoiceName":"other","ChoiceLabel":"Other (specified in notes)","ChoiceObsolete":1,"ColumnPhysicalName":"geomicrorelief","ColumnLogicalName":"geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":6,"ChoiceName":"microslope","ChoiceLabel":"Microslope","ChoiceObsolete":0,"ChoiceDescription":"A generic Microrelief term applied to areas of nominal surface relief (slightly sloping to level), relative to the adjacent ground surface; differences in overall local relief range from several centimeters to several meters. Cross-sectional profiles can be simple or complex and generally consist of low and gently rounded, convex tops (microhigh) with gently sloping to level sides (microslope), and depressional low areas (microlow). Microslopes commonly constitute the majority of the land surface area in gilgai and other settings with microrelief. SW.","ColumnPhysicalName":"geomicrorelief","ColumnLogicalName":"geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"microhigh","ChoiceLabel":"Microhigh","ChoiceObsolete":0,"ChoiceDescription":"A generic microrelief term applied to slightly elevated areas relative to the adjacent ground surface; differences in relief range from several centimeters to several meters; cross sectional profiles can be simple or complex and generally consist of gently rounded, convex tops with gently sloping sides.","ColumnPhysicalName":"osdgeomicrorelief","ColumnLogicalName":"osd_geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"microlow","ChoiceLabel":"Microlow","ChoiceObsolete":0,"ChoiceDescription":"A generic microrelief term applied to slightly lower areas relative to the adjacent ground surface; differences in relief range from several centimeters to several meters; ; cross sectional profiles can be simple or complex and generally consist of subdued, concave, open or closed depressions with gently sloping sides.","ColumnPhysicalName":"osdgeomicrorelief","ColumnLogicalName":"osd_geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"microdepression","ChoiceLabel":"Microdepression","ChoiceObsolete":1,"ChoiceDescription":"refer to micro-low","ColumnPhysicalName":"osdgeomicrorelief","ColumnLogicalName":"osd_geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"microknoll","ChoiceLabel":"Microknoll","ChoiceObsolete":1,"ChoiceDescription":"refer to micro-high.","ColumnPhysicalName":"osdgeomicrorelief","ColumnLogicalName":"osd_geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":5,"ChoiceName":"other","ChoiceLabel":"Other (specified in notes)","ChoiceObsolete":1,"ColumnPhysicalName":"osdgeomicrorelief","ColumnLogicalName":"osd_geomorph_micro_relief"} {"DomainID":972,"DomainName":"microrelief_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":6,"ChoiceName":"microslope","ChoiceLabel":"Microslope","ChoiceObsolete":0,"ChoiceDescription":"A generic Microrelief term applied to areas of nominal surface relief (slightly sloping to level), relative to the adjacent ground surface; differences in overall local relief range from several centimeters to several meters. Cross-sectional profiles can be simple or complex and generally consist of low and gently rounded, convex tops (microhigh) with gently sloping to level sides (microslope), and depressional low areas (microlow). Microslopes commonly constitute the majority of the land surface area in gilgai and other settings with microrelief. SW.","ColumnPhysicalName":"osdgeomicrorelief","ColumnLogicalName":"osd_geomorph_micro_relief"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":43,"ChoiceValue":1,"ChoiceName":"a","ChoiceLabel":"A","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":42,"ChoiceValue":2,"ChoiceName":"b","ChoiceLabel":"B","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":41,"ChoiceValue":3,"ChoiceName":"c","ChoiceLabel":"C","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":40,"ChoiceValue":4,"ChoiceName":"d","ChoiceLabel":"D","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":39,"ChoiceValue":5,"ChoiceName":"e","ChoiceLabel":"E","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":38,"ChoiceValue":6,"ChoiceName":"f","ChoiceLabel":"F","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":37,"ChoiceValue":7,"ChoiceName":"g","ChoiceLabel":"G","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":36,"ChoiceValue":8,"ChoiceName":"h","ChoiceLabel":"H","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":35,"ChoiceValue":9,"ChoiceName":"i","ChoiceLabel":"I","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":34,"ChoiceValue":10,"ChoiceName":"j","ChoiceLabel":"J","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":33,"ChoiceValue":11,"ChoiceName":"k","ChoiceLabel":"K","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":32,"ChoiceValue":12,"ChoiceName":"l","ChoiceLabel":"L","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":31,"ChoiceValue":13,"ChoiceName":"m","ChoiceLabel":"M","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":30,"ChoiceValue":14,"ChoiceName":"n","ChoiceLabel":"N","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":29,"ChoiceValue":15,"ChoiceName":"o","ChoiceLabel":"O","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":28,"ChoiceValue":16,"ChoiceName":"p","ChoiceLabel":"P","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":27,"ChoiceValue":17,"ChoiceName":"q","ChoiceLabel":"Q","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":18,"ChoiceName":"r","ChoiceLabel":"R","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":25,"ChoiceValue":19,"ChoiceName":"s","ChoiceLabel":"S","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":20,"ChoiceName":"t","ChoiceLabel":"T","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":21,"ChoiceName":"u","ChoiceLabel":"U","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":22,"ChoiceName":"v","ChoiceLabel":"V","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":23,"ChoiceName":"w","ChoiceLabel":"W","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":24,"ChoiceName":"x","ChoiceLabel":"X","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":25,"ChoiceName":"y","ChoiceLabel":"Y","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":26,"ChoiceName":"z","ChoiceLabel":"Z","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":27,"ChoiceName":"aa","ChoiceLabel":"AA","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":28,"ChoiceName":"bb","ChoiceLabel":"BB","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":29,"ChoiceName":"cc","ChoiceLabel":"CC","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":30,"ChoiceName":"dd","ChoiceLabel":"DD","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":31,"ChoiceName":"ee","ChoiceLabel":"EE","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":32,"ChoiceName":"ff","ChoiceLabel":"FF","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":33,"ChoiceName":"gg","ChoiceLabel":"GG","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":34,"ChoiceName":"hh","ChoiceLabel":"HH","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":35,"ChoiceName":"ii","ChoiceLabel":"II","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":36,"ChoiceName":"jj","ChoiceLabel":"JJ","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":37,"ChoiceName":"kk","ChoiceLabel":"KK","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":38,"ChoiceName":"ll","ChoiceLabel":"LL","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":39,"ChoiceName":"mm","ChoiceLabel":"MM","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":40,"ChoiceName":"nn","ChoiceLabel":"NN","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":41,"ChoiceName":"oo","ChoiceLabel":"OO","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":42,"ChoiceName":"pp","ChoiceLabel":"PP","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":973,"DomainName":"va_soil_management_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":43,"ChoiceName":"qq","ChoiceLabel":"QQ","ChoiceObsolete":0,"ChoiceDescription":"Reference: Virginia Polytechnic Institute and State University. 1994. VALUES - Virginia Agronomic Land Use and Evaluation System. In Soil Test Recommendations for Virginia. Virginia Cooperative Extension.","ColumnPhysicalName":"vasoimgtgrp","ColumnLogicalName":"va_soil_management_group"} {"DomainID":974,"DomainName":"va_soil_productivity_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":1,"ChoiceName":"I","ChoiceLabel":"I","ChoiceObsolete":0,"ChoiceDescription":"Reference: Simpson, T.W., Baker, J.C., Monnett, M.M. VALUES Guidebook, Virginia Tech, Department of Crop and Soil Environmental Sciences","ColumnPhysicalName":"vasoiprdgrp","ColumnLogicalName":"va_soil_productivity_group"} {"DomainID":974,"DomainName":"va_soil_productivity_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":2,"ChoiceName":"Ia","ChoiceLabel":"Ia","ChoiceObsolete":0,"ChoiceDescription":"Reference: Simpson, T.W., Baker, J.C., Monnett, M.M. 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VALUES Guidebook, Virginia Tech, Department of Crop and Soil Environmental Sciences","ColumnPhysicalName":"vasoiprdgrp","ColumnLogicalName":"va_soil_productivity_group"} {"DomainID":974,"DomainName":"va_soil_productivity_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":9,"ChoiceName":"IIIb","ChoiceLabel":"IIIb","ChoiceObsolete":0,"ChoiceDescription":"Reference: Simpson, T.W., Baker, J.C., Monnett, M.M. VALUES Guidebook, Virginia Tech, Department of Crop and Soil Environmental Sciences","ColumnPhysicalName":"vasoiprdgrp","ColumnLogicalName":"va_soil_productivity_group"} {"DomainID":974,"DomainName":"va_soil_productivity_group","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":10,"ChoiceName":"IV","ChoiceLabel":"IV","ChoiceObsolete":0,"ChoiceDescription":"Reference: Simpson, T.W., Baker, J.C., Monnett, M.M. 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SW","ColumnPhysicalName":"geomposflats","ColumnLogicalName":"geomorphic_position_flats"} {"DomainID":1092,"DomainName":"geomor_pos_flat","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"flat","ChoiceLabel":"Flat","ChoiceObsolete":1,"ChoiceDescription":"default choice, official choices to be determined later","ColumnPhysicalName":"osdgeomposflats","ColumnLogicalName":"osd_geomorphic_position_flats"} {"DomainID":1092,"DomainName":"geomor_pos_flat","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"dip","ChoiceLabel":"Dip","ChoiceObsolete":0,"ChoiceDescription":"A geomorphic component (characteristic piece) of flat plains (e.g., lake plain, low coastal plain, low-relief till plain) consisting of a shallow and typically closed depression that tends to be an area of focused groundwater recharge but not a permanent water body and that lies slightly lower and is wetter than the adjacent talf, and favors the accumulation of fine sediments and organic materials. 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Generally less than 1m x 2m in size.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":6,"ChoiceName":"trench","ChoiceLabel":"Trench","ChoiceObsolete":0,"ChoiceDescription":"Sample extracted from the wall of a trench or pit dug with the aide of a backhoe. Generally larger than 1 x 2m in size.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":7,"ChoiceName":"cut","ChoiceLabel":"Cut","ChoiceObsolete":0,"ChoiceDescription":"Sample extracted from a relatively large near vertical cut such as a roadcut. Generally greater than 4 m in length.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"pit, large or quarry","ChoiceLabel":"Large Pit or Quarry","ChoiceObsolete":0,"ChoiceDescription":"Sample extracted from a large open pit or large very vertical bank, such as borrow pit, quarry, or stream cutbank. Generally greater than 33 m in length.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":9,"ChoiceName":"cut, beveled","ChoiceLabel":"Beveled Cut","ChoiceObsolete":0,"ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":10,"ChoiceName":"vibracore tube","ChoiceLabel":"Vibracore tube","ChoiceObsolete":0,"ChoiceDescription":"A method of collecting a soil sample by means of a core tube driven into the soil by the force of gravity, enhanced by vibration energy. The vibrating mechanism of a vibracorer, sometimes called the \"vibrahead\", operates on hydraulic, pneumatic, mechanical or electrical power from an external source. When the insertion is completed, the vibracorer is turned off, and the tube is withdrawn with the aid of hoist equipment.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":11,"ChoiceName":"auger, dutch","ChoiceLabel":"Dutch auger","ChoiceObsolete":0,"ChoiceDescription":"An open, strap-sided bucket auger (5-10 cm diam.) with a sharpened outer edge and a screw tip with a partial twist; also called a 'mud auger'.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":12,"ChoiceName":"dive observation","ChoiceLabel":"Dive observation","ChoiceObsolete":0,"ChoiceDescription":"A visual assessment of undisturbed conditions or site performed under water.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":13,"ChoiceName":"macaulay sampler","ChoiceLabel":"Macaulay sampler","ChoiceObsolete":0,"ChoiceDescription":"A hollow push tube with a hinged door that is driven into soft sediments (e.g., organics) and partially rotated to obtain an undisturbed sample.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"video","ChoiceLabel":"Video","ChoiceObsolete":0,"ChoiceDescription":"Electronically recoded, sequential digital images of a subaqueous setting/site.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1270,"DomainName":"observation_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"permafrost auger","ChoiceLabel":"Permafrost Auger","ChoiceObsolete":0,"ChoiceDescription":"Sample extracted by means of a permafrost auger. This auger is a tool for taking cores in ice and frozen soils. It takes a 7.62 cm (3 inch) diameter core and can be used to core several meters by hand and further if used with a vehicle mounted drill rig. Used in AK. Added to the list in 2016.","ColumnPhysicalName":"osdobsmethod","ColumnLogicalName":"osd_observation_method"} {"DomainID":1271,"DomainName":"pedon_purpose","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"crop yield data site","ChoiceLabel":"Crop yield data site","ChoiceObsolete":0,"ChoiceDescription":"Documentation gathered to associate agronomic data collection on a particular soil.","ColumnPhysicalName":"pedonpurpose","ColumnLogicalName":"pedon_desc_purpose"} {"DomainID":1271,"DomainName":"pedon_purpose","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":2,"ChoiceName":"soil survey inventory","ChoiceLabel":"Soil survey inventory","ChoiceObsolete":0,"ChoiceDescription":"Documentation gathered for general purposes of supporting the soil survey inventory.","ColumnPhysicalName":"pedonpurpose","ColumnLogicalName":"pedon_desc_purpose"} {"DomainID":1271,"DomainName":"pedon_purpose","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"forestry data site","ChoiceLabel":"Forestry data site","ChoiceObsolete":1,"ColumnPhysicalName":"pedonpurpose","ColumnLogicalName":"pedon_desc_purpose"} {"DomainID":1271,"DomainName":"pedon_purpose","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"full pedon description","ChoiceLabel":"Full pedon description","ChoiceObsolete":1,"ColumnPhysicalName":"pedonpurpose","ColumnLogicalName":"pedon_desc_purpose"} {"DomainID":1271,"DomainName":"pedon_purpose","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":5,"ChoiceName":"research site","ChoiceLabel":"Research site","ChoiceObsolete":0,"ChoiceDescription":"Site where research other than vegetation data is collected or repeated measurements are taken. Includes environmental monitoring site for precipitation, air/soil temperature or moisture, Snow Survey Snotel site.","ColumnPhysicalName":"pedonpurpose","ColumnLogicalName":"pedon_desc_purpose"} {"DomainID":1271,"DomainName":"pedon_purpose","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"range data site","ChoiceLabel":"Range data site","ChoiceObsolete":1,"ColumnPhysicalName":"pedonpurpose","ColumnLogicalName":"pedon_desc_purpose"} {"DomainID":1271,"DomainName":"pedon_purpose","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":7,"ChoiceName":"ecological site data","ChoiceLabel":"Ecological site data","ChoiceObsolete":0,"ChoiceDescription":"Documentation gathered to associate ecological data collection on a particular soil.","ColumnPhysicalName":"pedonpurpose","ColumnLogicalName":"pedon_desc_purpose"} {"DomainID":1271,"DomainName":"pedon_purpose","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":8,"ChoiceName":"laboratory sampling site","ChoiceLabel":"Laboratory sampling site","ChoiceObsolete":0,"ChoiceDescription":"Location where soil samples and description taken to be analyzed by laboratory; should have laboratory analysis results associated with point now or in near future.","ColumnPhysicalName":"pedonpurpose","ColumnLogicalName":"pedon_desc_purpose"} {"DomainID":1271,"DomainName":"pedon_purpose","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"technical soil services","ChoiceLabel":"Technical soil services","ChoiceObsolete":0,"ChoiceDescription":"Documentation gathered to provide onsite technical soil services to customer.","ColumnPhysicalName":"pedonpurpose","ColumnLogicalName":"pedon_desc_purpose"} 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{"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"wet, non-satiated","ChoiceLabel":"Wet, non-satiated","ChoiceObsolete":0,"ChoiceDescription":"=>0.01 to 1.0 (0.5 for coarse soils) kPA suction, (=>0.00001 bar to 0.01 bar, 0.005 for coarse soils). Water films are visible, sand grains and peds glisten, but no free water is present.","ColumnPhysicalName":"excavdifms","ColumnLogicalName":"excavation_difficulty_moist_st"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"wet, satiated","ChoiceLabel":"Wet, satiated","ChoiceObsolete":0,"ChoiceDescription":"<0.01 kPa (<0.00001 bar) suction; free water present.","ColumnPhysicalName":"excavdifms","ColumnLogicalName":"excavation_difficulty_moist_st"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"saturation","ChoiceLabel":"Saturation from capillary fringe","ChoiceObsolete":1,"ColumnPhysicalName":"excavdifms","ColumnLogicalName":"excavation_difficulty_moist_st"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"frozen","ChoiceLabel":"Frozen","ChoiceObsolete":1,"ColumnPhysicalName":"excavdifms","ColumnLogicalName":"excavation_difficulty_moist_st"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"dry","ChoiceLabel":"Dry","ChoiceObsolete":0,"ChoiceDescription":">1500 kPa (>15 bar) suction","ColumnPhysicalName":"obssoimoiststat","ColumnLogicalName":"observed_soil_moisture_status"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"very dry","ChoiceLabel":"Very dry","ChoiceObsolete":0,"ChoiceDescription":"Less than 0.35 of the 15 bar water retention.","ColumnPhysicalName":"obssoimoiststat","ColumnLogicalName":"observed_soil_moisture_status"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderately dry","ChoiceLabel":"Moderately dry","ChoiceObsolete":0,"ChoiceDescription":"0.35 to 0.8 of the 15 bar water retention.","ColumnPhysicalName":"obssoimoiststat","ColumnLogicalName":"observed_soil_moisture_status"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"slightly dry","ChoiceLabel":"Slightly dry","ChoiceObsolete":0,"ChoiceDescription":"0.8 to 1.0 of the 15 bar water retention.","ColumnPhysicalName":"obssoimoiststat","ColumnLogicalName":"observed_soil_moisture_status"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"moist","ChoiceLabel":"Moist","ChoiceObsolete":0,"ChoiceDescription":"=<1500 to 0.01 kPa ( =<15 bar to 0.00001 bar) suction.","ColumnPhysicalName":"obssoimoiststat","ColumnLogicalName":"observed_soil_moisture_status"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"slightly moist","ChoiceLabel":"Slightly moist","ChoiceObsolete":0,"ChoiceDescription":"15 bar suction to MWR (see SSM p 91).","ColumnPhysicalName":"obssoimoiststat","ColumnLogicalName":"observed_soil_moisture_status"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"moderately moist","ChoiceLabel":"Moderately moist","ChoiceObsolete":0,"ChoiceDescription":"MWR to UWR water content (see SSM p91).","ColumnPhysicalName":"obssoimoiststat","ColumnLogicalName":"observed_soil_moisture_status"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"very moist","ChoiceLabel":"Very moist","ChoiceObsolete":0,"ChoiceDescription":"UWR to 0.01 bar suction (see SSM p91).","ColumnPhysicalName":"obssoimoiststat","ColumnLogicalName":"observed_soil_moisture_status"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"wet","ChoiceLabel":"Wet","ChoiceObsolete":0,"ChoiceDescription":"<1.0 kPa, or <0.5 for coarse soils, (<0.01 bar or 0.005 for coarse soils) suction.","ColumnPhysicalName":"obssoimoiststat","ColumnLogicalName":"observed_soil_moisture_status"} {"DomainID":1272,"DomainName":"observed_soil_moisture_status","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"wet, non-satiated","ChoiceLabel":"Wet, non-satiated","ChoiceObsolete":0,"ChoiceDescription":"=>0.01 to 1.0 (0.5 for coarse soils) kPA suction, (=>0.00001 bar to 0.01 bar, 0.005 for coarse soils). 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It sometimes contains impurities such as calcite, iron oxide, or the remains of silicious and other organisims. It has a tough, splintery to conchoidal fracture and may be white or variously colored gray, green, blue, pink, red, yellow, brown, and black. 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{"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":118,"ChoiceValue":141,"ChoiceName":"schist and phyllite","ChoiceLabel":"Schist and phyllite","ChoiceObsolete":1,"ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":84,"ChoiceValue":142,"ChoiceName":"metamorphic, basic","ChoiceLabel":"Basic metamorphic rock","ChoiceObsolete":1,"ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":36,"ChoiceValue":143,"ChoiceName":"gneiss, biotite","ChoiceLabel":"Biotite gneiss","ChoiceObsolete":0,"ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} 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{"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":39,"ChoiceValue":147,"ChoiceName":"gneiss, migmatitic","ChoiceLabel":"Migmatitic gneiss","ChoiceObsolete":0,"ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":40,"ChoiceValue":148,"ChoiceName":"gneiss, muscovite-biotite","ChoiceLabel":"Muscovite-biotite gneiss","ChoiceObsolete":0,"ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":122,"ChoiceValue":149,"ChoiceName":"schist, graphitic","ChoiceLabel":"Graphitic schist","ChoiceObsolete":0,"ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":141,"ChoiceValue":150,"ChoiceName":"slate, sulfidic","ChoiceLabel":"Sulfidic slate","ChoiceObsolete":0,"ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":45,"ChoiceValue":151,"ChoiceName":"granitoid","ChoiceLabel":"Granitoid","ChoiceObsolete":0,"ChoiceDescription":"a) In the IUGS classification, a preliminary term for (for field use) for a plutonic rock with Q (quartz) between 20 and 40 (%). b) A general term for all phaneritic igneous rocks (mineral crystals visible unaided and all about the same size) dominated by quartz and feldspars.","ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":152,"ChoiceName":"bauxite","ChoiceLabel":"Bauxite","ChoiceObsolete":0,"ChoiceDescription":"An off-white to dark red brown weathered detritus or rock composed of aluminum oxides (mainly gibbsite with some boehmite and diaspore), iron hydroxides, silica, silt, and especially clay minerals. 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SW","ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":154,"ChoiceName":"anhydrite, rock","ChoiceLabel":"Rock anhydrite","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed chiefly of mineral anhydrite (anhydrous CaSO4); The rock is generally massive, cryptocrystalline, and may exhibit rhythmic sedimentation (rhymites). Compare - rock gypsum, rock halite. SW","ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":52,"ChoiceValue":155,"ChoiceName":"halite, rock","ChoiceLabel":"Rock halite","ChoiceObsolete":0,"ChoiceDescription":"A sedimentary rock (evaporite) composed primarily of halite (NaCl). SW","ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":78,"ChoiceValue":156,"ChoiceName":"limonite","ChoiceLabel":"Limonite","ChoiceObsolete":0,"ChoiceDescription":"A general 'field' term for various brown to yellowish brown, amorphous- to- cryptocrystalline hydrous ferric oxides that are an undetermined mixture of goethite, hematite, and lepidocrocite formed by weathering and iron oxidation from iron-bearing, rocks and minerals. SW & GG","ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":97,"ChoiceValue":157,"ChoiceName":"novaculite","ChoiceLabel":"Novaculite","ChoiceObsolete":0,"ChoiceDescription":"A dense, extremely finely grained, even-textured, siliceous, sedimentary rock similar to chert. 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Siltite differs from siltstone, mudstone, or shale in that it exhibits very low to low grade metamorphic or diagenetic layer silicate and feldspar alteration to sericite, chlorite, and albite (subgreenschist to greenschist metamorphic facies) (Maxwell, 1973; Kidder, 1987).","ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":121,"ChoiceValue":159,"ChoiceName":"schist, biotite","ChoiceLabel":"Biotite schist","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily biotite.","ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":124,"ChoiceValue":160,"ChoiceName":"schist, muscovite","ChoiceLabel":"Muscovite schist","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily muscovite.","ColumnPhysicalName":"pmorigin","ColumnLogicalName":"parent_material_origin"} {"DomainID":2587,"DomainName":"parent_material_origin","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":125,"ChoiceValue":161,"ChoiceName":"schist, sericite","ChoiceLabel":"Sericite schist","ChoiceObsolete":0,"ChoiceDescription":"A strongly foliated crystalline rock formed by dynamic metamorphism that has well-developed parallelism of more than 50 percent of the minerals present, primarily sericite. 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These are advance data, subject to change.\r\n\r\nNote that this certification status applies to only the legend object.","ColumnPhysicalName":"legendcertstat","ColumnLogicalName":"legend_certification_status"} {"DomainID":2589,"DomainName":"legend_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"partly certified","ChoiceLabel":"partly certified","ChoiceObsolete":0,"ChoiceDescription":"The data in the legend object, including mapunits, correlation notes, and area overlaps, have been appropriately populated and the data have been reviewed. At least some of the data elements have been certified for use in specific applications. Other data elements in the object have advance data, subject to change.\r\n\r\nNote that this certification status applies to only the legend object.","ColumnPhysicalName":"legendcertstat","ColumnLogicalName":"legend_certification_status"} {"DomainID":2589,"DomainName":"legend_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"certified","ChoiceLabel":"certified","ChoiceObsolete":0,"ChoiceDescription":"The data in the legend object, including mapunits, correlation notes, and area overlaps, have been appropriately populated, reviewed, and certified for general use.\r\n\r\nNote, that this certification status applies to only the legend object.","ColumnPhysicalName":"legendcertstat","ColumnLogicalName":"legend_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"not for distribution","ChoiceLabel":"not for distribution","ChoiceObsolete":0,"ChoiceDescription":"The data map unit object has been created, but is not populated or the data are preliminary and incomplete. The data are subject to major changes. A data mapunit with this status should not be interpreted, exported, or used by other applications.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"not certified","ChoiceLabel":"not certified","ChoiceObsolete":0,"ChoiceDescription":"The data in the data map unit object have been created and have been appropriately populated, at least in part, but the data have not been reviewed or certified. Data in some data elements in these tables may be more complete than in others. These are advance data, subject to change.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":9,"ChoiceValue":3,"ChoiceName":"partly certified","ChoiceLabel":"partly certified","ChoiceObsolete":1,"ChoiceDescription":"The data in the data map unit object have been appropriately populated and the data have been reviewed. At least some of the data elements have been certified for use in specific applications. Other data elements in the object have advance data, subject to change.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":10,"ChoiceValue":4,"ChoiceName":"certified","ChoiceLabel":"certified","ChoiceObsolete":1,"ChoiceDescription":"The data in the data map unit object have been appropriately populated, reviewed, and certified for general use.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":3,"ChoiceValue":5,"ChoiceName":"partly certified, all components","ChoiceLabel":"partly certified, all components","ChoiceObsolete":0,"ChoiceDescription":"The data for both major and minor components in the data mapunit object have been appropriately populated and the data have been reviewed. These data mapunits are typically associated with on-going projects. At least some of the data elements have been certified for use in specific applications. Other data elements in the object have advance data, subject to change.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":4,"ChoiceValue":6,"ChoiceName":"partly certified, major components","ChoiceLabel":"partly certified, major components","ChoiceObsolete":0,"ChoiceDescription":"The data for major components in the data mapunit object have been appropriately populated. Minor components are not intended for interpretation, and are populated with only a limited number of the most significant data elements. These data mapunits are typically associated with on-going projects. All the data have been reviewed, and at least some of the data elements have been certified for use in specific applications. Other data elements in the object have advance data, subject to change.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":5,"ChoiceValue":7,"ChoiceName":"partly certified, minimal data","ChoiceLabel":"partly certified, minimal data","ChoiceObsolete":0,"ChoiceDescription":"The data for major components in the data mapunit object have been populated and meet minimum standards, but some data elements are not appropriately populated. Minor components are not intended for interpretation, and are populated with only a limited number of the most significant data elements. These data mapunits are typically associated with initial soil surveys that were initiated years ago but are not yet completed. Data have received only a minimum amount of recent updating. The data mapunit does not have the level of quality and completeness equivalent to a recently populated dataset, but it is minimally acceptable. All the data have been reviewed, and at least some of the data elements have been certified for use in specific applications. Other data elements in the object are incomplete or have advance data, subject to change. Valid interpretations are available only for the major components with certified data elements, and some interpretations may be marginally valid.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":6,"ChoiceValue":8,"ChoiceName":"certified, all components","ChoiceLabel":"certified, all components","ChoiceObsolete":0,"ChoiceDescription":"The data for both major and minor components in the data mapunit object have been appropriately populated, reviewed, and certified for general use. Valid interpretations can be generated for all components.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":7,"ChoiceValue":9,"ChoiceName":"certified, major components","ChoiceLabel":"certified, major components","ChoiceObsolete":0,"ChoiceDescription":"The data for major components in the data mapunit object have been appropriately populated, reviewed, and certified for general use. Minor components are not intended for interpretation, and are populated with only a limited number of the most significant data elements. Valid interpretations can be generated for major components only.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2590,"DomainName":"dmu_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":8,"ChoiceValue":10,"ChoiceName":"certified, minimal data","ChoiceLabel":"certified, minimal data","ChoiceObsolete":0,"ChoiceDescription":"The data for major components in the data mapunit object have been populated, reviewed, and certified for general use. Minor components are not intended for interpretation, and are populated with only a limited number of the most significant data elements. These data mapunits are typically associated with initial soil surveys that were completed years ago. Data was originally populated under less stringent standards than are in place today, and data have received only a minimum amount of recent updating. The data mapunit does not have the level of quality and completeness equivalent to a recently populated dataset, but it is minimally acceptable and certifiable. Interpretations can be generated for major components only, and some interpretations may be only marginally valid.","ColumnPhysicalName":"dmucertstat","ColumnLogicalName":"dmu_certification_status"} {"DomainID":2591,"DomainName":"export_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":2,"ChoiceValue":1,"ChoiceName":"not certified","ChoiceLabel":"not certified","ChoiceObsolete":0,"ChoiceDescription":"The legend and data mapunits to be included in the export file have been appropriately populated, at least in part, but have not been reviewed or certified. These are advance data, subject to change. \r\n\r\nThis certification applies to the whole export package as a single entity.","ColumnPhysicalName":"exportcertstatus","ColumnLogicalName":"export_certification_status"} {"DomainID":2591,"DomainName":"export_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":8,"ChoiceValue":2,"ChoiceName":"partly certified","ChoiceLabel":"partly certified","ChoiceObsolete":1,"ChoiceDescription":"The legend and data mapunits to be included in the export file have been appropriately populated and the data have been reviewed. At least some of the data elements have been certified for use in specific applications. Other data elements in the export have advance data, subject to change.\r\n\r\nThis certification applies to the whole export package as a single entity.","ColumnPhysicalName":"exportcertstatus","ColumnLogicalName":"export_certification_status"} {"DomainID":2591,"DomainName":"export_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":9,"ChoiceValue":3,"ChoiceName":"fully certified","ChoiceLabel":"fully certified","ChoiceObsolete":1,"ChoiceDescription":"The legend and data mapunits to be included in the export file have been appropriately populated, reviewed, and certified for general use.\r\n\r\nThis certification applies to the whole export package as a single entity.","ColumnPhysicalName":"exportcertstatus","ColumnLogicalName":"export_certification_status"} {"DomainID":2591,"DomainName":"export_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":3,"ChoiceValue":4,"ChoiceName":"partly certified, all components","ChoiceLabel":"partly certified, all components","ChoiceObsolete":0,"ChoiceDescription":"This certification applies to the whole export package as a single entity. The legend and data mapunits to be included in the export file have been appropriately populated (both major and minor components) and the data elements have been reviewed. These datasets are typically exports from on-going projects. At least some of the data elements have been certified for use in specific applications. Other data elements in the export have advance data, subject to change. Both major and minor components are intended for interpretation. The components with uncertified data elements may not have valid interpretations.","ColumnPhysicalName":"exportcertstatus","ColumnLogicalName":"export_certification_status"} {"DomainID":2591,"DomainName":"export_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":4,"ChoiceValue":5,"ChoiceName":"partly certified, major components","ChoiceLabel":"partly certified, major components","ChoiceObsolete":0,"ChoiceDescription":"This certification applies to the whole export package as a single entity. The legend and data mapunits to be included in the export file have been appropriately populated (major components only) and the data elements have been reviewed. Minor components are not intended for interpretation, and are populated with only a limited number of data elements. These datasets are typically exports from on-going projects. At least some of the data elements have been certified for use in specific applications. Other data elements in the export have advance data, subject to change. The major components with uncertified data elements may not have valid interpretations. Minor components are not sufficiently populated to allow valid interpretations.","ColumnPhysicalName":"exportcertstatus","ColumnLogicalName":"export_certification_status"} {"DomainID":2591,"DomainName":"export_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":5,"ChoiceValue":6,"ChoiceName":"certified, all components","ChoiceLabel":"certified, all components","ChoiceObsolete":0,"ChoiceDescription":"This certification applies to the whole export package as a single entity. The legend and data mapunits to be included in the export file have been appropriately populated, reviewed, and certified for general use. Both major and minor components are fully populated. These datasets are typically exports from completed projects. Valid interpretations are available for both major and minor components.","ColumnPhysicalName":"exportcertstatus","ColumnLogicalName":"export_certification_status"} {"DomainID":2591,"DomainName":"export_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":6,"ChoiceValue":7,"ChoiceName":"certified, major components","ChoiceLabel":"certified, major components","ChoiceObsolete":0,"ChoiceDescription":"This certification applies to the whole export package as a single entity. The legend and data mapunits to be included in the export file have been appropriately populated (major components only). Minor components are not intended for interpretation, and are populated with only a limited number of data elements. Data have been reviewed and certified for general use. These datasets are typically exports from completed projects. Valid interpretations are available for major components only.","ColumnPhysicalName":"exportcertstatus","ColumnLogicalName":"export_certification_status"} {"DomainID":2591,"DomainName":"export_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":7,"ChoiceValue":8,"ChoiceName":"certified, minimal data","ChoiceLabel":"certified, minimal data","ChoiceObsolete":0,"ChoiceDescription":"This certification applies to the whole export package as a single entity. The legend and data mapunits to be included in the export file have been populated (major components only). Minor components are not intended for interpretation, and are populated with only a limited number of data elements. Data have been reviewed and certified for general use. These datasets are typically exports from initial soil surveys that were completed years ago. Data was originally populated under less stringent standards than are in place today, and data have received only a minimum amount of recent updating. The data in the export does not have the level of quality and completeness equivalent to a recently populated dataset, but it is minimally acceptable and certifiable. Valid interpretations are available for all soil map units but for major components only, and some interpretations may be marginally valid.","ColumnPhysicalName":"exportcertstatus","ColumnLogicalName":"export_certification_status"} {"DomainID":2591,"DomainName":"export_certification_status","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":1,"ChoiceValue":9,"ChoiceName":"status unknown, record inserted during conversion","ChoiceLabel":"status unknown, record inserted during conversion","ChoiceObsolete":0,"ColumnPhysicalName":"exportcertstatus","ColumnLogicalName":"export_certification_status"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":1,"ChoiceName":"site association, formatted","ChoiceLabel":"Site association, formatted","ChoiceObsolete":1,"ChoiceDescription":"A formatted note written at the time of describing a site, pedon. or horizon. This note may be included into the pedon description report.","ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":2,"ChoiceName":"site association, unformatted","ChoiceLabel":"Site association, unformatted","ChoiceObsolete":1,"ChoiceDescription":"A free-form note written at the time of describing a site, pedon. or horizon.","ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":3,"ChoiceName":"miscellaneous notes","ChoiceLabel":"Miscellaneous notes","ChoiceObsolete":0,"ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":4,"ChoiceName":"correlation notes","ChoiceLabel":"Correlation notes","ChoiceObsolete":1,"ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":5,"ChoiceName":"transect, formatted","ChoiceLabel":"Transect, formatted","ChoiceObsolete":0,"ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":6,"ChoiceName":"transect, unformatted","ChoiceLabel":"Transect, unformatted","ChoiceObsolete":0,"ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"transect methodology","ChoiceLabel":"Transect methodology","ChoiceObsolete":0,"ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":8,"ChoiceName":"windows pedon import issue","ChoiceLabel":"Windows Pedon import issue","ChoiceObsolete":0,"ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":9,"ChoiceName":"quality assurance","ChoiceLabel":"Quality assurance","ChoiceObsolete":0,"ChoiceDescription":"A text note related to Quality Assurance.","ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2812,"DomainName":"transect_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":10,"ChoiceName":"quality control","ChoiceLabel":"Quality control","ChoiceObsolete":0,"ChoiceDescription":"A text note related to Quality Control.","ColumnPhysicalName":"transecttextkind","ColumnLogicalName":"transect_text_kind"} {"DomainID":2817,"DomainName":"calculation_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":4,"ChoiceName":"miscellaneous notes","ChoiceLabel":"Miscellaneous notes","ChoiceObsolete":0,"ChoiceDescription":"Text entries not related to any of the other choices.","ColumnPhysicalName":"calctextkind","ColumnLogicalName":"calculation_text_kind"} {"DomainID":2817,"DomainName":"calculation_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":6,"ChoiceName":"edit notes","ChoiceLabel":"Edit notes","ChoiceObsolete":0,"ChoiceDescription":"Text entries that describe what changes were made to the data, and why those changes were made.","ColumnPhysicalName":"calctextkind","ColumnLogicalName":"calculation_text_kind"} {"DomainID":2820,"DomainName":"hydric_rating","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"yes","ChoiceLabel":"Yes","ChoiceObsolete":0,"ChoiceDescription":"The soil meets the criteria for hydric soils. Reference: NSSH Part 622.","ColumnPhysicalName":"hydricrating","ColumnLogicalName":"hydric_rating"} {"DomainID":2820,"DomainName":"hydric_rating","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"no","ChoiceLabel":"No","ChoiceObsolete":0,"ChoiceDescription":"The soil does not meet the criteria for hydric soils. Reference: NSSH Part 622.","ColumnPhysicalName":"hydricrating","ColumnLogicalName":"hydric_rating"} {"DomainID":2820,"DomainName":"hydric_rating","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"unranked","ChoiceLabel":"Unranked","ChoiceObsolete":0,"ChoiceDescription":"The soil has not yet been determined to either have or not have hydric criteria. Reference: NSSH Part 622.","ColumnPhysicalName":"hydricrating","ColumnLogicalName":"hydric_rating"} {"DomainID":2822,"DomainName":"rule_design","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":1,"ChoiceName":"limitation","ChoiceLabel":"limitation","ChoiceObsolete":0,"ChoiceDescription":"The rule is designed in a manner such that the higher the fuzzy value, the more limited the soil is for the stated use. The fuzzy values, of child-rules, closest to 1 represent the most limiting features and will be sorted in descending order.","ColumnPhysicalName":"ruledesign","ColumnLogicalName":"rule_design"} {"DomainID":2822,"DomainName":"rule_design","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":2,"ChoiceName":"suitability","ChoiceLabel":"suitability","ChoiceObsolete":0,"ChoiceDescription":"The rule is designed in a manner such that the higher the fuzzy value, the better suited the soil is for the stated use. The fuzzy values, of child-rules, closest to 0 represent the most limiting features and will be sorted in ascending order.","ColumnPhysicalName":"ruledesign","ColumnLogicalName":"rule_design"} {"DomainID":2822,"DomainName":"rule_design","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":3,"ChoiceName":"class","ChoiceLabel":"class","ChoiceObsolete":0,"ChoiceDescription":"The rule is designed to result in the soil being interpreted as a member of a discrete class. Reportable features are those with fuzzy values closest to 1. The fuzzy values of child-rules will be sorted in descending order.","ColumnPhysicalName":"ruledesign","ColumnLogicalName":"rule_design"} {"DomainID":3308,"DomainName":"correlation_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":1,"ChoiceName":"status change - added","ChoiceLabel":"Status change - added","ChoiceObsolete":0,"ChoiceDescription":"The map unit has just been added to the Mapunit table for this legend - generally with a status of provisional or approved.","ColumnPhysicalName":"corkind","ColumnLogicalName":"correlation_kind"} {"DomainID":3308,"DomainName":"correlation_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":2,"ChoiceName":"status change - dropped/combined","ChoiceLabel":"Status change - dropped/combined","ChoiceObsolete":0,"ChoiceDescription":"Documentation for map units that are removed from the list of active map units - changed to \"additional\" status. This would also apply to map units that are \"combined\" with other map units.","ColumnPhysicalName":"corkind","ColumnLogicalName":"correlation_kind"} {"DomainID":3308,"DomainName":"correlation_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":3,"ChoiceName":"status change - disapproved","ChoiceLabel":"Status change - disapproved","ChoiceObsolete":0,"ChoiceDescription":"Documentation as to why a provisional mapunit did not move to the approved list, or an approved one did not move to correlated. More study is needed to make the correlation decision.","ColumnPhysicalName":"corkind","ColumnLogicalName":"correlation_kind"} {"DomainID":3308,"DomainName":"correlation_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":4,"ChoiceName":"status change - reinstated","ChoiceLabel":"Status change - reinstated","ChoiceObsolete":0,"ChoiceDescription":"Documentation as to why a previously \"dropped\" map unit is revived and added to the list of active map units -- status generally changed from additional to approved or possibly correlated.","ColumnPhysicalName":"corkind","ColumnLogicalName":"correlation_kind"} {"DomainID":3308,"DomainName":"correlation_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":5,"ChoiceName":"name change","ChoiceLabel":"Name change","ChoiceObsolete":0,"ChoiceDescription":"Documentation regarding changing the name on an existing map unit. If the status is changed at the same time, the action should be coded as \"status change.\"","ColumnPhysicalName":"corkind","ColumnLogicalName":"correlation_kind"} {"DomainID":3308,"DomainName":"correlation_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":6,"ChoiceName":"symbol change","ChoiceLabel":"Symbol change","ChoiceObsolete":1,"ChoiceDescription":"Documentation regarding changing the mapunit symbol on an existing unit.","ColumnPhysicalName":"corkind","ColumnLogicalName":"correlation_kind"} {"DomainID":3308,"DomainName":"correlation_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":7,"ChoiceName":"notes to accompany","ChoiceLabel":"Notes to accompany","ChoiceObsolete":0,"ChoiceDescription":"Notes designed to be included with either the final correlation document or a field review report.","ColumnPhysicalName":"corkind","ColumnLogicalName":"correlation_kind"} {"DomainID":3308,"DomainName":"correlation_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":8,"ChoiceName":"join statement","ChoiceLabel":"Join statement","ChoiceObsolete":0,"ChoiceDescription":"Documentation regarding the joining of this map unit with those of surrounding soil survey areas.","ColumnPhysicalName":"corkind","ColumnLogicalName":"correlation_kind"} {"DomainID":3309,"DomainName":"correlation_event","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":1,"ChoiceName":"initial field review","ChoiceLabel":"Initial field review","ChoiceObsolete":0,"ColumnPhysicalName":"corevent","ColumnLogicalName":"correlation_event"} {"DomainID":3309,"DomainName":"correlation_event","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":2,"ChoiceName":"progress field review","ChoiceLabel":"Progress field review","ChoiceObsolete":0,"ColumnPhysicalName":"corevent","ColumnLogicalName":"correlation_event"} {"DomainID":3309,"DomainName":"correlation_event","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":3,"ChoiceName":"final field review","ChoiceLabel":"Final field review","ChoiceObsolete":0,"ColumnPhysicalName":"corevent","ColumnLogicalName":"correlation_event"} {"DomainID":3309,"DomainName":"correlation_event","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":4,"ChoiceName":"technical assist","ChoiceLabel":"Technical assist","ChoiceObsolete":0,"ColumnPhysicalName":"corevent","ColumnLogicalName":"correlation_event"} {"DomainID":3309,"DomainName":"correlation_event","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":5,"ChoiceName":"correlation team meeting","ChoiceLabel":"Correlation team meeting","ChoiceObsolete":0,"ColumnPhysicalName":"corevent","ColumnLogicalName":"correlation_event"} {"DomainID":3309,"DomainName":"correlation_event","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":6,"ChoiceName":"final correlation","ChoiceLabel":"Final correlation","ChoiceObsolete":0,"ColumnPhysicalName":"corevent","ColumnLogicalName":"correlation_event"} {"DomainID":3309,"DomainName":"correlation_event","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":7,"ChoiceName":"correlation amendment","ChoiceLabel":"Correlation amendment","ChoiceObsolete":0,"ColumnPhysicalName":"corevent","ColumnLogicalName":"correlation_event"} {"DomainID":3310,"DomainName":"soil_odor","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none","ChoiceLabel":"None","ChoiceObsolete":0,"ChoiceDescription":"no odor detected","ColumnPhysicalName":"osdsoilodor","ColumnLogicalName":"osd_soil_odor"} {"DomainID":3310,"DomainName":"soil_odor","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"petrochemical","ChoiceLabel":"Petrochemical","ChoiceObsolete":0,"ChoiceDescription":"The presence (smell) of gaseous or liquid gasoline, oil, creosote, etc.","ColumnPhysicalName":"osdsoilodor","ColumnLogicalName":"osd_soil_odor"} {"DomainID":3310,"DomainName":"soil_odor","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"sulfurous","ChoiceLabel":"Sulfurous","ChoiceObsolete":0,"ChoiceDescription":"Presence of H2S (hydrogen sulfide); rotten eggs; commonly associated with strongly reduced soil containing sulfur compounds.","ColumnPhysicalName":"osdsoilodor","ColumnLogicalName":"osd_soil_odor"} {"DomainID":3310,"DomainName":"soil_odor","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none","ChoiceLabel":"None","ChoiceObsolete":0,"ChoiceDescription":"no odor detected","ColumnPhysicalName":"soilodor","ColumnLogicalName":"soil_odor"} {"DomainID":3310,"DomainName":"soil_odor","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"petrochemical","ChoiceLabel":"Petrochemical","ChoiceObsolete":0,"ChoiceDescription":"The presence (smell) of gaseous or liquid gasoline, oil, creosote, etc.","ColumnPhysicalName":"soilodor","ColumnLogicalName":"soil_odor"} {"DomainID":3310,"DomainName":"soil_odor","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"sulfurous","ChoiceLabel":"Sulfurous","ChoiceObsolete":0,"ChoiceDescription":"Presence of H2S (hydrogen sulfide); rotten eggs; commonly associated with strongly reduced soil containing sulfur compounds.","ColumnPhysicalName":"soilodor","ColumnLogicalName":"soil_odor"} {"DomainID":4601,"DomainName":"dmf_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"indiana","ChoiceLabel":"Indiana","ChoiceObsolete":0,"ColumnPhysicalName":"dmfsite","ColumnLogicalName":"dmf_site"} {"DomainID":4601,"DomainName":"dmf_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":2,"ChoiceName":"montana","ChoiceLabel":"Montana","ChoiceObsolete":0,"ColumnPhysicalName":"dmfsite","ColumnLogicalName":"dmf_site"} {"DomainID":4601,"DomainName":"dmf_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":3,"ChoiceName":"missouri","ChoiceLabel":"Missouri","ChoiceObsolete":0,"ColumnPhysicalName":"dmfsite","ColumnLogicalName":"dmf_site"} {"DomainID":4601,"DomainName":"dmf_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":4,"ChoiceName":"ngmc","ChoiceLabel":"NGMC","ChoiceObsolete":0,"ColumnPhysicalName":"dmfsite","ColumnLogicalName":"dmf_site"} {"DomainID":4601,"DomainName":"dmf_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":5,"ChoiceName":"nevada","ChoiceLabel":"Nevada","ChoiceObsolete":0,"ColumnPhysicalName":"dmfsite","ColumnLogicalName":"dmf_site"} {"DomainID":4601,"DomainName":"dmf_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"oregon","ChoiceLabel":"Oregon","ChoiceObsolete":0,"ColumnPhysicalName":"dmfsite","ColumnLogicalName":"dmf_site"} {"DomainID":4601,"DomainName":"dmf_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"tennessee","ChoiceLabel":"Tennessee","ChoiceObsolete":0,"ColumnPhysicalName":"dmfsite","ColumnLogicalName":"dmf_site"} {"DomainID":4602,"DomainName":"editor_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"portland, or","ChoiceLabel":"Portland, OR","ChoiceObsolete":0,"ColumnPhysicalName":"editorsite","ColumnLogicalName":"editor_site"} {"DomainID":4602,"DomainName":"editor_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"davis, ca","ChoiceLabel":"Davis, CA","ChoiceObsolete":1,"ColumnPhysicalName":"editorsite","ColumnLogicalName":"editor_site"} {"DomainID":4602,"DomainName":"editor_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"reno, nv","ChoiceLabel":"Reno, NV","ChoiceObsolete":1,"ColumnPhysicalName":"editorsite","ColumnLogicalName":"editor_site"} {"DomainID":4602,"DomainName":"editor_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"bozeman, mt","ChoiceLabel":"Bozeman, MT","ChoiceObsolete":1,"ColumnPhysicalName":"editorsite","ColumnLogicalName":"editor_site"} {"DomainID":4602,"DomainName":"editor_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"salina, ks","ChoiceLabel":"Salina, KS","ChoiceObsolete":1,"ColumnPhysicalName":"editorsite","ColumnLogicalName":"editor_site"} {"DomainID":4602,"DomainName":"editor_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"lakewood, co","ChoiceLabel":"Lakewood, CO","ChoiceObsolete":0,"ColumnPhysicalName":"editorsite","ColumnLogicalName":"editor_site"} {"DomainID":4602,"DomainName":"editor_site","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"bismarck, 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For lichen growing on bare soil in dry rangeland conditions see cryptogamic crust.","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4889,"DomainName":"usfs_ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"litter and duff","ChoiceLabel":"Litter and duff","ChoiceObsolete":0,"ChoiceDescription":"Leaf and needle litter, and duff not yet incorporated into the decomposed top humus layer. Non-continuous litter is not included (for example, scattered needles over soil is classified as BARE.","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4889,"DomainName":"usfs_ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"moss","ChoiceLabel":"Moss","ChoiceObsolete":0,"ChoiceDescription":"Nonvascular, terrestrial green plant, including mosses, hornworts, and liverworts. Always herbaceous. This code does not apply to moss growing on bare soil in dry rangeland conditions. For rangeland conditions, see cryptogamic crusts.","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4889,"DomainName":"usfs_ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"non-vascular plant","ChoiceLabel":"Non-vascular plant","ChoiceObsolete":0,"ChoiceDescription":"Plants or plant-like organisms without specialized water or fluid conductive tissue (xylem and phloem). Includes mosses, liverworts, hornworts, lichens, algae, and bacterial soil crusts.","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4889,"DomainName":"usfs_ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"pavement","ChoiceLabel":"Pavement","ChoiceObsolete":0,"ChoiceDescription":"A natural, concentration of closely packed and polished stones at the soil surface in a desert (may or may not be an erosional lag).","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4889,"DomainName":"usfs_ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"permanent ice and snow","ChoiceLabel":"Permanent ice and snow","ChoiceObsolete":0,"ChoiceDescription":"Surface area covered by ice and snow at the time of plot measurement, considered permanent. For use when permanent ice and snow are not differentiated.","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4889,"DomainName":"usfs_ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"road","ChoiceLabel":"Road","ChoiceObsolete":0,"ChoiceDescription":"Improved roads, paved roads, gravel roads, improved dirt roads, and off-road vehicle trails regularly maintained or in long-term continuing use. Generally constructed using machinery. Includes cutbanks and fills.","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4889,"DomainName":"usfs_ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"transient ice and snow","ChoiceLabel":"Transient ice and snow","ChoiceObsolete":0,"ChoiceDescription":"Surface area covered by ice and snow at the time of plot measurement, considered transient. For use when permanent ice and snow are not differentiated.","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4889,"DomainName":"usfs_ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"water","ChoiceLabel":"Water","ChoiceObsolete":0,"ChoiceDescription":"Where the water table is above the ground surface during the growing season, such as streams, bogs, swamps, marshes, and ponds.","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4889,"DomainName":"usfs_ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"wood","ChoiceLabel":"Wood","ChoiceObsolete":0,"ChoiceDescription":"Woody material, slash, and debris; any woody material, small and large woody debris, regardless of depth. Litter and non-continuous litter are not included (for example, scattered needles over soil is classified as BARE).","ColumnPhysicalName":"usfsgrndcovtyp","ColumnLogicalName":"usfs_ground_cover_type"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":8,"ChoiceName":"Ia","ChoiceLabel":"Ia","ChoiceObsolete":0,"ChoiceDescription":"This unit is well suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The rapid permeability in the substratum is a concern. Backfilling absorption trenches with at least one foot of finer textured material or other site modifications may be necessary to slow the percolation rate enough to allow for thorough filtering of effluent.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":9,"ChoiceName":"Ib","ChoiceLabel":"Ib","ChoiceObsolete":0,"ChoiceDescription":"This unit is well suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The rapid permeability in the substratum and slopes greater than 20 percent in some areas are concerns. Backfilling absorption trenches with at least one foot of finer textured material or other site modifications may be necessary to slow the percolation rate enough to allow for thorough filtering of effluent. There may be less-sloping areas within the unit that are suitable for siting a septic system, or, if feasible, cut and fill site modifications may produce an acceptable area within the unit. An erosion prevention and sediment control plan is required by the State for construction on sites over 20 percent slope.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":10,"ChoiceName":"Ic","ChoiceLabel":"Ic","ChoiceObsolete":0,"ChoiceDescription":"This unit is well suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. With moderate permeability and slopes less than 20 percent, there are few limitations.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":11,"ChoiceName":"Id","ChoiceLabel":"Id","ChoiceObsolete":0,"ChoiceDescription":"This unit is well suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. Slopes greater than 20 percent in some areas are a concern. There may be less-sloping areas within the unit that are suitable for siting a septic system, or, if feasible, cut and fill site modifications may produce an acceptable area within the unit. An erosion prevention and sediment control plan is required by the State for construction on sites over 20 percent slope.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":12,"ChoiceName":"IIa","ChoiceLabel":"IIa","ChoiceObsolete":0,"ChoiceDescription":"This unit is moderately suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The slow permeability in the substratum is the primary concern. Mound system construction and other site modifications may be necessary.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":13,"ChoiceName":"IIb","ChoiceLabel":"IIb","ChoiceObsolete":0,"ChoiceDescription":"This unit is moderately suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The slow permeability in the substratum and slopes greater than 20 percent in some areas are the primary concerns. Mound system construction and other site modifications may be necessary. There may be less-sloping areas within the unit that are suitable for siting a septic system, or, if feasible, cut and fill site modifications may produce an acceptable area within the unit. An erosion prevention and sediment control plan is required by the State for construction on sites over 20 percent slope.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":14,"ChoiceName":"IIc","ChoiceLabel":"IIc","ChoiceObsolete":0,"ChoiceDescription":"This unit is moderately suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The depth to bedrock in some areas is the primary concern. A significant percentage of this map unit has sufficient soil depth over bedrock to accept a range of designs. On-site investigations can help avoid areas with limited depth to bedrock. Additional fill material may be needed in some areas in order to meet the separation distance requirement between the bottom of the leachfield and bedrock.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":15,"ChoiceName":"IId","ChoiceLabel":"IId","ChoiceObsolete":0,"ChoiceDescription":"This unit is moderately suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The depth to bedrock and slopes greater than 20 percent in some areas are the primary concerns. A significant percentage of this map unit has sufficient soil depth over bedrock to accept a range of designs. On-site investigations can help avoid areas with limited depth to bedrock. Additional fill material may be needed in some areas in order to meet the separation distance requirement between the bottom of the leachfield and bedrock. There may be less-sloping areas within the unit that are suitable for siting a septic system, or, if feasible, cut and fill site modifications may produce an acceptable area within the unit. An erosion prevention and sediment control plan is required by the State for construction on sites over 20 percent slope.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":16,"ChoiceName":"IIe","ChoiceLabel":"IIe","ChoiceObsolete":0,"ChoiceDescription":"This unit is moderately suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The rapid permeability in the substratum and slopes greater than 20 percent are the primary concerns. Backfilling absorption trenches and beds with at least one foot of finer textured material, or other site modifications, may be necessary to slow the percolation rate enough to allow for thorough filtering of effluent. Cut and fill site modifications may produce an acceptable area within the unit. An erosion prevention and sediment control plan is required by the State for construction on sites over 20 percent slope","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":17,"ChoiceName":"IIf","ChoiceLabel":"IIf","ChoiceObsolete":0,"ChoiceDescription":"This unit is moderately suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. Slopes greater than 20 percent are the primary concern. Cut and fill site modifications may produce an acceptable area within the unit. An erosion prevention and sediment control plan is required by the State for construction on sites over 20 percent slope.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":18,"ChoiceName":"IIg","ChoiceLabel":"IIg","ChoiceObsolete":1,"ChoiceDescription":"This unit is moderately suited as a site for on-site waste disposal, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2002 Environmental Protection Rules. Flooding from surface waters is the primary concern. Locating the septic system on the highest part of the floodplain and with the maximum setback from surface waters is recommended.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":19,"ChoiceName":"IIh","ChoiceLabel":"IIh","ChoiceObsolete":0,"ChoiceDescription":"This unit is moderately suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The depth to the seasonal high water table is the primary concern. Mound system construction and other site modifications are often necessary. On sloping sites, curtain drains can help lower the water table to an acceptable level. In some cases, a detailed, site-specific analysis with groundwater level monitoring and determination of induced groundwater mounding may be required to establish the suitability of this unit.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":20,"ChoiceName":"IIIa","ChoiceLabel":"IIIa","ChoiceObsolete":0,"ChoiceDescription":"This unit is marginally suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The depth to bedrock is the major limitation. On-site investigations are needed to locate areas with sufficient soil depth. A significant percentage of the soils in this unit are less than 18 inches to bedrock and are not suitable as a site. However, there may be deeper areas that are suitable. Additional fill material may be needed in some areas in order to meet the separation distance requirement between the bottom of the leachfield and bedrock.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":21,"ChoiceName":"IIIb","ChoiceLabel":"IIIb","ChoiceObsolete":0,"ChoiceDescription":"This unit is marginally suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The hazard of flooding and the depth to the seasonal high water table are the major limitations. This unit is on floodplains and typically includes land in the floodway and the special flood hazard area. Consult flood hazard maps prepared by the Federal Emergency Management Agency (FEMA) in local town offices for more information. Wastewater systems must be located, designed and constructed in a manner that avoids impairment to the system and contamination from the system due to flooding. A detailed, site-specific analysis with groundwater level monitoring and determination of induced groundwater mounding may be required to establish the suitability of this unit. Mound system construction and other site modifications are often necessary.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":22,"ChoiceName":"IIIc","ChoiceLabel":"IIIc","ChoiceObsolete":0,"ChoiceDescription":"This unit is marginally suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The depth to the seasonal high water table in association with the minimal slope is the major limitation. A detailed, site-specific analysis is generally required. On-site groundwater level monitoring and determination of induced groundwater mounding is often necessary to establish the suitability of this unit. Curtain drains may help lower the water table to an acceptable level, however, the minimal slope may prevent their use in many areas.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":23,"ChoiceName":"IIId","ChoiceLabel":"IIId","ChoiceObsolete":0,"ChoiceDescription":"This unit is marginally suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The depth to the seasonal high water table is the major limitation. A detailed, site-specific analysis is generally required. On-site groundwater level monitoring and determination of induced groundwater mounding is often necessary to establish the suitability of this unit. Curtain drains may help lower the water table to an acceptable level.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":24,"ChoiceName":"IIIe","ChoiceLabel":"IIIe","ChoiceObsolete":0,"ChoiceDescription":"This unit is marginally suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The depth to the seasonal high water table and slopes greater than 20 percent in some areas are the major limitations. A detailed, site-specific analysis is generally required. On-site groundwater level monitoring and determination of induced groundwater mounding is often necessary to establish the suitability of this unit. Curtain drains may help lower the water table to an acceptable level. There may be less-sloping areas within the unit that are suitable for siting a septic system, or, if feasible, cut and fill site modifications may produce an acceptable area within the unit. An erosion prevention and sediment control plan is required by the State for construction on sites over 20 percent slope.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":25,"ChoiceName":"IIIf","ChoiceLabel":"IIIf","ChoiceObsolete":0,"ChoiceDescription":"This unit is marginally suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The depth to the seasonal high water table and the restricted depth to bedrock in some areas are the major limitations. On-site investigations can help avoid areas with limited depth to bedrock. Additional fill material may be needed in some areas in order to meet the separation distance requirement between the bottom of the leachfield and bedrock. A detailed, site-specific analysis with groundwater level monitoring and determination of induced groundwater mounding may be required to establish the suitability of this unit. Mound system construction and other site modifications are often necessary. On sloping sites, curtain drains can help lower the water table to an acceptable level.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":26,"ChoiceName":"IVa","ChoiceLabel":"IVa","ChoiceObsolete":0,"ChoiceDescription":"This unit is generally not suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. Excessive soil wetness in association with the minimal slope is the limiting condition. Prolonged periods of saturation at or near the soil surface do not allow for the proper functioning of septic systems.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":27,"ChoiceName":"IVb","ChoiceLabel":"IVb","ChoiceObsolete":0,"ChoiceDescription":"This unit is generally not suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. Steep slopes in association with the depth to bedrock is the limiting condition. Cut and fill site modifications that reduce the slope gradient are difficult to achieve due to the depth to bedrock.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":28,"ChoiceName":"IVc","ChoiceLabel":"IVc","ChoiceObsolete":0,"ChoiceDescription":"This unit is generally not suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The very shallow to shallow depth to bedrock is the limiting condition.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":29,"ChoiceName":"IVd","ChoiceLabel":"IVd","ChoiceObsolete":0,"ChoiceDescription":"This unit is generally not suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. Steep slopes in association with the slowly permeable substratum is the limiting condition. Cut and fill site modifications that reduce the slope gradient are not generally effective due to the slowly permeable substratum.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":30,"ChoiceName":"V","ChoiceLabel":"V","ChoiceObsolete":0,"ChoiceDescription":"This unit is not rated as a site for soil-based residential wastewater disposal systems. Due to the variable nature of the soils, on-site investigations are needed to determine their suitability.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4890,"DomainName":"vt_septic_system_class_2007","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":31,"ChoiceName":"IIIg","ChoiceLabel":"IIIg","ChoiceObsolete":0,"ChoiceDescription":"This unit is marginally suited as a site for soil-based residential wastewater disposal systems, based on a review by the Natural Resources Conservation Service of criteria set forth in the Vermont 2007 Environmental Protection Rules. The hazard of flooding is the major limitation. This unit is on floodplains and typically includes land in the floodway and the special flood hazard area. Consult flood hazard maps prepared by the Federal Emergency Management Agency (FEMA) in local town offices for more information. Wastewater systems must be located, designed and constructed in a manner that avoids impairment to the system and contamination from the system due to flooding.","ColumnPhysicalName":"vtsepticsyscl","ColumnLogicalName":"vt_septic_system_class"} {"DomainID":4891,"DomainName":"human_artifact_safety","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"innocuous artifacts","ChoiceLabel":"Innocuous artifacts","ChoiceObsolete":0,"ChoiceDescription":"Artifacts considered to be harmless to living beings. Examples include untreated wood products, iron, bricks, cinder blocks, concrete, plastic, glass, rubber, organic fibers, inorganic fibers, unprinted paper and cardboard, and some mineral and metal products. Any sharp innocuous artifacts can cause injury, but the materials themselves are still considered innocuous.","ColumnPhysicalName":"huartsafety","ColumnLogicalName":"human_artifact_safety"} {"DomainID":4891,"DomainName":"human_artifact_safety","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"noxious artifacts","ChoiceLabel":"Noxious artifacts","ChoiceObsolete":0,"ChoiceDescription":"Artifacts that are potentially harmful or destructive to living beings unless dealt with carefully. The harm may be immediate or long-term, or through direct or indirect contact. Examples include Arsenic-treated wood products, batteries, waste and garbage, radioactive fallout, liquid petroleum products, asphalt, coal ash, paper printed with metallic ink, and some mineral and metal products.","ColumnPhysicalName":"huartsafety","ColumnLogicalName":"human_artifact_safety"} {"DomainID":4891,"DomainName":"human_artifact_safety","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"innocuous artifacts","ChoiceLabel":"Innocuous artifacts","ChoiceObsolete":0,"ChoiceDescription":"Artifacts considered to be harmless to living beings. Examples include untreated wood products, iron, bricks, cinder blocks, concrete, plastic, glass, rubber, organic fibers, inorganic fibers, unprinted paper and cardboard, and some mineral and metal products. Any sharp innocuous artifacts can cause injury, but the materials themselves are still considered innocuous.","ColumnPhysicalName":"osdhuartsafety","ColumnLogicalName":"osd_human_artifact_safety"} {"DomainID":4891,"DomainName":"human_artifact_safety","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"noxious artifacts","ChoiceLabel":"Noxious artifacts","ChoiceObsolete":0,"ChoiceDescription":"Artifacts that are potentially harmful or destructive to living beings unless dealt with carefully. The harm may be immediate or long-term, or through direct or indirect contact. Examples include Arsenic-treated wood products, batteries, waste and garbage, radioactive fallout, liquid petroleum products, asphalt, coal ash, paper printed with metallic ink, and some mineral and metal products.","ColumnPhysicalName":"osdhuartsafety","ColumnLogicalName":"osd_human_artifact_safety"} {"DomainID":4892,"DomainName":"human_artifact_cohesion","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"cohesive","ChoiceLabel":"Cohesive","ChoiceObsolete":0,"ChoiceDescription":"Artifacts adhere together sufficiently so that they can not be easily broken into <2 mm size pieces either by hand or with a simple crushing device such as a mortar and pestle.","ColumnPhysicalName":"huartco","ColumnLogicalName":"human_artifact_cohesion"} {"DomainID":4892,"DomainName":"human_artifact_cohesion","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"noncohesive","ChoiceLabel":"Noncohesive","ChoiceObsolete":0,"ChoiceDescription":"Artifacts are easily broken into <2 mm size pieces either by hand or with a simple crushing device such as a mortar and pestle. They are similar to pararock fragments and will be incorporated into fine-earth fraction of the soil during routine laboratory sample preparation.","ColumnPhysicalName":"huartco","ColumnLogicalName":"human_artifact_cohesion"} {"DomainID":4892,"DomainName":"human_artifact_cohesion","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"cohesive","ChoiceLabel":"Cohesive","ChoiceObsolete":0,"ChoiceDescription":"Artifacts adhere together sufficiently so that they can not be easily broken into <2 mm size pieces either by hand or with a simple crushing device such as a mortar and pestle.","ColumnPhysicalName":"osdhuartco","ColumnLogicalName":"osd_human_artifact_cohesion"} {"DomainID":4892,"DomainName":"human_artifact_cohesion","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"noncohesive","ChoiceLabel":"Noncohesive","ChoiceObsolete":0,"ChoiceDescription":"Artifacts are easily broken into <2 mm size pieces either by hand or with a simple crushing device such as a mortar and pestle. They are similar to pararock fragments and will be incorporated into fine-earth fraction of the soil during routine laboratory sample preparation.","ColumnPhysicalName":"osdhuartco","ColumnLogicalName":"osd_human_artifact_cohesion"} {"DomainID":4893,"DomainName":"human_artifact_persistence","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"nonpersistent","ChoiceLabel":"Nonpersistent","ChoiceObsolete":0,"ChoiceDescription":"The artifact is susceptible to relatively rapid weathering or decay and is expected to be lost from the soil in less than a decade.","ColumnPhysicalName":"huartper","ColumnLogicalName":"human_artifact_persistence"} {"DomainID":4893,"DomainName":"human_artifact_persistence","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"persistent","ChoiceLabel":"Persistent","ChoiceObsolete":0,"ChoiceDescription":"The artifact is expected to remain intact in the soil for a decade or more.","ColumnPhysicalName":"huartper","ColumnLogicalName":"human_artifact_persistence"} {"DomainID":4893,"DomainName":"human_artifact_persistence","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"nonpersistent","ChoiceLabel":"Nonpersistent","ChoiceObsolete":0,"ChoiceDescription":"The artifact is susceptible to relatively rapid weathering or decay and is expected to be lost from the soil in less than a decade.","ColumnPhysicalName":"osdhuartper","ColumnLogicalName":"osd_human_artifact_persistence"} {"DomainID":4893,"DomainName":"human_artifact_persistence","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"persistent","ChoiceLabel":"Persistent","ChoiceObsolete":0,"ChoiceDescription":"The artifact is expected to remain intact in the soil for a decade or more.","ColumnPhysicalName":"osdhuartper","ColumnLogicalName":"osd_human_artifact_persistence"} 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{"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":12,"ChoiceValue":5,"ChoiceName":"a5","ChoiceLabel":"A5 Stratified Layers","ChoiceObsolete":0,"ChoiceDescription":"Several stratified layers startingat a depth of less than or equal to 15 cm (6 inches) from the soil surface. At least one of the layers has value of 3 or less and chroma of 1 or less, or it is muck, mucky peat, peat, or a mucky modified mineral texture. The remaining layers have chroma of 2 or less. For any sandy material that constitutes the layer with value of 3 or less and chroma of 1 or less, at least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":13,"ChoiceValue":6,"ChoiceName":"a6","ChoiceLabel":"A6 Organic Bodies","ChoiceObsolete":0,"ChoiceDescription":"Presence of 2 percent or more organic bodies of muck or a mucky modified mineral texture starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":14,"ChoiceValue":7,"ChoiceName":"a7","ChoiceLabel":"A7 5 cm Mucky Mineral","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky modified mineral soil material 5 cm (2 inches) or more thick, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":15,"ChoiceValue":8,"ChoiceName":"a8","ChoiceLabel":"A8 Muck Presence","ChoiceObsolete":0,"ChoiceDescription":"A layer of muck with value of 3 or less and chroma of 1 or less, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":16,"ChoiceValue":9,"ChoiceName":"a9","ChoiceLabel":"A9 1 cm Muck","ChoiceObsolete":0,"ChoiceDescription":"A layer of muck 1 cm (0.5 inch) or more thick with value of 3 or less and chroma of 1 or less and starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":2,"ChoiceValue":10,"ChoiceName":"a10","ChoiceLabel":"A10 2 cm Muck","ChoiceObsolete":0,"ChoiceDescription":"A layer of muck 2 cm (0.75 inch) or more thick with value of 3 or less and chroma of 1 or less, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":3,"ChoiceValue":11,"ChoiceName":"a11","ChoiceLabel":"A11 Depleted Below Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer with a depleted or gleyed matrix that has 60 percent or more chroma of 2 or less, starting at a depth of less than or equal to 30 cm (12 inches) from the soil surface, and having a minimum thickness of either:\r\n a. 15 cm (6 inches), or \r\n b. 5 cm (2 inches) if the 5 cm consists of fragmental soil material.\r\n\r\nOrganic, loamy or clayey layer(s) above the depleted or gleyed matrix must have value of 3 or less and chroma of 2 or less starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface and extend to the depleted or gleyed matrix. Any sandy material above the depleted or gleyed matrix must have value of 3 or less and chroma of 1 or less starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface and extend to the depleted or gleyed matrix. Viewed through a10x or 15x hand lens, at least 70 percent of the visible soil particles must be masked with organic material. Observed without a hand lens, the particles appear to be close to 100 percent masked.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":4,"ChoiceValue":12,"ChoiceName":"a12","ChoiceLabel":"A12 Thick Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer at least 15 cm (6 inches) thick with a depleted or gleyed matrix that has 60 percent or more chroma of 2 or less starting below 30 cm (12 inches) of the surface. The layer(s) above the depleted or gleyed matrix and starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface must have value of 2.5 or less and chroma of 1 or less to a depth of at least 30 cm (12 inches) and value of 3 or less and chroma of 1 or less in any remaining layers above the depleted or gleyed matrix. \r\nIn any sandy material above the depleted or gleyed matrix, at least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":5,"ChoiceValue":13,"ChoiceName":"a13","ChoiceLabel":"A13 Alaska Gleyed","ChoiceObsolete":0,"ChoiceDescription":"A mineral layer with a dominant hue of N, 10Y, 5GY, 10GY, 5G, 10G, 5BG, 10BG, 5B, 10B, or 5PB and with value of 4 or more in more than 50 percent of the matrix. The layer starts at a depth of less than or equal to 30 cm (12 inches) from the mineral surface and is underlain at a depth of less than or equal to 1.5 m (60 inches) from the soil surface by soil material with hue of 5Y or redder in the same type of parent material.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":6,"ChoiceValue":14,"ChoiceName":"a14","ChoiceLabel":"A14 Alaska Redox","ChoiceObsolete":0,"ChoiceDescription":"A mineral layer that has dominant hue of 5Y with chroma of 3 or less, or a gleyed matrix, with 10 percent or more distinct or prominent redox concentrations occurring as pore linings with value and chroma of 4 or more. The layer occurs at a depth of less than or equal to 30 cm (12 inches) from the soil surface.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":7,"ChoiceValue":15,"ChoiceName":"a15","ChoiceLabel":"A15 Alaska Gleyed Pores","ChoiceObsolete":0,"ChoiceDescription":"A mineral layer that has 10 percent or more hue of N, 10Y, 5GY, 10GY, 5G, 10G, 5BG, 10BG, 5B, 10B, or 5PB with value of 4 or more along root channels or other pores and that starts at a depth of less than or equal to 30 cm (12 inches) from the soil surface. The matrix has a dominant hue of 5Y or redder.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":8,"ChoiceValue":16,"ChoiceName":"a16","ChoiceLabel":"A16 Coast Prairie Redox","ChoiceObsolete":0,"ChoiceDescription":"A layer starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface that is at least 10 cm (4 inches) thick and has a matrix chroma of 3 or less with 2 percent or more distinct or prominent redox concentrations occurring as soft masses and/or pore linings.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":34,"ChoiceValue":17,"ChoiceName":"s1","ChoiceLabel":"S1 Sandy Mucky Mineral","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky modified sandy soil material 5 cm (2 inches) or more thick starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":35,"ChoiceValue":18,"ChoiceName":"s2","ChoiceLabel":"S2 2.5 cm Mucky Peat or Peat","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky peat or peat 2.5 cm (1 inch) or more thick with value of 4 or less and chroma of 3 or less, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface, and underlain by sandy soil material.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":36,"ChoiceValue":19,"ChoiceName":"s3","ChoiceLabel":"S3 5 cm Mucky Peat or Peat","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky peat or peat 5 cm (2 inches) or more thick with value of 3 or less and chroma of 2 or less, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface, and underlain by sandy soil material.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":37,"ChoiceValue":20,"ChoiceName":"s4","ChoiceLabel":"S4 Sandy Gleyed Matrix","ChoiceObsolete":0,"ChoiceDescription":"A gleyed matrix that occupies 60 percent or more of a layer starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":38,"ChoiceValue":21,"ChoiceName":"s5","ChoiceLabel":"S5 Sandy Redox","ChoiceObsolete":0,"ChoiceDescription":"A layer starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface that is at least 10 cm (4 inches) thick and has a matrix with 60 percent or more chroma of 2 or less and 2 percent or more distinct or prominent redox concentrations occurring as soft masses and/or pore linings.\r\n","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":39,"ChoiceValue":22,"ChoiceName":"s6","ChoiceLabel":"S6 Stripped Matrix","ChoiceObsolete":0,"ChoiceDescription":"A layer starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface in which iron-manganese oxides and/or organic matter have been stripped from the matrix and the primary base color of the soil material has been exposed. The stripped areas and translocated oxides and/or organic matter form a faintly contrasting pattern of two or more colors with diffuse boundaries. The stripped zones are 10 percent or more of the volume and are rounded.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":40,"ChoiceValue":23,"ChoiceName":"s7","ChoiceLabel":"S7 Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer 10 cm (4 inches) thick, starting at a depth of less than or equal to the upper 15 cm (6 inches) from the soil surface, with a matrix value 3 of or less and chroma of 1 or less. At least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked. The matrix color of the layer directly below the dark layer must have the same colors as those described above or any color that has chroma of 2 or less.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":41,"ChoiceValue":24,"ChoiceName":"s8","ChoiceLabel":"S8 Polyvalue Below Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer with value of 3 or less and chroma of 1 or less starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface. At least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked. Directly below this layer, 5 percent or more of the soil volume has value of 3 or less and chroma of 1 or less, and the remainder of the soil volume has value of 4 or more and chroma of 1 or less to a depth of 30 cm (12 inches) or to the spodic horizon, whichever is less.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":42,"ChoiceValue":25,"ChoiceName":"s9","ChoiceLabel":"S9 Thin Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer 5 cm (2 inches) or more thick, at a depth of less than or equal to 15 cm (6 inches) from the soil surface, with value of 3 or less and chroma of 1 or less. At least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked. This layer is underlain by a layer or layers with value of 4 or less and chroma of 1 or less to a depth of 30 cm (12 inches) or to the spodic horizon, whichever is less.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":17,"ChoiceValue":26,"ChoiceName":"f1","ChoiceLabel":"F1 Loamy Mucky Mineral","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky modified loamy or clayey soil material 10 cm (4 inches) or more thick starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":26,"ChoiceValue":27,"ChoiceName":"f2","ChoiceLabel":"F2 Loamy Gleyed Matrix","ChoiceObsolete":0,"ChoiceDescription":"A gleyed matrix that occupies 60 percent or more of a layer starting at a depth of less than or equal to 30 cm (12 inches) from the soil surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":29,"ChoiceValue":28,"ChoiceName":"f3","ChoiceLabel":"F3 Depleted Matrix","ChoiceObsolete":0,"ChoiceDescription":"A layer that has a depleted matrix with 60 percent or more chroma of 2 or less and that has a minimum thickness of either:\r\n a. 5 cm (2 inches) if the 5 cm is entirely at a depth of less than or equal to 15 cm (6 inches) from the soil surface, or \r\n b. 15 cm (6 inches), at a depth of less than or equal to 25 cm (10 inches) from the soil surface surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":30,"ChoiceValue":29,"ChoiceName":"f6","ChoiceLabel":"F6 Redox Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer that is at least 10 cm (4 inches) thick, is at a depth of less than or equal to 20 cm (8 inches) of the mineral soil surface, and has:\r\n a. Matrix value of 3 or less and chroma of 1 or less and 2 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings, or\r\n b. Matrix value of 3 or less and chroma of 2 or less and 5 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":31,"ChoiceValue":30,"ChoiceName":"f7","ChoiceLabel":"F7 Depleted Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"Redox depletions with value of 5 or more and chroma of 2 or less in a layer that is at least 10 cm (4 inches) thick, is at a depth of less than or equal to 20 cm (8 inches) from the mineral soil surface, and has:\r\n a. Matrix value of 3 or less and chroma of 1 or less and 10 percent or more redox depletions, or\r\n b. Matrix value of 3 or less and chroma of 2 or less and 20 percent or more redox depletions.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":32,"ChoiceValue":31,"ChoiceName":"f8","ChoiceLabel":"F8 Redox Depressions","ChoiceObsolete":0,"ChoiceDescription":"In closed depressions subject to ponding, 5 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings in a layer that is 5 cm (2 inches) or more thick and is at a depth of less than or equal to 10 cm (4 inches) from the soil surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":33,"ChoiceValue":32,"ChoiceName":"f9","ChoiceLabel":"F9 Vernal Pools","ChoiceObsolete":1,"ChoiceDescription":"In closed depressions that are subject to ponding, presence of a depleted matrix with 60 percent or more chroma of 2 or less in a layer 5 cm (2 inches) thick entirely within the upper 15 cm (6 inches) of the soil.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":18,"ChoiceValue":33,"ChoiceName":"f10","ChoiceLabel":"F10 Marl","ChoiceObsolete":0,"ChoiceDescription":"A layer of marl with value of 5 or more and chroma less than 2 starting at a depth of less than or equal to 10 cm (4 inches) from the soil surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":19,"ChoiceValue":34,"ChoiceName":"f11","ChoiceLabel":"F11 Depleted Ochric","ChoiceObsolete":0,"ChoiceDescription":"A layer(s) 10 cm (4 inches) or more thick in which 60 percent or more of the matrix has value of 4 or more and chroma of 1 or less. The layer is at a depth of less than or equal to 25 cm (10 inches) from the soil surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":20,"ChoiceValue":35,"ChoiceName":"f12","ChoiceLabel":"F12 Iron-Manganese Masses","ChoiceObsolete":0,"ChoiceDescription":"On flood plains, a layer 10 cm (4 inches) or more thick with 40 percent or more chroma of 2 or less and 2 percent or more distinct or prominent redox concentrations occurring as soft iron-manganese masses with diffuse boundaries. The layer occurs at a depth of less than or equal to 20 cm (8 inches) from the soil surface. Iron-manganese masses have value and chroma of 3 or less. Most commonly, they are black. The thickness requirement is waived if the layer is the mineral surface layer","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":21,"ChoiceValue":36,"ChoiceName":"f13","ChoiceLabel":"F13 Umbric Surface","ChoiceObsolete":0,"ChoiceDescription":"In depressions and other concave landforms, a layer 25 cm (10 inches) or more thick, starting at a depth of less than or equal to 15 cm (6 inches) fromthe soil surface, in which the upper 15 cm (6 inches) has value of 3 or less and chroma of 1 or less and in which the lower 10 cm (4 inches) has the same colors as those described above or any other color that has chroma of 2 or less.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":22,"ChoiceValue":37,"ChoiceName":"f16","ChoiceLabel":"F16 High Plains Depressions","ChoiceObsolete":0,"ChoiceDescription":"In closed depressions that are subject to ponding, a mineral soil that has chroma of 1 or less to a depth of at least 35 cm (13.5 inches) and a layer at least 10 cm (4 inches) thick starting at a depth of less than or equal to 35 cm (13.5 inches) from the mineral soil that has either:\r\n a. 1 percent or more redox concentrations occurring as nodules or concretions, or\r\n b. Redox concentrations occurring as nodules or concretions with distinct or prominent corona.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":23,"ChoiceValue":38,"ChoiceName":"f17","ChoiceLabel":"F17 Delta Ochric","ChoiceObsolete":0,"ChoiceDescription":"A layer 10 cm (4 inches) or more thick in which 60 percent or more of the matrix has value of 4 or more and chroma of 2 or less and there are no redox concentrations. This layer occurs at a depth of less than or equal to 20 cm (8 inches) of the soil.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":24,"ChoiceValue":39,"ChoiceName":"f18","ChoiceLabel":"F18 Reduced Vertic","ChoiceObsolete":0,"ChoiceDescription":"In Vertisols and Vertic intergrades, a positive reaction to alpha-alpha-dipyridyl that:\r\n a. Is the dominant (60 percent or more) condition of a layer at least 4 inches thick at a depth of less than or equal to (30 cm) 12 inches from the soil surface (or at least 2 inches thick at a depth of less than or equal to 15cm (6 inches) of the mineral or muck soil surface,\r\n b. Occurs for at least 7 continuous days and 28 cumulative days, and\r\n c. Occurs during a normal or drier season and month (within 16 to 84 percent of probable precipitation).","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":25,"ChoiceValue":40,"ChoiceName":"f19","ChoiceLabel":"F19 Piedmont Flood Plain Soils","ChoiceObsolete":0,"ChoiceDescription":"On flood plains, a mineral layer at least 15 cm (6 inches) thick, starting at a depth of less than or equal to 25 cm (10 inches) from the soil surface, with a matrix (60 percent or more of the volume) chroma of less than 4 and 20 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":27,"ChoiceValue":41,"ChoiceName":"f20","ChoiceLabel":"F20 Anomalous Bright Loamy Soils","ChoiceObsolete":0,"ChoiceDescription":"Within 200 meters (656 feet) of estuarine marshes or water and within 1 m (3.28 feet) of mean high water, a mineral layer at least 10 cm (4 inches) thick, starting at a depth of less than or equal to 20 cm (8 inches) from the soil surface, with a matrix (60 percent or more of the volume) chroma of less than 5 and 10 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings and/or depletions.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":28,"ChoiceValue":42,"ChoiceName":"f21","ChoiceLabel":"F21 Red Parent Material","ChoiceObsolete":0,"ChoiceDescription":"A layer derived from red parent material (see glossary) that is at least 10 cm (4 inches) thick, starting at a depth of less than or equal to 25 cm (10 inches) from the soil surface with a hue of 7.5YR or redder. The matrix has a value and chroma greater than 2 and less than or equal to 4. The layer must contain 10 percent or more depletions and/or distinct or prominent redox concentrations occurring as soft masses or pore linings. Redox depletions should differ in color by having: a.) Value one or more higher and chroma one or more lower than the matrix, or b.) Value of 4 or more and chroma of 2 or less.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":43,"ChoiceValue":43,"ChoiceName":"f22","ChoiceLabel":"F22 Very Shallow Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"In depressions and flood plains subject to frequent ponding and/or flooding, one of the following:\r\na. if bedrock occurs between 15 cm (6 inches) and 25 cm (10 inches), a layer at least 15 cm (6 inches) thick starting at a depth of less than or equal to 10 cm (4 inches) from the soil surface with value 2.5 or less and chroma 1 or less, and the remaining soil to bedrock must have the same colors as above or any other color that has a chroma 2 or less. \r\nb. if bedrock occurs within 15 cm (6 inches), more than half of the soil thickness must have value 2.5 or less and chroma 1 or less, and the remaining soil to bedrock must have the same colors as above or any other color that has a chroma 2 or less.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":44,"ChoiceValue":44,"ChoiceName":"s11","ChoiceLabel":"S11 High Chroma Sands","ChoiceObsolete":0,"ChoiceDescription":"In coastal zones and dune-and-swale complexes, a layer 2 inches (5 cm) or more thick starting at a depth of less than or equal to 4 inches (10 cm) from the soil surface with chroma 4 or less and 2% or more distinct or prominent redox concentrations.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":45,"ChoiceValue":45,"ChoiceName":"s12","ChoiceLabel":"S12 Barrier Islands","ChoiceObsolete":0,"ChoiceDescription":"In the swale prtion of dune-and-swale complexes of barrier islands, a layer of muck 1 cm (0.5 inches) or more thick with value of 3 or less and chroma of 2 or less and starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"hydricsoilfieldindicator","ColumnLogicalName":"hydric_soil_field_indicator"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"a1","ChoiceLabel":"A1 Histosol or Histel","ChoiceObsolete":0,"ChoiceDescription":"Classifies as a Histosol (except Folist) or as a Histel (except Folistel).","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":9,"ChoiceValue":2,"ChoiceName":"a2","ChoiceLabel":"A2 Histic Epipedon","ChoiceObsolete":0,"ChoiceDescription":"A histic epipedon underlain by mineral soil material with chroma of 2 or less.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":10,"ChoiceValue":3,"ChoiceName":"a3","ChoiceLabel":"A3 Black Histic","ChoiceObsolete":0,"ChoiceDescription":"A layer of peat, mucky peat, or muck 20 cm (8 inches) or more thick that starts at a depth of less than or equal to 15 cm (6 inches) from the soil surface; has hue of 10YR or yellower, value of 3 or less, and chroma of 1 or less; and is underlain by mineral soil material with chroma of 2 or less.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":11,"ChoiceValue":4,"ChoiceName":"a4","ChoiceLabel":"A4 Hydrogen Sulfide","ChoiceObsolete":0,"ChoiceDescription":"A hydrogen sulfide odor at a depth of less than or equal to 30 cm (12 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":12,"ChoiceValue":5,"ChoiceName":"a5","ChoiceLabel":"A5 Stratified Layers","ChoiceObsolete":0,"ChoiceDescription":"Several stratified layers startingat a depth of less than or equal to 15 cm (6 inches) from the soil surface. At least one of the layers has value of 3 or less and chroma of 1 or less, or it is muck, mucky peat, peat, or a mucky modified mineral texture. The remaining layers have chroma of 2 or less. For any sandy material that constitutes the layer with value of 3 or less and chroma of 1 or less, at least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":13,"ChoiceValue":6,"ChoiceName":"a6","ChoiceLabel":"A6 Organic Bodies","ChoiceObsolete":0,"ChoiceDescription":"Presence of 2 percent or more organic bodies of muck or a mucky modified mineral texture starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":14,"ChoiceValue":7,"ChoiceName":"a7","ChoiceLabel":"A7 5 cm Mucky Mineral","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky modified mineral soil material 5 cm (2 inches) or more thick, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":15,"ChoiceValue":8,"ChoiceName":"a8","ChoiceLabel":"A8 Muck Presence","ChoiceObsolete":0,"ChoiceDescription":"A layer of muck with value of 3 or less and chroma of 1 or less, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":16,"ChoiceValue":9,"ChoiceName":"a9","ChoiceLabel":"A9 1 cm Muck","ChoiceObsolete":0,"ChoiceDescription":"A layer of muck 1 cm (0.5 inch) or more thick with value of 3 or less and chroma of 1 or less and starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":2,"ChoiceValue":10,"ChoiceName":"a10","ChoiceLabel":"A10 2 cm Muck","ChoiceObsolete":0,"ChoiceDescription":"A layer of muck 2 cm (0.75 inch) or more thick with value of 3 or less and chroma of 1 or less, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":3,"ChoiceValue":11,"ChoiceName":"a11","ChoiceLabel":"A11 Depleted Below Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer with a depleted or gleyed matrix that has 60 percent or more chroma of 2 or less, starting at a depth of less than or equal to 30 cm (12 inches) from the soil surface, and having a minimum thickness of either:\r\n a. 15 cm (6 inches), or \r\n b. 5 cm (2 inches) if the 5 cm consists of fragmental soil material.\r\n\r\nOrganic, loamy or clayey layer(s) above the depleted or gleyed matrix must have value of 3 or less and chroma of 2 or less starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface and extend to the depleted or gleyed matrix. Any sandy material above the depleted or gleyed matrix must have value of 3 or less and chroma of 1 or less starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface and extend to the depleted or gleyed matrix. Viewed through a10x or 15x hand lens, at least 70 percent of the visible soil particles must be masked with organic material. Observed without a hand lens, the particles appear to be close to 100 percent masked.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":4,"ChoiceValue":12,"ChoiceName":"a12","ChoiceLabel":"A12 Thick Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer at least 15 cm (6 inches) thick with a depleted or gleyed matrix that has 60 percent or more chroma of 2 or less starting below 30 cm (12 inches) of the surface. The layer(s) above the depleted or gleyed matrix and starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface must have value of 2.5 or less and chroma of 1 or less to a depth of at least 30 cm (12 inches) and value of 3 or less and chroma of 1 or less in any remaining layers above the depleted or gleyed matrix. \r\nIn any sandy material above the depleted or gleyed matrix, at least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":5,"ChoiceValue":13,"ChoiceName":"a13","ChoiceLabel":"A13 Alaska Gleyed","ChoiceObsolete":0,"ChoiceDescription":"A mineral layer with a dominant hue of N, 10Y, 5GY, 10GY, 5G, 10G, 5BG, 10BG, 5B, 10B, or 5PB and with value of 4 or more in more than 50 percent of the matrix. The layer starts at a depth of less than or equal to 30 cm (12 inches) from the mineral surface and is underlain at a depth of less than or equal to 1.5 m (60 inches) from the soil surface by soil material with hue of 5Y or redder in the same type of parent material.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":6,"ChoiceValue":14,"ChoiceName":"a14","ChoiceLabel":"A14 Alaska Redox","ChoiceObsolete":0,"ChoiceDescription":"A mineral layer that has dominant hue of 5Y with chroma of 3 or less, or a gleyed matrix, with 10 percent or more distinct or prominent redox concentrations occurring as pore linings with value and chroma of 4 or more. The layer occurs at a depth of less than or equal to 30 cm (12 inches) from the soil surface.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":7,"ChoiceValue":15,"ChoiceName":"a15","ChoiceLabel":"A15 Alaska Gleyed Pores","ChoiceObsolete":0,"ChoiceDescription":"A mineral layer that has 10 percent or more hue of N, 10Y, 5GY, 10GY, 5G, 10G, 5BG, 10BG, 5B, 10B, or 5PB with value of 4 or more along root channels or other pores and that starts at a depth of less than or equal to 30 cm (12 inches) from the soil surface. The matrix has a dominant hue of 5Y or redder.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":8,"ChoiceValue":16,"ChoiceName":"a16","ChoiceLabel":"A16 Coast Prairie Redox","ChoiceObsolete":0,"ChoiceDescription":"A layer starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface that is at least 10 cm (4 inches) thick and has a matrix chroma of 3 or less with 2 percent or more distinct or prominent redox concentrations occurring as soft masses and/or pore linings.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":34,"ChoiceValue":17,"ChoiceName":"s1","ChoiceLabel":"S1 Sandy Mucky Mineral","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky modified sandy soil material 5 cm (2 inches) or more thick starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":35,"ChoiceValue":18,"ChoiceName":"s2","ChoiceLabel":"S2 2.5 cm Mucky Peat or Peat","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky peat or peat 2.5 cm (1 inch) or more thick with value of 4 or less and chroma of 3 or less, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface, and underlain by sandy soil material.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":36,"ChoiceValue":19,"ChoiceName":"s3","ChoiceLabel":"S3 5 cm Mucky Peat or Peat","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky peat or peat 5 cm (2 inches) or more thick with value of 3 or less and chroma of 2 or less, starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface, and underlain by sandy soil material.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":37,"ChoiceValue":20,"ChoiceName":"s4","ChoiceLabel":"S4 Sandy Gleyed Matrix","ChoiceObsolete":0,"ChoiceDescription":"A gleyed matrix that occupies 60 percent or more of a layer starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":38,"ChoiceValue":21,"ChoiceName":"s5","ChoiceLabel":"S5 Sandy Redox","ChoiceObsolete":0,"ChoiceDescription":"A layer starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface that is at least 10 cm (4 inches) thick and has a matrix with 60 percent or more chroma of 2 or less and 2 percent or more distinct or prominent redox concentrations occurring as soft masses and/or pore linings.\r\n","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":39,"ChoiceValue":22,"ChoiceName":"s6","ChoiceLabel":"S6 Stripped Matrix","ChoiceObsolete":0,"ChoiceDescription":"A layer starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface in which iron-manganese oxides and/or organic matter have been stripped from the matrix and the primary base color of the soil material has been exposed. The stripped areas and translocated oxides and/or organic matter form a faintly contrasting pattern of two or more colors with diffuse boundaries. The stripped zones are 10 percent or more of the volume and are rounded.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":40,"ChoiceValue":23,"ChoiceName":"s7","ChoiceLabel":"S7 Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer 10 cm (4 inches) thick, starting at a depth of less than or equal to the upper 15 cm (6 inches) from the soil surface, with a matrix value 3 of or less and chroma of 1 or less. At least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked. The matrix color of the layer directly below the dark layer must have the same colors as those described above or any color that has chroma of 2 or less.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":41,"ChoiceValue":24,"ChoiceName":"s8","ChoiceLabel":"S8 Polyvalue Below Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer with value of 3 or less and chroma of 1 or less starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface. At least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked. Directly below this layer, 5 percent or more of the soil volume has value of 3 or less and chroma of 1 or less, and the remainder of the soil volume has value of 4 or more and chroma of 1 or less to a depth of 30 cm (12 inches) or to the spodic horizon, whichever is less.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":42,"ChoiceValue":25,"ChoiceName":"s9","ChoiceLabel":"S9 Thin Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer 5 cm (2 inches) or more thick, at a depth of less than or equal to 15 cm (6 inches) from the soil surface, with value of 3 or less and chroma of 1 or less. At least 70 percent of the visible soil particles must be masked with organic material, viewed through a 10x or 15x hand lens. Observed without a hand lens, the particles appear to be close to 100 percent masked. This layer is underlain by a layer or layers with value of 4 or less and chroma of 1 or less to a depth of 30 cm (12 inches) or to the spodic horizon, whichever is less.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":17,"ChoiceValue":26,"ChoiceName":"f1","ChoiceLabel":"F1 Loamy Mucky Mineral","ChoiceObsolete":0,"ChoiceDescription":"A layer of mucky modified loamy or clayey soil material 10 cm (4 inches) or more thick starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":26,"ChoiceValue":27,"ChoiceName":"f2","ChoiceLabel":"F2 Loamy Gleyed Matrix","ChoiceObsolete":0,"ChoiceDescription":"A gleyed matrix that occupies 60 percent or more of a layer starting at a depth of less than or equal to 30 cm (12 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":29,"ChoiceValue":28,"ChoiceName":"f3","ChoiceLabel":"F3 Depleted Matrix","ChoiceObsolete":0,"ChoiceDescription":"A layer that has a depleted matrix with 60 percent or more chroma of 2 or less and that has a minimum thickness of either:\r\n a. 5 cm (2 inches) if the 5 cm is entirely at a depth of less than or equal to 15 cm (6 inches) from the soil surface, or \r\n b. 15 cm (6 inches), at a depth of less than or equal to 25 cm (10 inches) from the soil surface surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":30,"ChoiceValue":29,"ChoiceName":"f6","ChoiceLabel":"F6 Redox Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"A layer that is at least 10 cm (4 inches) thick, is at a depth of less than or equal to 20 cm (8 inches) of the mineral soil surface, and has:\r\n a. Matrix value of 3 or less and chroma of 1 or less and 2 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings, or\r\n b. Matrix value of 3 or less and chroma of 2 or less and 5 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":31,"ChoiceValue":30,"ChoiceName":"f7","ChoiceLabel":"F7 Depleted Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"Redox depletions with value of 5 or more and chroma of 2 or less in a layer that is at least 10 cm (4 inches) thick, is at a depth of less than or equal to 20 cm (8 inches) from the mineral soil surface, and has:\r\n a. Matrix value of 3 or less and chroma of 1 or less and 10 percent or more redox depletions, or\r\n b. Matrix value of 3 or less and chroma of 2 or less and 20 percent or more redox depletions.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":32,"ChoiceValue":31,"ChoiceName":"f8","ChoiceLabel":"F8 Redox Depressions","ChoiceObsolete":0,"ChoiceDescription":"In closed depressions subject to ponding, 5 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings in a layer that is 5 cm (2 inches) or more thick and is at a depth of less than or equal to 10 cm (4 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":33,"ChoiceValue":32,"ChoiceName":"f9","ChoiceLabel":"F9 Vernal Pools","ChoiceObsolete":1,"ChoiceDescription":"In closed depressions that are subject to ponding, presence of a depleted matrix with 60 percent or more chroma of 2 or less in a layer 5 cm (2 inches) thick entirely within the upper 15 cm (6 inches) of the soil.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":18,"ChoiceValue":33,"ChoiceName":"f10","ChoiceLabel":"F10 Marl","ChoiceObsolete":0,"ChoiceDescription":"A layer of marl with value of 5 or more and chroma less than 2 starting at a depth of less than or equal to 10 cm (4 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":19,"ChoiceValue":34,"ChoiceName":"f11","ChoiceLabel":"F11 Depleted Ochric","ChoiceObsolete":0,"ChoiceDescription":"A layer(s) 10 cm (4 inches) or more thick in which 60 percent or more of the matrix has value of 4 or more and chroma of 1 or less. The layer is at a depth of less than or equal to 25 cm (10 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":20,"ChoiceValue":35,"ChoiceName":"f12","ChoiceLabel":"F12 Iron-Manganese Masses","ChoiceObsolete":0,"ChoiceDescription":"On flood plains, a layer 10 cm (4 inches) or more thick with 40 percent or more chroma of 2 or less and 2 percent or more distinct or prominent redox concentrations occurring as soft iron-manganese masses with diffuse boundaries. The layer occurs at a depth of less than or equal to 20 cm (8 inches) from the soil surface. Iron-manganese masses have value and chroma of 3 or less. Most commonly, they are black. The thickness requirement is waived if the layer is the mineral surface layer","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":21,"ChoiceValue":36,"ChoiceName":"f13","ChoiceLabel":"F13 Umbric Surface","ChoiceObsolete":0,"ChoiceDescription":"In depressions and other concave landforms, a layer 25 cm (10 inches) or more thick, starting at a depth of less than or equal to 15 cm (6 inches) fromthe soil surface, in which the upper 15 cm (6 inches) has value of 3 or less and chroma of 1 or less and in which the lower 10 cm (4 inches) has the same colors as those described above or any other color that has chroma of 2 or less.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":22,"ChoiceValue":37,"ChoiceName":"f16","ChoiceLabel":"F16 High Plains Depressions","ChoiceObsolete":0,"ChoiceDescription":"In closed depressions that are subject to ponding, a mineral soil that has chroma of 1 or less to a depth of at least 35 cm (13.5 inches) and a layer at least 10 cm (4 inches) thick starting at a depth of less than or equal to 35 cm (13.5 inches) from the mineral soil that has either:\r\n a. 1 percent or more redox concentrations occurring as nodules or concretions, or\r\n b. Redox concentrations occurring as nodules or concretions with distinct or prominent corona.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":23,"ChoiceValue":38,"ChoiceName":"f17","ChoiceLabel":"F17 Delta Ochric","ChoiceObsolete":0,"ChoiceDescription":"A layer 10 cm (4 inches) or more thick in which 60 percent or more of the matrix has value of 4 or more and chroma of 2 or less and there are no redox concentrations. This layer occurs at a depth of less than or equal to 20 cm (8 inches) of the soil.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":24,"ChoiceValue":39,"ChoiceName":"f18","ChoiceLabel":"F18 Reduced Vertic","ChoiceObsolete":0,"ChoiceDescription":"In Vertisols and Vertic intergrades, a positive reaction to alpha-alpha-dipyridyl that:\r\n a. Is the dominant (60 percent or more) condition of a layer at least 4 inches thick at a depth of less than or equal to (30 cm) 12 inches from the soil surface (or at least 2 inches thick at a depth of less than or equal to 15cm (6 inches) of the mineral or muck soil surface,\r\n b. Occurs for at least 7 continuous days and 28 cumulative days, and\r\n c. Occurs during a normal or drier season and month (within 16 to 84 percent of probable precipitation).","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":25,"ChoiceValue":40,"ChoiceName":"f19","ChoiceLabel":"F19 Piedmont Flood Plain Soils","ChoiceObsolete":0,"ChoiceDescription":"On flood plains, a mineral layer at least 15 cm (6 inches) thick, starting at a depth of less than or equal to 25 cm (10 inches) from the soil surface, with a matrix (60 percent or more of the volume) chroma of less than 4 and 20 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":27,"ChoiceValue":41,"ChoiceName":"f20","ChoiceLabel":"F20 Anomalous Bright Loamy Soils","ChoiceObsolete":0,"ChoiceDescription":"Within 200 meters (656 feet) of estuarine marshes or water and within 1 m (3.28 feet) of mean high water, a mineral layer at least 10 cm (4 inches) thick, starting at a depth of less than or equal to 20 cm (8 inches) from the soil surface, with a matrix (60 percent or more of the volume) chroma of less than 5 and 10 percent or more distinct or prominent redox concentrations occurring as soft masses or pore linings and/or depletions.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":28,"ChoiceValue":42,"ChoiceName":"f21","ChoiceLabel":"F21 Red Parent Material","ChoiceObsolete":0,"ChoiceDescription":"A layer derived from red parent material (see glossary) that is at least 10 cm (4 inches) thick, starting at a depth of less than or equal to 25 cm (10 inches) from the soil surface with a hue of 7.5YR or redder. The matrix has a value and chroma greater than 2 and less than or equal to 4. The layer must contain 10 percent or more depletions and/or distinct or prominent redox concentrations occurring as soft masses or pore linings. Redox depletions should differ in color by having: a.) Value one or more higher and chroma one or more lower than the matrix, or b.) Value of 4 or more and chroma of 2 or less.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":43,"ChoiceValue":43,"ChoiceName":"f22","ChoiceLabel":"F22 Very Shallow Dark Surface","ChoiceObsolete":0,"ChoiceDescription":"In depressions and flood plains subject to frequent ponding and/or flooding, one of the following:\r\na. if bedrock occurs between 15 cm (6 inches) and 25 cm (10 inches), a layer at least 15 cm (6 inches) thick starting at a depth of less than or equal to 10 cm (4 inches) from the soil surface with value 2.5 or less and chroma 1 or less, and the remaining soil to bedrock must have the same colors as above or any other color that has a chroma 2 or less. \r\nb. if bedrock occurs within 15 cm (6 inches), more than half of the soil thickness must have value 2.5 or less and chroma 1 or less, and the remaining soil to bedrock must have the same colors as above or any other color that has a chroma 2 or less.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":44,"ChoiceValue":44,"ChoiceName":"s11","ChoiceLabel":"S11 High Chroma Sands","ChoiceObsolete":0,"ChoiceDescription":"In coastal zones and dune-and-swale complexes, a layer 2 inches (5 cm) or more thick starting at a depth of less than or equal to 4 inches (10 cm) from the soil surface with chroma 4 or less and 2% or more distinct or prominent redox concentrations.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4920,"DomainName":"hydric_soil_indicator","DomainRanked":0,"DisplayLabel":1,"ChoiceSequence":45,"ChoiceValue":45,"ChoiceName":"s12","ChoiceLabel":"S12 Barrier Islands","ChoiceObsolete":0,"ChoiceDescription":"In the swale prtion of dune-and-swale complexes of barrier islands, a layer of muck 1 cm (0.5 inches) or more thick with value of 3 or less and chroma of 2 or less and starting at a depth of less than or equal to 15 cm (6 inches) from the soil surface.","ColumnPhysicalName":"osdhydricsoilfieldindicator","ColumnLogicalName":"osd_hydric_soil_field_indicatr"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"class 1","ChoiceLabel":"Class 1","ChoiceObsolete":0,"ChoiceDescription":"Interconnected persistent plant cover or dense bunchgrasses and surrounding round interpatch areas <30cm.","ColumnPhysicalName":"osdresourceretentionclass","ColumnLogicalName":"osd_resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"class 2","ChoiceLabel":"Class 2","ChoiceObsolete":0,"ChoiceDescription":"Persistent plants interconnected and surrounding round/oval interpatch areas >30 cm.","ColumnPhysicalName":"osdresourceretentionclass","ColumnLogicalName":"osd_resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"class 3","ChoiceLabel":"Class 3","ChoiceObsolete":0,"ChoiceDescription":"Persistent plant patches fragmented by elongated interpatch areas that are bounded in the plot.","ColumnPhysicalName":"osdresourceretentionclass","ColumnLogicalName":"osd_resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"class 4","ChoiceLabel":"Class 4","ChoiceObsolete":0,"ChoiceDescription":"Persistent plant patches fragmented by elongated interpatch areas that cross through the plot.","ColumnPhysicalName":"osdresourceretentionclass","ColumnLogicalName":"osd_resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"class 5","ChoiceLabel":"Class 5","ChoiceObsolete":0,"ChoiceDescription":"Interpatch areas interconnected and crossing the plot in several directions; isolated persistent plant patches.","ColumnPhysicalName":"osdresourceretentionclass","ColumnLogicalName":"osd_resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"class 6","ChoiceLabel":"Class 6","ChoiceObsolete":0,"ChoiceDescription":"Interpatch areas interconnected; scattered or no persistent plants.","ColumnPhysicalName":"osdresourceretentionclass","ColumnLogicalName":"osd_resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"class 1","ChoiceLabel":"Class 1","ChoiceObsolete":0,"ChoiceDescription":"Interconnected persistent plant cover or dense bunchgrasses and surrounding round interpatch areas <30cm.","ColumnPhysicalName":"resourceretentionclass","ColumnLogicalName":"resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"class 2","ChoiceLabel":"Class 2","ChoiceObsolete":0,"ChoiceDescription":"Persistent plants interconnected and surrounding round/oval interpatch areas >30 cm.","ColumnPhysicalName":"resourceretentionclass","ColumnLogicalName":"resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"class 3","ChoiceLabel":"Class 3","ChoiceObsolete":0,"ChoiceDescription":"Persistent plant patches fragmented by elongated interpatch areas that are bounded in the plot.","ColumnPhysicalName":"resourceretentionclass","ColumnLogicalName":"resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"class 4","ChoiceLabel":"Class 4","ChoiceObsolete":0,"ChoiceDescription":"Persistent plant patches fragmented by elongated interpatch areas that cross through the plot.","ColumnPhysicalName":"resourceretentionclass","ColumnLogicalName":"resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"class 5","ChoiceLabel":"Class 5","ChoiceObsolete":0,"ChoiceDescription":"Interpatch areas interconnected and crossing the plot in several directions; isolated persistent plant patches.","ColumnPhysicalName":"resourceretentionclass","ColumnLogicalName":"resource_retention_class"} {"DomainID":4922,"DomainName":"resource_retention_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"class 6","ChoiceLabel":"Class 6","ChoiceObsolete":0,"ChoiceDescription":"Interpatch areas interconnected; scattered or no persistent plants.","ColumnPhysicalName":"resourceretentionclass","ColumnLogicalName":"resource_retention_class"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"algae","ChoiceLabel":"Algae","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypedom","ColumnLogicalName":"biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"cyanobacteria","ChoiceLabel":"Cyanobacteria","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypedom","ColumnLogicalName":"biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"lichen","ChoiceLabel":"Lichen","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypedom","ColumnLogicalName":"biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"liverworts","ChoiceLabel":"Liverworts","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypedom","ColumnLogicalName":"biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"moss","ChoiceLabel":"Moss","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypedom","ColumnLogicalName":"biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"none evident","ChoiceLabel":"None evident","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypedom","ColumnLogicalName":"biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"algae","ChoiceLabel":"Algae","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypesecond","ColumnLogicalName":"biological_crust_type_second"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"cyanobacteria","ChoiceLabel":"Cyanobacteria","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypesecond","ColumnLogicalName":"biological_crust_type_second"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"lichen","ChoiceLabel":"Lichen","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypesecond","ColumnLogicalName":"biological_crust_type_second"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"liverworts","ChoiceLabel":"Liverworts","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypesecond","ColumnLogicalName":"biological_crust_type_second"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"moss","ChoiceLabel":"Moss","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypesecond","ColumnLogicalName":"biological_crust_type_second"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"none evident","ChoiceLabel":"None evident","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"biolcrusttypesecond","ColumnLogicalName":"biological_crust_type_second"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"algae","ChoiceLabel":"Algae","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypedom","ColumnLogicalName":"osd_biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"cyanobacteria","ChoiceLabel":"Cyanobacteria","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypedom","ColumnLogicalName":"osd_biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"lichen","ChoiceLabel":"Lichen","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypedom","ColumnLogicalName":"osd_biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"liverworts","ChoiceLabel":"Liverworts","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypedom","ColumnLogicalName":"osd_biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"moss","ChoiceLabel":"Moss","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypedom","ColumnLogicalName":"osd_biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"none evident","ChoiceLabel":"None evident","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypedom","ColumnLogicalName":"osd_biological_crust_type_dom"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"algae","ChoiceLabel":"Algae","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypesecond","ColumnLogicalName":"osd_biological_crust_type_sec"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"cyanobacteria","ChoiceLabel":"Cyanobacteria","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypesecond","ColumnLogicalName":"osd_biological_crust_type_sec"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"lichen","ChoiceLabel":"Lichen","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypesecond","ColumnLogicalName":"osd_biological_crust_type_sec"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"liverworts","ChoiceLabel":"Liverworts","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypesecond","ColumnLogicalName":"osd_biological_crust_type_sec"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"moss","ChoiceLabel":"Moss","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypesecond","ColumnLogicalName":"osd_biological_crust_type_sec"} {"DomainID":4923,"DomainName":"biological_crust_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"none evident","ChoiceLabel":"None evident","ChoiceObsolete":0,"ChoiceDescription":"Reference: Field Guide to Classify Biological Soil Crusts for Ecological Site Evaluation. N. Pietrasiak, PhD.","ColumnPhysicalName":"osdbiolcrusttypesecond","ColumnLogicalName":"osd_biological_crust_type_sec"} {"DomainID":4924,"DomainName":"soil_redistribution_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"class 0","ChoiceLabel":"Class 0","ChoiceObsolete":0,"ChoiceDescription":"No evidence of erosion or deposition.","ColumnPhysicalName":"osdsoilredistributionclass","ColumnLogicalName":"osd_soil_redistribution_class"} {"DomainID":4924,"DomainName":"soil_redistribution_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"class 1","ChoiceLabel":"Class 1","ChoiceObsolete":0,"ChoiceDescription":"Very slight soil redistribution. No noticeable thinning of the soil surface and soil movement occurs within a matrix of vegetated/stable soil. ","ColumnPhysicalName":"osdsoilredistributionclass","ColumnLogicalName":"osd_soil_redistribution_class"} {"DomainID":4924,"DomainName":"soil_redistribution_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"class 2","ChoiceLabel":"Class 2","ChoiceObsolete":0,"ChoiceDescription":"Patchy, slight (<5cm) soil loss and deposition. The soil surface is thinned in discrete patches within a matrix of vegetated/stable soil. Sediment source may be on or off the plot. ","ColumnPhysicalName":"osdsoilredistributionclass","ColumnLogicalName":"osd_soil_redistribution_class"} {"DomainID":4924,"DomainName":"soil_redistribution_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"class 3a","ChoiceLabel":"Class 3a","ChoiceObsolete":0,"ChoiceDescription":"Extensive, moderate soil loss (<10cm). Noticeable thinning of the soil surface across the plot, with or without patches of stable soil or sediment accumulation. 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","ColumnPhysicalName":"osdsoilredistributionclass","ColumnLogicalName":"osd_soil_redistribution_class"} {"DomainID":4924,"DomainName":"soil_redistribution_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"class 4a","ChoiceLabel":"Class 4a","ChoiceObsolete":0,"ChoiceDescription":"Extensive, severe erosion (>10cm); little deposition. Plot is embedded in an extensive area of erosion.","ColumnPhysicalName":"osdsoilredistributionclass","ColumnLogicalName":"osd_soil_redistribution_class"} {"DomainID":4924,"DomainName":"soil_redistribution_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"class 4b","ChoiceLabel":"Class 4b","ChoiceObsolete":0,"ChoiceDescription":"Extensive, severe erosion (>10cm) coupled with patchy sediment deposition. Plot is embedded in an extensive area of erosion and deposition. ","ColumnPhysicalName":"osdsoilredistributionclass","ColumnLogicalName":"osd_soil_redistribution_class"} {"DomainID":4924,"DomainName":"soil_redistribution_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"class 4c","ChoiceLabel":"Class 4c","ChoiceObsolete":0,"ChoiceDescription":"Extensive, severe sediment deposition (>10cm). Sedimentation continuous across plot. May be hard to detect without excavation. Sediments originate from off the plot. ","ColumnPhysicalName":"osdsoilredistributionclass","ColumnLogicalName":"osd_soil_redistribution_class"} {"DomainID":4924,"DomainName":"soil_redistribution_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"class 0","ChoiceLabel":"Class 0","ChoiceObsolete":0,"ChoiceDescription":"No evidence of erosion or deposition.","ColumnPhysicalName":"soilredistributionclass","ColumnLogicalName":"soil_redistribution_class"} {"DomainID":4924,"DomainName":"soil_redistribution_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"class 1","ChoiceLabel":"Class 1","ChoiceObsolete":0,"ChoiceDescription":"Very slight soil redistribution. No noticeable thinning of the soil surface and soil movement occurs within a matrix of vegetated/stable soil. 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{"DomainID":4957,"DomainName":"soil_moisture_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":26,"ChoiceValue":26,"ChoiceName":"global water data logger wl15x-015","ChoiceLabel":"Global Water Data Logger WL15X-015","ChoiceObsolete":0,"ChoiceDescription":"By Global Water.\r\n\r\nUsed in MLRA SSO 3-RHI.","ColumnPhysicalName":"soilmoistsensorkind","ColumnLogicalName":"soil_moisture_sensor_kind"} {"DomainID":4958,"DomainName":"soil_odor_intensity","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"slight","ChoiceLabel":"Slight","ChoiceObsolete":0,"ChoiceDescription":"Odor is faint (e.g., only detected when some of the sample is brought close to the nose).","ColumnPhysicalName":"osdsoilodorintensity","ColumnLogicalName":"osd_soil_odor_intensity"} {"DomainID":4958,"DomainName":"soil_odor_intensity","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Odor is readily noticeable at arms length as one handles the material (e.g., intermediate intensity); only detected as one starts to dig into the sample.","ColumnPhysicalName":"osdsoilodorintensity","ColumnLogicalName":"osd_soil_odor_intensity"} {"DomainID":4958,"DomainName":"soil_odor_intensity","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"strong","ChoiceLabel":"Strong","ChoiceObsolete":0,"ChoiceDescription":"Odor is quite intense and readily detected before or immediately after the sample is exposed to air.","ColumnPhysicalName":"osdsoilodorintensity","ColumnLogicalName":"osd_soil_odor_intensity"} {"DomainID":4958,"DomainName":"soil_odor_intensity","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"slight","ChoiceLabel":"Slight","ChoiceObsolete":0,"ChoiceDescription":"Odor is faint (e.g., only detected when some of the sample is brought close to the nose).","ColumnPhysicalName":"soilodorintensity","ColumnLogicalName":"soil_odor_intensity"} {"DomainID":4958,"DomainName":"soil_odor_intensity","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Odor is readily noticeable at arms length as one handles the material (e.g., intermediate intensity); only detected as one starts to dig into the sample.","ColumnPhysicalName":"soilodorintensity","ColumnLogicalName":"soil_odor_intensity"} {"DomainID":4958,"DomainName":"soil_odor_intensity","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"strong","ChoiceLabel":"Strong","ChoiceObsolete":0,"ChoiceDescription":"Odor is quite intense and readily detected before or immediately after the sample is exposed to air.","ColumnPhysicalName":"soilodorintensity","ColumnLogicalName":"soil_odor_intensity"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":1,"ChoiceName":"cs109","ChoiceLabel":"CS109","ChoiceObsolete":0,"ChoiceDescription":"CS109 by Campbell Scientific Inc.","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"cs107","ChoiceLabel":"CS107","ChoiceObsolete":0,"ChoiceDescription":"CS107 by Campbell Scientific 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{"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":5,"ChoiceName":"mrc probe","ChoiceLabel":"MRC Probe","ChoiceObsolete":0,"ChoiceDescription":"MRC Probe by Measurement Research Corporation","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":6,"ChoiceName":"s-tmb-m006","ChoiceLabel":"S-TMB-M006","ChoiceObsolete":0,"ChoiceDescription":"S-TMB-M006 by Onset.","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":7,"ChoiceName":"watermark","ChoiceLabel":"Watermark","ChoiceObsolete":0,"ChoiceDescription":"Watermark by Soil Moisture 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{"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":13,"ChoiceName":"tt-103r-w","ChoiceLabel":"TT-103R-W","ChoiceObsolete":1,"ChoiceDescription":"TT-103R-W by Texas Electronics.","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"sto1","ChoiceLabel":"ST01","ChoiceObsolete":1,"ChoiceDescription":"ST01 by Hukselux","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"ts10","ChoiceLabel":"TS10","ChoiceObsolete":0,"ChoiceDescription":"TS10 by Environ Data","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":16,"ChoiceName":"t300","ChoiceLabel":"T300","ChoiceObsolete":1,"ChoiceDescription":"T300 by Aquaterrinstrument","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":17,"ChoiceName":"decagon rt-1","ChoiceLabel":"Decagon RT-1","ChoiceObsolete":0,"ChoiceDescription":"By Decagon Devices","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":18,"ChoiceName":"hobo u23 pro v2","ChoiceLabel":"Hobo U23 Pro V2","ChoiceObsolete":0,"ChoiceDescription":"Hobo by Onset","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":19,"ChoiceName":"decagon 5tm","ChoiceLabel":"Decagon 5TM","ChoiceObsolete":0,"ChoiceDescription":"By Decagon Devices","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":20,"ChoiceName":"hobo pendant ua-001","ChoiceLabel":"Hobo Pendant UA-001","ChoiceObsolete":0,"ChoiceDescription":"Hobo by Onset","ColumnPhysicalName":"soiltempsensorkind","ColumnLogicalName":"soil_temp_sensor_kind"} {"DomainID":4959,"DomainName":"soil_temperature_sensor_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":22,"ChoiceName":"hobo pendant ua-000-08","ChoiceLabel":"Hobo Pendant UA-000-08","ChoiceObsolete":0,"ChoiceDescription":"Hobo pendant soil temperature probe. \r\n\r\nUsed in MLRA SSO 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{"DomainID":4961,"DomainName":"fragment_estimate_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":1,"ChoiceName":"visual inspection","ChoiceLabel":"Visual inspection","ChoiceObsolete":0,"ChoiceDescription":"Horizon fragment volume was determined using visual inspection.","ColumnPhysicalName":"fragestmethod","ColumnLogicalName":"fragment_estimate_method"} {"DomainID":4961,"DomainName":"fragment_estimate_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":2,"ChoiceName":"weighed","ChoiceLabel":"Weighed","ChoiceObsolete":0,"ChoiceDescription":"Horizon fragment percent by weight was determined by weighing","ColumnPhysicalName":"fragestmethod","ColumnLogicalName":"fragment_estimate_method"} {"DomainID":4961,"DomainName":"fragment_estimate_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":3,"ChoiceName":"displacement","ChoiceLabel":"Displacement","ChoiceObsolete":0,"ChoiceDescription":"Horizon fragment volume was 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{"DomainID":4961,"DomainName":"fragment_estimate_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":1,"ChoiceName":"visual inspection","ChoiceLabel":"Visual inspection","ChoiceObsolete":0,"ChoiceDescription":"Horizon fragment volume was determined using visual inspection.","ColumnPhysicalName":"osdfragestmethod","ColumnLogicalName":"osd_fragment_estimate_method"} {"DomainID":4961,"DomainName":"fragment_estimate_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":2,"ChoiceName":"weighed","ChoiceLabel":"Weighed","ChoiceObsolete":0,"ChoiceDescription":"Horizon fragment percent by weight was determined by weighing","ColumnPhysicalName":"osdfragestmethod","ColumnLogicalName":"osd_fragment_estimate_method"} {"DomainID":4961,"DomainName":"fragment_estimate_method","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":3,"ChoiceName":"displacement","ChoiceLabel":"Displacement","ChoiceObsolete":0,"ChoiceDescription":"Horizon fragment 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For example, statements of prior survey and legend-wide join statements.","ColumnPhysicalName":"lmutextkind","ColumnLogicalName":"legend_mapunit_text_kind"} {"DomainID":4962,"DomainName":"legend_mapunit_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"correlation notes","ChoiceLabel":"Correlation notes","ChoiceObsolete":0,"ChoiceDescription":"Text entries related to correlation concerns that affect the entire legend.","ColumnPhysicalName":"lmutextkind","ColumnLogicalName":"legend_mapunit_text_kind"} {"DomainID":4962,"DomainName":"legend_mapunit_text_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"miscellaneous notes","ChoiceLabel":"Miscellaneous notes","ChoiceObsolete":0,"ChoiceDescription":"Text entries not relate to any of the other choices.","ColumnPhysicalName":"lmutextkind","ColumnLogicalName":"legend_mapunit_text_kind"} {"DomainID":4963,"DomainName":"outflow_chamber_conv_factor","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":1,"ChoiceName":"20","ChoiceLabel":"20","ChoiceObsolete":0,"ColumnPhysicalName":"outflowchamberconvfact","ColumnLogicalName":"outflow_chamber_conv_factor"} {"DomainID":4963,"DomainName":"outflow_chamber_conv_factor","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":2,"ChoiceName":"105","ChoiceLabel":"105","ChoiceObsolete":0,"ColumnPhysicalName":"outflowchamberconvfact","ColumnLogicalName":"outflow_chamber_conv_factor"} {"DomainID":4964,"DomainName":"texture_structure_category","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"0.01","ChoiceLabel":"0.01","ChoiceObsolete":0,"ChoiceDescription":"Compacted, structureless, clayey or silty materials such as landfill caps and liners, lacustrine or marine sediments.","ColumnPhysicalName":"texturestructurecat","ColumnLogicalName":"texture_structure_category"} {"DomainID":4964,"DomainName":"texture_structure_category","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"0.04","ChoiceLabel":"0.04","ChoiceObsolete":0,"ChoiceDescription":"Soils that are both fine textured (clayey or silty) and unstructured; may also include some fine sands.","ColumnPhysicalName":"texturestructurecat","ColumnLogicalName":"texture_structure_category"} {"DomainID":4964,"DomainName":"texture_structure_category","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"0.12","ChoiceLabel":"0.12","ChoiceObsolete":0,"ChoiceDescription":"Most structured soils from clays through loams; also includes unstructured medium and fine sands. The category most frequently applicable for agricultural soils.","ColumnPhysicalName":"texturestructurecat","ColumnLogicalName":"texture_structure_category"} {"DomainID":4964,"DomainName":"texture_structure_category","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"0.36","ChoiceLabel":"0.36","ChoiceObsolete":0,"ChoiceDescription":"Coarse and gravelly sands; may also include highly structured or aggregated soils, as well as soils with large and/or numerous cracks or macropores.","ColumnPhysicalName":"texturestructurecat","ColumnLogicalName":"texture_structure_category"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"badland","ChoiceLabel":"Badland","ChoiceObsolete":0,"ChoiceDescription":"Badland is moderately steep to very steep barren land that is dissected by many intermittent drainage channels. Ordinarily, the areas are not stony. Badland is most common in semiarid and arid regions where streams cut into soft geologic material. Local relief generally ranges from 10 and 200 meters in height. Potential runoff is very high, and erosion is active.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"beaches","ChoiceLabel":"Beaches","ChoiceObsolete":0,"ChoiceDescription":"Beaches are sandy, gravelly, or cobbly shores that are washed and rewashed by waves. The areas may be partly covered with water during high tides or storms.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"blown-out land","ChoiceLabel":"Blown-out land","ChoiceObsolete":1,"ChoiceDescription":"Blownout land consists of areas from which all or most of the soil material has been removed by extreme wind erosion. The areas are generally shallow depressions that have flat or irregular floors. In some places the floor is a layer of material that is more resistant to wind erosion than the removed material or is a layer of pebbles or cobbles. In other places the floor may have been formed from exposure of the water table. Areas that are covered by water most of the year are mapped as Water. Some areas have a few hummocks or small dunes. Few areas of blown-out land are large enough to be delineated; small areas can be shown by spot symbols.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"chutes","ChoiceLabel":"Chutes","ChoiceObsolete":0,"ChoiceDescription":"Chutes are elongated areas on steep mountain slopes that lack vegetation. The vegetation has been removed by avalanche or mass movement activity. Chutes consist of exposed bedrock, rock fragments, and large woody debris. Their slopes are parallel to the slope of the mountain, and their lengths are at least ten times their widths.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"cinder land","ChoiceLabel":"Cinder land","ChoiceObsolete":0,"ChoiceDescription":"Cinder land is composed of loose cinders and other scoriaceous magmatic ejecta. The water-holding capacity is very low, and trafficability is poor.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"cirque land","ChoiceLabel":"Cirque land","ChoiceObsolete":1,"ChoiceDescription":"Cirque land consists of areas of rock and rubble that are characteristically bowl-like and semicircular in shape. The areas have been caused by glacial erosion.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"dams","ChoiceLabel":"Dams","ChoiceObsolete":0,"ChoiceDescription":"Dams are artificial structures, oriented across a watercourse or natural drainage area, for the purpose of impounding or diverting water.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"dumps","ChoiceLabel":"Dumps","ChoiceObsolete":0,"ChoiceDescription":"Dumps are areas of smoothed or uneven accumulations or piles of waste rock and general refuse. The phase, Dumps, mine, consist of areas of waste rock from mines, quarries, and smelters. The component name remains Dumps. Some dumps that are closely associated pits are mapped as Dumps-Pits complex.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"dune land","ChoiceLabel":"Dune land","ChoiceObsolete":0,"ChoiceDescription":"Dune land consists of sand in ridges and intervening troughs that shift with the wind.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"glaciers","ChoiceLabel":"Glaciers","ChoiceObsolete":0,"ChoiceDescription":"Glaciers are large masses of ice that formed, at least in part, on land by the compaction and recrystallization of snow. They may be moving slowly downslope or outward in all directions because of the stress of their own weight; or, they may be retreating or be stagnant. A little earthy material may be on or in the ice.","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"gullied land","ChoiceLabel":"Gullied land","ChoiceObsolete":0,"ChoiceDescription":"Gullied land consists of areas where erosion has cut a network of V-shaped or U-shaped channels. The areas resemble miniature badlands. Generally, gullies are so deep that extensive reshaping is necessary for most uses. Small areas can be shown by spot symbols. Phases that indicate the kind of material remaining may be useful for some areas.","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"gypsum land","ChoiceLabel":"Gypsum land","ChoiceObsolete":1,"ChoiceDescription":"Gypsum land consists of exposures of nearly pure soft gypsum. The surface is generally very unstable and erodes easily. Trafficability is very poor. Areas of hard gypsum are mapped as Rock outcrop.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"lava flows","ChoiceLabel":"Lava flows","ChoiceObsolete":0,"ChoiceDescription":"Lava flows are areas covered with lava. In most humid regions, the flows are of Holcene age; but, in arid and very cold regions, they may be older. Most flows have sharp, jagged surfaces, crevices, and angular blocks that are characteristic of lava. Others are relatively smooth and have a ropy glazed surface. A little earthy material may be in a few rocks and sheltered pockets, but the flows are virtually devoid of plants other than lichens.\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":14,"ChoiceName":"oil-waste land","ChoiceLabel":"Oil-waste land","ChoiceObsolete":0,"ChoiceDescription":"Oil-waste land consists of areas where liquid oily wastes, principally of saltwater and oil, have accumulated. It includes slush pits and adjacent areas that are affected by the liquid wastes. The land is barren, although some of it can be reclaimed at high cost.","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":15,"ChoiceName":"pits","ChoiceLabel":"Pits","ChoiceObsolete":0,"ChoiceDescription":"Pits are open excavations from which soil and commonly underlying material have been removed, exposing either rock or other material. ","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":16,"ChoiceName":"playas","ChoiceLabel":"Playas","ChoiceObsolete":0,"ChoiceDescription":"Playas are barren flats in closed basins in arid regions. Many of the areas are subject to wind erosion, and many are saline, sodic, or both. The water table may be near the surface sometimes.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":17,"ChoiceName":"riverwash","ChoiceLabel":"Riverwash","ChoiceObsolete":0,"ChoiceDescription":"Riverwash is unstabilized sandy, silty, clayey, or gravelly sediment that is flooded, washed, and reworked frequently by rivers.\r\n\r\n","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":18,"ChoiceName":"rock outcrop","ChoiceLabel":"Rock outcrop","ChoiceObsolete":0,"ChoiceDescription":"Rock outcrop consists of exposures of bare bedrock, other than lava flows and rock-lined pits. If needed, map units can be named according to the kind of rock. ","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":19,"ChoiceName":"rubble land","ChoiceLabel":"Rubble land","ChoiceObsolete":0,"ChoiceDescription":"Rubble land consists of areas of cobbles, stones, and boulders. Rubble land is commonly at the base of mountains, but some areas are deposits of cobbles, stones, and boulders left on mountainsides by glaciation or by periglacial processes. Rubble land has a length that is less than ten times the width. A line connecting the widest points of rubble land is perpendicular to the slope of the mountain.","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":20,"ChoiceName":"salt flats","ChoiceLabel":"Salt flats","ChoiceObsolete":1,"ChoiceDescription":"Salt flats are undrained flats that have surface deposits of crystalline salt overlying stratified, very strongly saline sediment. These areas are closed basins in arid regions. The water table may be near the surface sometimes.","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":21,"ChoiceName":"scoria land","ChoiceLabel":"Scoria land","ChoiceObsolete":1,"ChoiceDescription":"Scoria land consists of areas of slaglike clinkers, burned shale, and fine-grained sandstone which remain after coal beds burn out. (Scoria land should not be confused with volcanic slag.)","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4976,"DomainName":"miscellaneous_areas","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":22,"ChoiceName":"slickens","ChoiceLabel":"Slickens","ChoiceObsolete":0,"ChoiceDescription":"Slickens are accumulations of fine-textured material, such as that separated in placer mine and ore mill operations. 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NSSH Part 627, Exhibit 627-1.","ColumnPhysicalName":"miscellaneousarea","ColumnLogicalName":"miscellaneous_area"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"bare mud","ChoiceLabel":"Bare mud","ChoiceObsolete":1,"ChoiceDescription":"A silty, clayey or organic bottom matrix, with little or no aquatic vegetation or algae.","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"bare sand","ChoiceLabel":"Bare sand","ChoiceObsolete":1,"ChoiceDescription":"A sandy bottom matrix, with little or no aquatic vegetation or algae.","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":3,"ChoiceName":"extremely stony/bouldery","ChoiceLabel":"Extreme stony/bouldery","ChoiceObsolete":1,"ChoiceDescription":"A bottom dominated (3 to <15% surface cover) by boulders (or stones).","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":4,"ChoiceName":"very stony/bouldery","ChoiceLabel":"Very stony/bouldery","ChoiceObsolete":0,"ChoiceDescription":"3 to <15 % cover with fragments > 250 mm in size","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":5,"ChoiceName":"stony/bouldery","ChoiceLabel":"Stony/bouldery","ChoiceObsolete":0,"ChoiceDescription":"0.1 to <0.1 % of surface cover with fragments > 250 mm in size","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"rubbly","ChoiceLabel":"Rubbly","ChoiceObsolete":0,"ChoiceDescription":"A bottom substantially covered (15 to <50% surface cover) by large coarse fragments of various sizes.","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":7,"ChoiceName":"very rubbly","ChoiceLabel":"Very Rubbly","ChoiceObsolete":0,"ChoiceDescription":">= 50 cover with fragments >250 mm in size.","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":8,"ChoiceName":"shelly","ChoiceLabel":"Shelly","ChoiceObsolete":1,"ChoiceDescription":"A bottom dominated by aquatic shells or shell fragments.","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":9,"ChoiceName":"extremely gravelly or cobbly","ChoiceLabel":"Extremely gravelly/cobbly","ChoiceObsolete":1,"ChoiceDescription":"a bottom dominated (3 to <15% surface cover) by gravel or cobbles.","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":10,"ChoiceName":"very gravelly/cobbly","ChoiceLabel":"Very gravelly/cobbly","ChoiceObsolete":0,"ChoiceDescription":"A bottom partially covered by gravel or cobbles (0.1 to <3% surface cover).","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":11,"ChoiceName":"gravelly/cobbly","ChoiceLabel":"Gravelly/cobbly","ChoiceObsolete":1,"ChoiceDescription":"A bottom partially covered by gravel or cobbles(0.01 to <0.1% surface cover).","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"fine unconsolidated mineral substrate - fine","ChoiceLabel":"Fine unconsolidated mineral substrate - fine","ChoiceObsolete":0,"ChoiceDescription":"Soil surface layer with textures of coarse sandy loam or finer. 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Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"coarse unconsolidated mineral substrate - gravel/cobble","ChoiceLabel":"Coarse unconsolidated mineral substrate - gravel/cobble","ChoiceObsolete":0,"ChoiceDescription":">= 5% surface cover with fragments 2 to 250 mm in size. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"coarse unconsolidated mineral substrate - very gravelly/cobbly","ChoiceLabel":"Coarse unconsolidated mineral substrate - very gravelly/cobbly","ChoiceObsolete":0,"ChoiceDescription":"5 to 50% surface cover with fragments 2 to 250 mm in size. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"coarse unconsolidated mineral substrate - extremely gravelly or cobbly","ChoiceLabel":"Coarse unconsolidated mineral substrate - extremely gravelly or cobbly","ChoiceObsolete":0,"ChoiceDescription":">=50 surface cover with fragments 2 to 250 mm in size. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"bedrock","ChoiceLabel":"Bedrock","ChoiceObsolete":0,"ChoiceDescription":"substrate with mostly continuous formations of bedrock that cover 50% or more of the substrate surface. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012) ","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"shell substrate","ChoiceLabel":"Shell substrate","ChoiceObsolete":0,"ChoiceDescription":"A biogenic substrate that is primarily composed of shells or shell particles (clams, mussels, oysters, and or scallops). The shells could also consist of non-living mollusks. This substrate could consist of attached oysters, mussels, clam beds or scallop beds. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"algal substrate","ChoiceLabel":"Algal substrate","ChoiceObsolete":0,"ChoiceDescription":"Substrate composed of algae in various states of decomposition or growth. Examples include macroalgae and attached sponges. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":20,"ChoiceName":"coral substrate","ChoiceLabel":"Coral substrate","ChoiceObsolete":0,"ChoiceDescription":"Non-living coral reefs (or coral particles) constitute this benthic substrate; the substrate may or may not be inhabited by live corals. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":21,"ChoiceName":"organic substrate","ChoiceLabel":"Organic substrate","ChoiceObsolete":0,"ChoiceDescription":"Substrate is primarily composed of non-living organic material, likely a former tidal marsh platform. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":22,"ChoiceName":"sub-aquatic vegetated substrate","ChoiceLabel":"Sub-aquatic vegetated substrate","ChoiceObsolete":0,"ChoiceDescription":"A vegetated substrate composed of sub-aquatic species. 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Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":24,"ChoiceName":"anthropogenic substrate","ChoiceLabel":"Anthropogenic substrate","ChoiceObsolete":0,"ChoiceDescription":"A substrate primarily composed of mineral or manufactured materials that were purposefully or accidentally deposited by humans. Examples include artificial reefs, dredge deposits, stone or breakwater materials, etc.). Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"bottomtype","ColumnLogicalName":"bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"bare mud","ChoiceLabel":"Bare mud","ChoiceObsolete":1,"ChoiceDescription":"A silty, clayey or organic bottom matrix, with little or no aquatic vegetation or algae.","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"bare sand","ChoiceLabel":"Bare sand","ChoiceObsolete":1,"ChoiceDescription":"A sandy bottom matrix, with little or no aquatic vegetation or algae.","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":3,"ChoiceName":"extremely stony/bouldery","ChoiceLabel":"Extreme stony/bouldery","ChoiceObsolete":1,"ChoiceDescription":"A bottom dominated (3 to <15% surface cover) by boulders (or stones).","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":4,"ChoiceName":"very stony/bouldery","ChoiceLabel":"Very stony/bouldery","ChoiceObsolete":0,"ChoiceDescription":"3 to <15 % cover with fragments > 250 mm in size","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":5,"ChoiceName":"stony/bouldery","ChoiceLabel":"Stony/bouldery","ChoiceObsolete":0,"ChoiceDescription":"0.1 to <0.1 % of surface cover with fragments > 250 mm in size","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"rubbly","ChoiceLabel":"Rubbly","ChoiceObsolete":0,"ChoiceDescription":"A bottom substantially covered (15 to <50% surface cover) by large coarse fragments of various sizes.","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":7,"ChoiceName":"very rubbly","ChoiceLabel":"Very Rubbly","ChoiceObsolete":0,"ChoiceDescription":">= 50 cover with fragments >250 mm in size.","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":8,"ChoiceName":"shelly","ChoiceLabel":"Shelly","ChoiceObsolete":1,"ChoiceDescription":"A bottom dominated by aquatic shells or shell fragments.","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":9,"ChoiceName":"extremely gravelly or cobbly","ChoiceLabel":"Extremely gravelly/cobbly","ChoiceObsolete":1,"ChoiceDescription":"a bottom dominated (3 to <15% surface cover) by gravel or cobbles.","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":10,"ChoiceName":"very gravelly/cobbly","ChoiceLabel":"Very gravelly/cobbly","ChoiceObsolete":0,"ChoiceDescription":"A bottom partially covered by gravel or cobbles (0.1 to <3% surface cover).","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":11,"ChoiceName":"gravelly/cobbly","ChoiceLabel":"Gravelly/cobbly","ChoiceObsolete":1,"ChoiceDescription":"A bottom partially covered by gravel or cobbles(0.01 to <0.1% surface cover).","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"fine unconsolidated mineral substrate - fine","ChoiceLabel":"Fine unconsolidated mineral substrate - fine","ChoiceObsolete":0,"ChoiceDescription":"Soil surface layer with textures of coarse sandy loam or finer. 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Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"coarse unconsolidated mineral substrate - gravel/cobble","ChoiceLabel":"Coarse unconsolidated mineral substrate - gravel/cobble","ChoiceObsolete":0,"ChoiceDescription":">= 5% surface cover with fragments 2 to 250 mm in size. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"coarse unconsolidated mineral substrate - very gravelly/cobbly","ChoiceLabel":"Coarse unconsolidated mineral substrate - very gravelly/cobbly","ChoiceObsolete":0,"ChoiceDescription":"5 to 50% surface cover with fragments 2 to 250 mm in size. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"coarse unconsolidated mineral substrate - extremely gravelly or cobbly","ChoiceLabel":"Coarse unconsolidated mineral substrate - extremely gravelly or cobbly","ChoiceObsolete":0,"ChoiceDescription":">=50 surface cover with fragments 2 to 250 mm in size. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"bedrock","ChoiceLabel":"Bedrock","ChoiceObsolete":0,"ChoiceDescription":"substrate with mostly continuous formations of bedrock that cover 50% or more of the substrate surface. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012) ","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"shell substrate","ChoiceLabel":"Shell substrate","ChoiceObsolete":0,"ChoiceDescription":"A biogenic substrate that is primarily composed of shells or shell particles (clams, mussels, oysters, and or scallops). The shells could also consist of non-living mollusks. This substrate could consist of attached oysters, mussels, clam beds or scallop beds. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"algal substrate","ChoiceLabel":"Algal substrate","ChoiceObsolete":0,"ChoiceDescription":"Substrate composed of algae in various states of decomposition or growth. Examples include macroalgae and attached sponges. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":20,"ChoiceName":"coral substrate","ChoiceLabel":"Coral substrate","ChoiceObsolete":0,"ChoiceDescription":"Non-living coral reefs (or coral particles) constitute this benthic substrate; the substrate may or may not be inhabited by live corals. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":21,"ChoiceName":"organic substrate","ChoiceLabel":"Organic substrate","ChoiceObsolete":0,"ChoiceDescription":"Substrate is primarily composed of non-living organic material, likely a former tidal marsh platform. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":22,"ChoiceName":"sub-aquatic vegetated substrate","ChoiceLabel":"Sub-aquatic vegetated substrate","ChoiceObsolete":0,"ChoiceDescription":"A vegetated substrate composed of sub-aquatic species. The vegetated coverage should be estimated and the species identified (Zostera, Ruppia, Halodule, Halophila, Thalassia, etc.). Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":23,"ChoiceName":"worm substrate","ChoiceLabel":"Worm substrate","ChoiceObsolete":0,"ChoiceDescription":"A biogenic substrate that is primarily composed of the cemented or conglomerated (fine or sandy) tubes of polychaetes or other worm-like fauna. Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4980,"DomainName":"bottom_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":24,"ChoiceValue":24,"ChoiceName":"anthropogenic substrate","ChoiceLabel":"Anthropogenic substrate","ChoiceObsolete":0,"ChoiceDescription":"A substrate primarily composed of mineral or manufactured materials that were purposefully or accidentally deposited by humans. Examples include artificial reefs, dredge deposits, stone or breakwater materials, etc.). Ref: Definitions modified from CMECS Substrate Classification (FGDC, 2012)","ColumnPhysicalName":"osdbottomtype","ColumnLogicalName":"osd_bottom_type"} {"DomainID":4982,"DomainName":"physical_crust_subtype","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"depositional crust","ChoiceLabel":"Depositional crust","ChoiceObsolete":0,"ChoiceDescription":"Reversibly bonded crusts composed predominantly of primary or secondary mineral grains of sediment. They are generally rigid when moist or dry. Thickness is variable.","ColumnPhysicalName":"osdphyscrustsubtype","ColumnLogicalName":"osd_physical_crust_subtype"} {"DomainID":4982,"DomainName":"physical_crust_subtype","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"freeze-thaw crust","ChoiceLabel":"Freeze-thaw crust","ChoiceObsolete":0,"ChoiceDescription":"Reversibly bonded crusts composed predominantly of primary or secondary mineral grains. 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Intermittent or intertidal channels of the Riverine System and intertidal channels of the Estuarine System are classified as Streambed.","ColumnPhysicalName":"cowardinwetlandclass","ColumnLogicalName":"cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"aquatic bed","ChoiceLabel":"Aquatic bed","ChoiceObsolete":0,"ChoiceDescription":"The Aquatic Bed class includes wetlands and deepwater habitats dominated by plants that grow principally on or below the surface of the water for most of the growing season in most years. Water regimes include subtidal, irregularly exposed, regularly flooded, permanently flooded, intermittently exposed, semipermanently flooded, and seasonally flooded.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"emergent wetland","ChoiceLabel":"Emergent wetland","ChoiceObsolete":0,"ChoiceDescription":"The Emergent Wetland class is characterized by erect, rooted, herbaceous hydrophytes, excluding mosses and lichens. This vegetation is present for most of the growing season in most years. These wetlands are usually dominated by perennial plants. All water regimes are included except subtidal and irregularly exposed.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"forested wetland","ChoiceLabel":"forested wetland","ChoiceObsolete":0,"ChoiceDescription":"The Forested Wetland class is characterized by woody vegetation that is 6 m tall or taller. All water regimes are included except subtidal.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moss-lichen wetland","ChoiceLabel":"Moss-lichen wetland","ChoiceObsolete":0,"ChoiceDescription":"The Moss-Lichen Wetland class includes areas where mosses or lichens cover substrates other than rock and where emergents, shrubs, or trees make up less than 30% of the areal cover. The only water regime is saturated.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"reef","ChoiceLabel":"Reef","ChoiceObsolete":0,"ChoiceDescription":"The Reef class includes ridge-like or mound-like structures formed by the colonization and growth of sedentary invertebrates. Water regimes are restricted to subtidal, irregularly exposed, regularly flooded, and irregularly flooded.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"rock bottom","ChoiceLabel":"Rock bottom","ChoiceObsolete":0,"ChoiceDescription":"The Rock Bottom class includes all wetlands and deepwater habitats with substrates having an areal cover of stones, boulders, or bedrock 75% or greater and vegetative cover of less than 30%. Water regimes are restricted to subtidal, permanently flooded, intermittently exposed, and semipermanently flooded.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"rocky shore","ChoiceLabel":"Rocky shore","ChoiceObsolete":0,"ChoiceDescription":"The Rocky Shore class includes wetland environments characterized by bedrock, stones, or boulders which singly or in combination have an areal cover of 75% or more and an areal coverage by vegetation of less than 30%. Water regimes are restricted to irregularly exposed, regularly flooded, irregularly flooded, seasonally flooded, temporarily flooded, and intermittently flooded.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"scrub-shrub wetland","ChoiceLabel":"Scrub-shrub wetland","ChoiceObsolete":0,"ChoiceDescription":"The Scrub-Shrub Wetland class includes areas dominated by woody vegetation less than 6 m (20 feet) tall. The species include true shrubs, young trees, and trees or shrubs that are small or stunted because of environmental conditions. All water regimes except subtidal are included.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"streambed","ChoiceLabel":"Streambed","ChoiceObsolete":0,"ChoiceDescription":"The Streambed class includes all wetland contained within the Intermittent Subsystem of the Riverine System and all channels of the Estuarine System or of the Tidal Subsystem of the Riverine System that are completely dewatered at low tide. Water regimes are restricted to irregularly exposed, regularly flooded, irregularly flooded, seasonally flooded, temporarily flooded, and intermittently flooded.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"unconsolidated bottom","ChoiceLabel":"Unconsolidated bottom","ChoiceObsolete":0,"ChoiceDescription":"The Unconsolidated Bottom class includes all wetland and deepwater habitats with at least 25% cover of particles smaller than stones, and a vegetative cover less than 30%. Water regimes are restricted to subtidal, permanently flooded, intermittently exposed, and semipermanently flooded.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5123,"DomainName":"cowardin_wetland_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"unconsolidated shore","ChoiceLabel":"Unconsolidated shore","ChoiceObsolete":0,"ChoiceDescription":"The Unconsolidated Shore class includes all wetland habitats having three characteristics: (1) unconsolidated substrates with less than 75% areal cover of stones, boulders, or bedrock; (2) less than 30% areal cover of vegetation other than pioneering plants; and (3) any of the following water regimes: irregularly exposed, regularly flooded, irregularly flooded, seasonally flooded, temporarily flooded, intermittently flooded, saturated, or artificially flooded. Intermittent or intertidal channels of the Riverine System and intertidal channels of the Estuarine System are classified as Streambed.","ColumnPhysicalName":"osdcowardinwetlandclass","ColumnLogicalName":"osd_cowardin_wetland_class"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"algal","ChoiceLabel":"Algal","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"aquatic moss","ChoiceLabel":"Aquatic moss","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"bedrock","ChoiceLabel":"Bedrock","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"broad-leaved deciduous","ChoiceLabel":"Broad-leaved deciduous","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"broad-leaved evergreen","ChoiceLabel":"Broad-leaved evergreen","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"cobble-gravel","ChoiceLabel":"Cobble-gravel","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"coral","ChoiceLabel":"Coral","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"dead","ChoiceLabel":"Dead","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"floating vascular","ChoiceLabel":"Floating vascular","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"lichen","ChoiceLabel":"Lichen","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"mollusk","ChoiceLabel":"Mollusk","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"moss","ChoiceLabel":"Moss","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"mud","ChoiceLabel":"Mud","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"needle-leaved deciduous","ChoiceLabel":"Needle-leaved deciduous","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"needle-leaved evergreen","ChoiceLabel":"Needle-leaved evergreen","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"nonpersistent","ChoiceLabel":"Nonpersistent","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"organic","ChoiceLabel":"Organic","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"persistent","ChoiceLabel":"Persistent","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"rooted vascular","ChoiceLabel":"Rooted vascular","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":20,"ChoiceName":"rubble","ChoiceLabel":"Rubble","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":21,"ChoiceName":"sand","ChoiceLabel":"Sand","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":22,"ChoiceName":"vegetated","ChoiceLabel":"Vegetated","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":23,"ChoiceName":"worm","ChoiceLabel":"Worm","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"cowardinwetlandsubclass","ColumnLogicalName":"cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"algal","ChoiceLabel":"Algal","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"aquatic moss","ChoiceLabel":"Aquatic moss","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"bedrock","ChoiceLabel":"Bedrock","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"broad-leaved deciduous","ChoiceLabel":"Broad-leaved deciduous","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"broad-leaved evergreen","ChoiceLabel":"Broad-leaved evergreen","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"cobble-gravel","ChoiceLabel":"Cobble-gravel","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"coral","ChoiceLabel":"Coral","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"dead","ChoiceLabel":"Dead","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"floating vascular","ChoiceLabel":"Floating vascular","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"lichen","ChoiceLabel":"Lichen","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"mollusk","ChoiceLabel":"Mollusk","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"moss","ChoiceLabel":"Moss","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"mud","ChoiceLabel":"Mud","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"needle-leaved deciduous","ChoiceLabel":"Needle-leaved deciduous","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"needle-leaved evergreen","ChoiceLabel":"Needle-leaved evergreen","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"nonpersistent","ChoiceLabel":"Nonpersistent","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"organic","ChoiceLabel":"Organic","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"persistent","ChoiceLabel":"Persistent","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"rooted vascular","ChoiceLabel":"Rooted vascular","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":20,"ChoiceName":"rubble","ChoiceLabel":"Rubble","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":21,"ChoiceValue":21,"ChoiceName":"sand","ChoiceLabel":"Sand","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":22,"ChoiceValue":22,"ChoiceName":"vegetated","ChoiceLabel":"Vegetated","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5124,"DomainName":"cowardin_wetland_subclass","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":23,"ChoiceValue":23,"ChoiceName":"worm","ChoiceLabel":"Worm","ChoiceObsolete":0,"ChoiceDescription":"Refer to Classification of Wetlands and Deep Water Habitats of the United States. FWS/OBS 79/31 December 1979 Reprinted 1992.","ColumnPhysicalName":"osdcowardinwetlandsubclass","ColumnLogicalName":"osd_cowardin_wetland_subclass"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"subtidal","ChoiceLabel":"Subtidal","ChoiceObsolete":0,"ChoiceDescription":"The substrate is continuously submerged.","ColumnPhysicalName":"cowardinwetlandsubsystem","ColumnLogicalName":"cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"tidal","ChoiceLabel":"Tidal","ChoiceObsolete":0,"ChoiceDescription":"The gradient is low and water velocity fluctuates under tidal influence. The streambed is mainly mud with occasional patches of sand. Oxygen deficits may sometimes occur and the fauna is similar to that in the Lower Perennial Subsystem. The floodplain is typically well developed.","ColumnPhysicalName":"cowardinwetlandsubsystem","ColumnLogicalName":"cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"intertidal","ChoiceLabel":"Intertidal","ChoiceObsolete":0,"ChoiceDescription":"The substrate is exposed and flooded by tides; includes the associated splash zone.","ColumnPhysicalName":"cowardinwetlandsubsystem","ColumnLogicalName":"cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"lower perennial","ChoiceLabel":"Lower perennial","ChoiceObsolete":0,"ChoiceDescription":"The gradient is low and water velocity is slow. There is no tidal influence, and some water flows throughout the year. The substrate consists mainly of sand and mud. Oxygen deficits may sometimes occur, the fauna is composed mostly of species that reach their maximum abundance in still water, and true planktonic organisms are common. The gradient is lower than that of the Upper Perennial Subsystem and the floodplain is well developed.","ColumnPhysicalName":"cowardinwetlandsubsystem","ColumnLogicalName":"cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"upper perennial","ChoiceLabel":"Upper perennial","ChoiceObsolete":0,"ChoiceDescription":"The gradient is high and velocity of the water fast. There is no tidal influence and some water flows throughout the year. The substrate consists of rock, cobbles, or gravel with occasional patches of sand. The natural dissolved oxygen concentration is normally near saturation. The fauna is characteristic of running water, and there are few or no planktonic forms. The gradient is high compared with that of the Lower Perennial Subsystem, and there is very little floodplain development.","ColumnPhysicalName":"cowardinwetlandsubsystem","ColumnLogicalName":"cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"intermittent","ChoiceLabel":"Intermittent","ChoiceObsolete":0,"ChoiceDescription":"In this Subsystem, the channel contains flowing water for only part of the year. When the water is not flowing, it may remain in isolated pools or surface water may be absent.","ColumnPhysicalName":"cowardinwetlandsubsystem","ColumnLogicalName":"cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"limnetic","ChoiceLabel":"Limnetic","ChoiceObsolete":0,"ChoiceDescription":"All deepwater habitats within the Lacustrine System; many small Lacustrine Systems have no Limnetic Subsystem.","ColumnPhysicalName":"cowardinwetlandsubsystem","ColumnLogicalName":"cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"littoral","ChoiceLabel":"Littoral","ChoiceObsolete":0,"ChoiceDescription":"All wetland habitats in the Lacustrine System. Extends from the shoreward boundary of the system to a depth of 2 m (6.6 feet) below low water or to the maximum extent of nonpersistent emergents, if these grow at depths greater than 2 m.","ColumnPhysicalName":"cowardinwetlandsubsystem","ColumnLogicalName":"cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"subtidal","ChoiceLabel":"Subtidal","ChoiceObsolete":0,"ChoiceDescription":"The substrate is continuously submerged.","ColumnPhysicalName":"osdcowardinwetlandsubsystem","ColumnLogicalName":"osd_cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"tidal","ChoiceLabel":"Tidal","ChoiceObsolete":0,"ChoiceDescription":"The gradient is low and water velocity fluctuates under tidal influence. The streambed is mainly mud with occasional patches of sand. 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There is no tidal influence, and some water flows throughout the year. The substrate consists mainly of sand and mud. Oxygen deficits may sometimes occur, the fauna is composed mostly of species that reach their maximum abundance in still water, and true planktonic organisms are common. The gradient is lower than that of the Upper Perennial Subsystem and the floodplain is well developed.","ColumnPhysicalName":"osdcowardinwetlandsubsystem","ColumnLogicalName":"osd_cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"upper perennial","ChoiceLabel":"Upper perennial","ChoiceObsolete":0,"ChoiceDescription":"The gradient is high and velocity of the water fast. There is no tidal influence and some water flows throughout the year. The substrate consists of rock, cobbles, or gravel with occasional patches of sand. The natural dissolved oxygen concentration is normally near saturation. The fauna is characteristic of running water, and there are few or no planktonic forms. The gradient is high compared with that of the Lower Perennial Subsystem, and there is very little floodplain development.","ColumnPhysicalName":"osdcowardinwetlandsubsystem","ColumnLogicalName":"osd_cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"intermittent","ChoiceLabel":"Intermittent","ChoiceObsolete":0,"ChoiceDescription":"In this Subsystem, the channel contains flowing water for only part of the year. When the water is not flowing, it may remain in isolated pools or surface water may be absent.","ColumnPhysicalName":"osdcowardinwetlandsubsystem","ColumnLogicalName":"osd_cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"limnetic","ChoiceLabel":"Limnetic","ChoiceObsolete":0,"ChoiceDescription":"All deepwater habitats within the Lacustrine System; many small Lacustrine Systems have no Limnetic Subsystem.","ColumnPhysicalName":"osdcowardinwetlandsubsystem","ColumnLogicalName":"osd_cowardin_wetland_subsystem"} {"DomainID":5125,"DomainName":"cowardin_wetland_subsystem","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"littoral","ChoiceLabel":"Littoral","ChoiceObsolete":0,"ChoiceDescription":"All wetland habitats in the Lacustrine System. Extends from the shoreward boundary of the system to a depth of 2 m (6.6 feet) below low water or to the maximum extent of nonpersistent emergents, if these grow at depths greater than 2 m.","ColumnPhysicalName":"osdcowardinwetlandsubsystem","ColumnLogicalName":"osd_cowardin_wetland_subsystem"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"estuarine","ChoiceLabel":"Estuarine","ChoiceObsolete":0,"ChoiceDescription":"The Estuarine System consists of deepwater tidal habitats and adjacent tidal wetlands that are usually semienclosed by land but have open, partly obstructed, or sporadic access to the open ocean, and in which ocean water is at least occasionally diluted by freshwater runoff from the land. The salinity may be periodically increased above that of the open ocean by evaporation. Along some low-energy coastlines there is appreciable dilution of sea water. Offshore areas with typical estuarine plants and animals, such as red mangroves (Rhizophora mangle) and eastern oysters (Crassostrea virginica), are also included in the Estuarine System.","ColumnPhysicalName":"cowardinwetlandsystem","ColumnLogicalName":"cowardin_wetland_system"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"lacustrine","ChoiceLabel":"Lacustrine","ChoiceObsolete":0,"ChoiceDescription":"The Lacustrine System includes wetlands and deepwater habitats with all of the following characteristics: (1) situated in a topographic depression or a dammed river channel; (2) lacking trees, shrubs, persistent emergents, emergent mosses or lichens with greater than 30% areal coverage; and (3) total area exceeds 8 ha (20 acres). Similar wetland and deepwater habitats totaling less than 8 ha are also included in the Lacustrine System if an active wave-formed or bedrock shoreline feature makes up all or part of the boundary, or if the water depth in the deepest part of the basin exceeds 2 m (6.6 feet) at low water. Lacustrine waters may be tidal or nontidal, but oceanderived salinity is always less than 0.5 %.","ColumnPhysicalName":"cowardinwetlandsystem","ColumnLogicalName":"cowardin_wetland_system"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"marine","ChoiceLabel":"Marine","ChoiceObsolete":0,"ChoiceDescription":"The Marine System consists of the open ocean overlying the continental shelf and its associated high-energy coastline. Marine habitats are exposed to the waves and currents of the open ocean and the water regimes are determined primarily by the ebb and flow of oceanic tides. Salinities exceed 30 , with little or no dilution except outside the mouths of estuaries. Shallow coastal indentations or bays without appreciable freshwater inflow, and coasts with exposed rocky islands that provide the mainland with little or no shelter from wind and waves, are also considered part of the Marine System because they generally support typical marine biota.","ColumnPhysicalName":"cowardinwetlandsystem","ColumnLogicalName":"cowardin_wetland_system"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"palustrine","ChoiceLabel":"Palustrine","ChoiceObsolete":0,"ChoiceDescription":"The Palustrine System includes all nontidal wetlands dominated by trees, shrubs, persistent emergents, emergent mosses or lichens, and all such wetlands that occur in tidal areas where salinity due to ocean-derived salts is below 0.5 %. It also includes wetlands lacking such vegetation, but with all of the following four characteristics: (1) area less than 8 ha (20 acres); (2) active wave-formed or bedrock shoreline features lacking; (3) water depth in the deepest part of basin less than 2 m at low water; and (4) salinity due to ocean-derived salts less than 0.5 %.","ColumnPhysicalName":"cowardinwetlandsystem","ColumnLogicalName":"cowardin_wetland_system"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"riverine","ChoiceLabel":"Riverine","ChoiceObsolete":0,"ChoiceDescription":"The Riverine System includes all wetlands and deepwater habitats contained within a channel, with two exceptions: (1) wetlands dominated by trees, shrubs, persistent emergents, emergent mosses, or lichens, and (2) habitats with water containing ocean-derived salts in excess of 0.5 . A channel is \"an open conduit either naturally or artificially created which periodically or continuously contains moving water, or which forms a connecting link between two bodies of standing water\" (Langbein and Iseri 1960:5).","ColumnPhysicalName":"cowardinwetlandsystem","ColumnLogicalName":"cowardin_wetland_system"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"estuarine","ChoiceLabel":"Estuarine","ChoiceObsolete":0,"ChoiceDescription":"The Estuarine System consists of deepwater tidal habitats and adjacent tidal wetlands that are usually semienclosed by land but have open, partly obstructed, or sporadic access to the open ocean, and in which ocean water is at least occasionally diluted by freshwater runoff from the land. The salinity may be periodically increased above that of the open ocean by evaporation. Along some low-energy coastlines there is appreciable dilution of sea water. Offshore areas with typical estuarine plants and animals, such as red mangroves (Rhizophora mangle) and eastern oysters (Crassostrea virginica), are also included in the Estuarine System.","ColumnPhysicalName":"osdcowardinwetlandsystem","ColumnLogicalName":"osd_cowardin_wetland_system"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"lacustrine","ChoiceLabel":"Lacustrine","ChoiceObsolete":0,"ChoiceDescription":"The Lacustrine System includes wetlands and deepwater habitats with all of the following characteristics: (1) situated in a topographic depression or a dammed river channel; (2) lacking trees, shrubs, persistent emergents, emergent mosses or lichens with greater than 30% areal coverage; and (3) total area exceeds 8 ha (20 acres). Similar wetland and deepwater habitats totaling less than 8 ha are also included in the Lacustrine System if an active wave-formed or bedrock shoreline feature makes up all or part of the boundary, or if the water depth in the deepest part of the basin exceeds 2 m (6.6 feet) at low water. Lacustrine waters may be tidal or nontidal, but oceanderived salinity is always less than 0.5 %.","ColumnPhysicalName":"osdcowardinwetlandsystem","ColumnLogicalName":"osd_cowardin_wetland_system"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"marine","ChoiceLabel":"Marine","ChoiceObsolete":0,"ChoiceDescription":"The Marine System consists of the open ocean overlying the continental shelf and its associated high-energy coastline. Marine habitats are exposed to the waves and currents of the open ocean and the water regimes are determined primarily by the ebb and flow of oceanic tides. Salinities exceed 30 , with little or no dilution except outside the mouths of estuaries. Shallow coastal indentations or bays without appreciable freshwater inflow, and coasts with exposed rocky islands that provide the mainland with little or no shelter from wind and waves, are also considered part of the Marine System because they generally support typical marine biota.","ColumnPhysicalName":"osdcowardinwetlandsystem","ColumnLogicalName":"osd_cowardin_wetland_system"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"palustrine","ChoiceLabel":"Palustrine","ChoiceObsolete":0,"ChoiceDescription":"The Palustrine System includes all nontidal wetlands dominated by trees, shrubs, persistent emergents, emergent mosses or lichens, and all such wetlands that occur in tidal areas where salinity due to ocean-derived salts is below 0.5 %. It also includes wetlands lacking such vegetation, but with all of the following four characteristics: (1) area less than 8 ha (20 acres); (2) active wave-formed or bedrock shoreline features lacking; (3) water depth in the deepest part of basin less than 2 m at low water; and (4) salinity due to ocean-derived salts less than 0.5 %.","ColumnPhysicalName":"osdcowardinwetlandsystem","ColumnLogicalName":"osd_cowardin_wetland_system"} {"DomainID":5126,"DomainName":"cowardin_wetland_system","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"riverine","ChoiceLabel":"Riverine","ChoiceObsolete":0,"ChoiceDescription":"The Riverine System includes all wetlands and deepwater habitats contained within a channel, with two exceptions: (1) wetlands dominated by trees, shrubs, persistent emergents, emergent mosses, or lichens, and (2) habitats with water containing ocean-derived salts in excess of 0.5 . A channel is \"an open conduit either naturally or artificially created which periodically or continuously contains moving water, or which forms a connecting link between two bodies of standing water\" (Langbein and Iseri 1960:5).","ColumnPhysicalName":"osdcowardinwetlandsystem","ColumnLogicalName":"osd_cowardin_wetland_system"} {"DomainID":5127,"DomainName":"crop_tree_category","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"timber","ChoiceLabel":"Timber","ChoiceObsolete":0,"ColumnPhysicalName":"croptreeprimarycat","ColumnLogicalName":"crop_tree_primary_cat"} {"DomainID":5127,"DomainName":"crop_tree_category","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"visual quality","ChoiceLabel":"Visual quality","ChoiceObsolete":0,"ColumnPhysicalName":"croptreeprimarycat","ColumnLogicalName":"crop_tree_primary_cat"} {"DomainID":5127,"DomainName":"crop_tree_category","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"water quality","ChoiceLabel":"Water quality","ChoiceObsolete":0,"ColumnPhysicalName":"croptreeprimarycat","ColumnLogicalName":"crop_tree_primary_cat"} {"DomainID":5127,"DomainName":"crop_tree_category","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"wildlife","ChoiceLabel":"Wildlife","ChoiceObsolete":0,"ColumnPhysicalName":"croptreeprimarycat","ColumnLogicalName":"crop_tree_primary_cat"} {"DomainID":5127,"DomainName":"crop_tree_category","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"timber","ChoiceLabel":"Timber","ChoiceObsolete":0,"ColumnPhysicalName":"croptreesecondarycat","ColumnLogicalName":"crop_tree_secondary_cat"} {"DomainID":5127,"DomainName":"crop_tree_category","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"visual quality","ChoiceLabel":"Visual quality","ChoiceObsolete":0,"ColumnPhysicalName":"croptreesecondarycat","ColumnLogicalName":"crop_tree_secondary_cat"} {"DomainID":5127,"DomainName":"crop_tree_category","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"water quality","ChoiceLabel":"Water quality","ChoiceObsolete":0,"ColumnPhysicalName":"croptreesecondarycat","ColumnLogicalName":"crop_tree_secondary_cat"} {"DomainID":5127,"DomainName":"crop_tree_category","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"wildlife","ChoiceLabel":"Wildlife","ChoiceObsolete":0,"ColumnPhysicalName":"croptreesecondarycat","ColumnLogicalName":"crop_tree_secondary_cat"} {"DomainID":5128,"DomainName":"crown_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"codominant","ChoiceLabel":"Codominant","ChoiceObsolete":0,"ChoiceDescription":"Tree whose crown helps to form the general level of the main canopy in even-aged stands or, in uneven-aged stands, the main canopy of the tree's immediate neighbors, receiving full light from above and comparatively little from the sides. ","ColumnPhysicalName":"crownclass","ColumnLogicalName":"crown_class"} {"DomainID":5128,"DomainName":"crown_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"dominant","ChoiceLabel":"Dominant","ChoiceObsolete":0,"ChoiceDescription":"Tree whose crown extends above the general level of the main canopy of even-aged stands or, in uneven-aged stands, above the crowns of the tree's immediate neighbors and receiving full light from above and partial light from the sides.","ColumnPhysicalName":"crownclass","ColumnLogicalName":"crown_class"} {"DomainID":5129,"DomainName":"cryptogam_cover_class_legacy","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"low","ChoiceLabel":"Low","ChoiceObsolete":0,"ChoiceDescription":"Added as a legacy choice from the ESIS database when the ESI data (from ESIS) was imported into NASIS. Actual definition of this choice is unknown.","ColumnPhysicalName":"cryptogamcovcllegacy","ColumnLogicalName":"cryptogam_cover_class_legacy"} {"DomainID":5129,"DomainName":"cryptogam_cover_class_legacy","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"medium","ChoiceLabel":"Medium","ChoiceObsolete":0,"ChoiceDescription":"Added as a legacy choice from the ESIS database when the ESI data (from ESIS) was imported into NASIS. Actual definition of this choice is unknown.","ColumnPhysicalName":"cryptogamcovcllegacy","ColumnLogicalName":"cryptogam_cover_class_legacy"} {"DomainID":5129,"DomainName":"cryptogam_cover_class_legacy","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"high","ChoiceLabel":"High","ChoiceObsolete":0,"ChoiceDescription":"Added as a legacy choice from the ESIS database when the ESI data (from ESIS) was imported into NASIS. 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{"DomainID":5164,"DomainName":"ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"tree","ChoiceLabel":"Tree","ChoiceObsolete":0,"ChoiceDescription":"Woody perennial plant species typically over 5m in height at maturity.","ColumnPhysicalName":"groundcovertype","ColumnLogicalName":"ground_cover_type"} {"DomainID":5164,"DomainName":"ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"water","ChoiceLabel":"Water","ChoiceObsolete":0,"ChoiceDescription":"The soil surface is covered by standing water.","ColumnPhysicalName":"groundcovertype","ColumnLogicalName":"ground_cover_type"} {"DomainID":5164,"DomainName":"ground_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"embedded litter","ChoiceLabel":"Embedded litter","ChoiceObsolete":1,"ChoiceDescription":"Soil surface is covered by fresh and/or partially decomposed plant residue material, including downed wood, that is not attached to a rooted plant, but is partially buried or embedded in the soil surface.","ColumnPhysicalName":"groundcovertype","ColumnLogicalName":"ground_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"bare ground","ChoiceLabel":"Bare ground","ChoiceObsolete":0,"ChoiceDescription":"Exposed bare soil surface with no other ground cover material type present.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"bedrock","ChoiceLabel":"Bedrock","ChoiceObsolete":0,"ChoiceDescription":"Exposed bare soil surface with no other ground cover material type present.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"biological crust","ChoiceLabel":"Biological crust","ChoiceObsolete":0,"ChoiceDescription":"A crust on the soil surface primarily composed of algae, cyanobacteria, and/or lichens.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"forb","ChoiceLabel":"Forb","ChoiceObsolete":0,"ChoiceDescription":"An herbaceous, broadleaved flowering plant whose above-ground stem does not become woody and persistent.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"grass or grasslike","ChoiceLabel":"Grass or grasslike","ChoiceObsolete":0,"ChoiceDescription":"Plant material that is a member of the Gramineae (true grasses), Cyperaceae (sedges), or Juncaceae (rushes) families.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"litter","ChoiceLabel":"Litter","ChoiceObsolete":0,"ChoiceDescription":"Soil surface is covered by fresh and/or partially decomposed plant residue material, including downed wood, that is not attached to a rooted plant.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"nonvascular plant","ChoiceLabel":"Nonvascular plant","ChoiceObsolete":0,"ChoiceDescription":"Plant material composed of mosses, liverworts, hornworts, or stemmed lichens.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":8,"ChoiceValue":8,"ChoiceName":"shrub or vine or liana","ChoiceLabel":"Shrub or vine or liana","ChoiceObsolete":0,"ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":9,"ChoiceValue":9,"ChoiceName":"surface fragments, large","ChoiceLabel":"Large surface fragments","ChoiceObsolete":0,"ChoiceDescription":"Loose fragments of rock equal to or greater than 3 inches in size.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":10,"ChoiceValue":10,"ChoiceName":"surface fragments, small","ChoiceLabel":"Small surface fragments","ChoiceObsolete":0,"ChoiceDescription":"Loose fragments of rock greater than 0.25 and less than 3 inches in size.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":11,"ChoiceValue":11,"ChoiceName":"tree","ChoiceLabel":"Tree","ChoiceObsolete":0,"ChoiceDescription":"Woody perennial plant species typically over 5m in height at maturity.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":12,"ChoiceValue":12,"ChoiceName":"water","ChoiceLabel":"Water","ChoiceObsolete":0,"ChoiceDescription":"The soil surface is covered by standing water.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":13,"ChoiceValue":13,"ChoiceName":"downed wood, fine-small","ChoiceLabel":"Fine-small downed wood","ChoiceObsolete":0,"ChoiceDescription":"Dead, downed wood less than 0.4 inches in diameter. 1 hour fuels.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":14,"ChoiceValue":14,"ChoiceName":"downed wood, fine-medium","ChoiceLabel":"Fine-medium downed wood","ChoiceObsolete":0,"ChoiceDescription":"Dead, downed wood 0.4 to less than 1 inch in diameter. 10 hour fuels.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":15,"ChoiceValue":15,"ChoiceName":"downed wood, fine-large","ChoiceLabel":"Fine-large downed wood","ChoiceObsolete":0,"ChoiceDescription":"Dead, downed wood 1 to less than 3 inches in diameter. 100 hour fuels.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":16,"ChoiceValue":16,"ChoiceName":"downed wood, coarse-small","ChoiceLabel":"Coarse-small downed wood","ChoiceObsolete":0,"ChoiceDescription":"Dead, downed wood 3 to less than 9 inches in diameter. 1,000 hour fuels.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":17,"ChoiceValue":17,"ChoiceName":"downed wood, coarse-large","ChoiceLabel":"Coarse-large downed wood","ChoiceObsolete":0,"ChoiceDescription":"Dead, downed wood equal to or greater than 9 inches in diameter. 10,000 hour fuels.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":18,"ChoiceValue":18,"ChoiceName":"tree snags, hard","ChoiceLabel":"Hard tree snags","ChoiceObsolete":0,"ChoiceDescription":"Dead, standing tree trunks that are > 4\" in diameter at 4.5 feet above the ground, and > 6 feet in height; have no evidence of decay; and with bark largely intact. Smaller snags count as downed wood.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":19,"ChoiceValue":19,"ChoiceName":"tree snags, soft","ChoiceLabel":"Soft tree snags","ChoiceObsolete":0,"ChoiceDescription":"Dead, standing tree trunks that are > 4\" in diameter at 4.5 feet above the ground, and > 6 feet in height; have no evidence of decay; and with bark that has partially or totally sloughed off. Smaller snags count as downed wood.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5165,"DomainName":"ground_surface_cover_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":20,"ChoiceValue":20,"ChoiceName":"embedded litter","ChoiceLabel":"Embedded litter","ChoiceObsolete":1,"ChoiceDescription":"Soil surface is covered by fresh and/or partially decomposed plant residue material, including downed wood, that is not attached to a rooted plant, but is partially buried or embedded in the soil surface.","ColumnPhysicalName":"groundsurfcovtype","ColumnLogicalName":"ground_surface_cover_type"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"unusually good","ChoiceLabel":"Unusually good","ChoiceObsolete":0,"ColumnPhysicalName":"growingseasonrating","ColumnLogicalName":"growing_season_rating"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"above average","ChoiceLabel":"Above average","ChoiceObsolete":0,"ColumnPhysicalName":"growingseasonrating","ColumnLogicalName":"growing_season_rating"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"average","ChoiceLabel":"Average","ChoiceObsolete":0,"ColumnPhysicalName":"growingseasonrating","ColumnLogicalName":"growing_season_rating"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"below average","ChoiceLabel":"Below average","ChoiceObsolete":0,"ColumnPhysicalName":"growingseasonrating","ColumnLogicalName":"growing_season_rating"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"unusually poor","ChoiceLabel":"Unusually poor","ChoiceObsolete":0,"ColumnPhysicalName":"growingseasonrating","ColumnLogicalName":"growing_season_rating"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"unusually good","ChoiceLabel":"Unusually good","ChoiceObsolete":0,"ColumnPhysicalName":"osdgrowingseasonrating","ColumnLogicalName":"osd_growing_season_rating"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"above average","ChoiceLabel":"Above average","ChoiceObsolete":0,"ColumnPhysicalName":"osdgrowingseasonrating","ColumnLogicalName":"osd_growing_season_rating"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"average","ChoiceLabel":"Average","ChoiceObsolete":0,"ColumnPhysicalName":"osdgrowingseasonrating","ColumnLogicalName":"osd_growing_season_rating"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"below average","ChoiceLabel":"Below average","ChoiceObsolete":0,"ColumnPhysicalName":"osdgrowingseasonrating","ColumnLogicalName":"osd_growing_season_rating"} {"DomainID":5166,"DomainName":"growing_season_rating","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"unusually poor","ChoiceLabel":"Unusually poor","ChoiceObsolete":0,"ColumnPhysicalName":"osdgrowingseasonrating","ColumnLogicalName":"osd_growing_season_rating"} {"DomainID":5167,"DomainName":"gully_rill_presence","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none","ChoiceLabel":"None","ChoiceObsolete":0,"ColumnPhysicalName":"gullyrillpresence","ColumnLogicalName":"gully_rill_presence"} {"DomainID":5167,"DomainName":"gully_rill_presence","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"few","ChoiceLabel":"Few","ChoiceObsolete":0,"ColumnPhysicalName":"gullyrillpresence","ColumnLogicalName":"gully_rill_presence"} {"DomainID":5167,"DomainName":"gully_rill_presence","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"numerous","ChoiceLabel":"Numerous","ChoiceObsolete":0,"ColumnPhysicalName":"gullyrillpresence","ColumnLogicalName":"gully_rill_presence"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"riverine","ChoiceLabel":"RIVERINE","ChoiceObsolete":0,"ChoiceDescription":"Riverine wetlands occur in flood plains and riparian corridors in association with stream channels. Dominant water sources are often overbank flow from the channel or subsurface hydraulic connections between the stream channel and wetlands. However, sources may be interflow and return flow from adjacent uplands, occasional overland flow from adjacent uplands, tributary inflow, and precipitation. At their headwater, RIVERINE wetlands often are replaced by SLOPE or DEPRESSIONAL wetlands where the channel morphology may disappear. They may intergrade with poorly drained flats or uplands. Perennial flow in the channel is not a requirement.","ColumnPhysicalName":"hgmclass","ColumnLogicalName":"hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"depressional","ChoiceLabel":"DEPRESSIONAL","ChoiceObsolete":0,"ChoiceDescription":"Depressional wetlands occur in topographic depressions. Dominant water sources are precipitation,\r\nground water discharge, and both interflow and overland flow from adjacent uplands. The direction of\r\nflow is normally from the surrounding uplands toward the center of the depression. Elevation contours are closed, thus allowing the accumulation of surface water. Depressional wetlands may have any combination of inlets and outlets or lack them completely. Dominant hydrodynamics are vertical fluctuations, primarily seasonal. Depressional wetlands may lose water through intermittent or perennial drainage from an outlet, by evapotranspiration and, if they are not receiving ground water discharge, may slowly contribute to ground water. Peat deposits may develop in depressional wetlands. Prairie potholes are a common example of depressional wetlands.","ColumnPhysicalName":"hgmclass","ColumnLogicalName":"hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"slope","ChoiceLabel":"SLOPE","ChoiceObsolete":0,"ChoiceDescription":"Slope wetlands normally are found where there is a discharge of ground water to the land surface. They normally occur on sloping land; elevation gradients may range from steep hillsides to slight slopes. Slope wetlands are usually incapable of depressional storage because they lack the necessary closed contours. Principal water sources are usually ground water return flow and interflow from surrounding uplands, as well as precipitation. Hydrodynamics are dominated by downslope unidirectional water flow. Slope wetlands can occur in nearly flat landscapes if ground water discharge is a dominant source to the wetland surface. Slope wetlands lose water primarily by saturation subsurface and surface flows and by evapotranspiration. SLOPE wetlands may develop channels, but the channels serve only to convey water away from the SLOPE wetland. Fens are a common example of slope wetlands.","ColumnPhysicalName":"hgmclass","ColumnLogicalName":"hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"mineral soil flats","ChoiceLabel":"MINERAL SOIL FLATS","ChoiceObsolete":0,"ChoiceDescription":"Mineral soils flats are most common on interfluves, extensive relic lake bottoms, or large historic flood plain terraces where the main source of water is precipitation. They receive no ground water discharge, which distinguishes them from DEPRESSIONAL and SLOPE wetlands. Dominant hydrodynamics are vertical fluctuations. Mineral soil flats lose water by evapotranspiration, saturation overland flow, and seepage to underlying ground water. They are distinguished from flat upland areas by their poor vertical drainage, often due to spodic horizons and hardpans, and low lateral drainage, usually due to low hydraulic\r\ngradients. Mineral soil flats that accumulate peat can eventually become the class ORGANIC SOIL FLATS. Pine flatwoods with hydric soils are a common example of MINERAL SOIL FLAT wetlands.","ColumnPhysicalName":"hgmclass","ColumnLogicalName":"hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"organic soil flats","ChoiceLabel":"ORGANIC SOIL FLATS","ChoiceObsolete":0,"ChoiceDescription":"Organic soil flats , or extensive peatlands, differ from mineral soil flats , in part because their elevation and topography are controlled by vertical accretion of organic matter. They occur commonly on flat interfluves, but may also be located where depressions have become filled with peat to form a relatively large flat surface. Water source is dominated by precipitation, while water loss is by saturation overland flow and seepage to underlying ground water. Raised bogs share many of these characteristics, but may be considered a separate class because of their convex upward form and distinct edaphic conditions for plants. Portions of the Everglades and northern Minnesota peatlands are common examples of organic soil flat wetlands.","ColumnPhysicalName":"hgmclass","ColumnLogicalName":"hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"estuarine fringe","ChoiceLabel":"ESTUARINE FRINGE","ChoiceObsolete":0,"ChoiceDescription":"Estuarine fringe wetlands occur along coasts and estuaries and are under the influence of sea level. They intergrade landward with Riverine wetlands where tidal currents diminish and riverflow becomes the dominant water source. Additional water sources may be ground water discharge and precipitation. The interface between the estuarine fringe and Riverine classes is where bidirectional flows from tides dominate\r\nover unidirectional ones controlled by flood plain slope of Riverine wetlands. Because estuarine fringe wetlands frequently flood and water table elevations are controlled mainly by sea surface elevation, estuarine fringe wetlands seldom dry for significant periods. estuarine fringe wetlands lose water by tidal exchange, by saturated overland flow to tidal creek channels, and by evapotranspiration. Organic matter\r\nnormally accumulates in higher elevation marsh areas where flooding is less frequent and the wetlands are isolated from shoreline wave erosion by intervening areas of low marsh. Spartina alterniflora salt marshes are common examples of estuarine fringe wetlands.","ColumnPhysicalName":"hgmclass","ColumnLogicalName":"hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"lacustrine fringe","ChoiceLabel":"LACUSTRINE FRINGE","ChoiceObsolete":0,"ChoiceDescription":"Lacustrine fringe wetlands are adjacent to lakes where the water elevation of the lake maintains the water table in the wetland. In some cases, these wetlands consist of a floating mat attached to land. Additional sources of water are precipitation and ground water discharge, the latter dominating where lacustrine fringe wetlands intergrade with uplands or SLOPE wetlands. Surface water flow is bidirectional, usually controlled by water-level fluctuations such as seiches in the adjoining lake. Lacustrine fringe wetlands are indistinguishable from depressional wetlands where the size of the lake becomes so small relative to fringe wetlands that the lake is incapable of stabilizing water tables. Lacustrine fringe wetlands lose water by flow returning to the lake after flooding, by saturation surface flow, and by evapotranspiration. Organic matter normally accumulates in areas sufficiently protected from shoreline wave erosion. Unimpounded marshes bordering the Great Lakes are a common example of lacustrine fringe wetlands.","ColumnPhysicalName":"hgmclass","ColumnLogicalName":"hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"riverine","ChoiceLabel":"RIVERINE","ChoiceObsolete":0,"ChoiceDescription":"Riverine wetlands occur in flood plains and riparian corridors in association with stream channels. Dominant water sources are often overbank flow from the channel or subsurface hydraulic connections between the stream channel and wetlands. However, sources may be interflow and return flow from adjacent uplands, occasional overland flow from adjacent uplands, tributary inflow, and precipitation. At their headwater, RIVERINE wetlands often are replaced by SLOPE or DEPRESSIONAL wetlands where the channel morphology may disappear. They may intergrade with poorly drained flats or uplands. Perennial flow in the channel is not a requirement.","ColumnPhysicalName":"osdhgmclass","ColumnLogicalName":"osd_hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"depressional","ChoiceLabel":"DEPRESSIONAL","ChoiceObsolete":0,"ChoiceDescription":"Depressional wetlands occur in topographic depressions. Dominant water sources are precipitation,\r\nground water discharge, and both interflow and overland flow from adjacent uplands. The direction of\r\nflow is normally from the surrounding uplands toward the center of the depression. Elevation contours are closed, thus allowing the accumulation of surface water. Depressional wetlands may have any combination of inlets and outlets or lack them completely. Dominant hydrodynamics are vertical fluctuations, primarily seasonal. Depressional wetlands may lose water through intermittent or perennial drainage from an outlet, by evapotranspiration and, if they are not receiving ground water discharge, may slowly contribute to ground water. Peat deposits may develop in depressional wetlands. Prairie potholes are a common example of depressional wetlands.","ColumnPhysicalName":"osdhgmclass","ColumnLogicalName":"osd_hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"slope","ChoiceLabel":"SLOPE","ChoiceObsolete":0,"ChoiceDescription":"Slope wetlands normally are found where there is a discharge of ground water to the land surface. They normally occur on sloping land; elevation gradients may range from steep hillsides to slight slopes. Slope wetlands are usually incapable of depressional storage because they lack the necessary closed contours. Principal water sources are usually ground water return flow and interflow from surrounding uplands, as well as precipitation. Hydrodynamics are dominated by downslope unidirectional water flow. Slope wetlands can occur in nearly flat landscapes if ground water discharge is a dominant source to the wetland surface. Slope wetlands lose water primarily by saturation subsurface and surface flows and by evapotranspiration. SLOPE wetlands may develop channels, but the channels serve only to convey water away from the SLOPE wetland. Fens are a common example of slope wetlands.","ColumnPhysicalName":"osdhgmclass","ColumnLogicalName":"osd_hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"mineral soil flats","ChoiceLabel":"MINERAL SOIL FLATS","ChoiceObsolete":0,"ChoiceDescription":"Mineral soils flats are most common on interfluves, extensive relic lake bottoms, or large historic flood plain terraces where the main source of water is precipitation. They receive no ground water discharge, which distinguishes them from DEPRESSIONAL and SLOPE wetlands. Dominant hydrodynamics are vertical fluctuations. Mineral soil flats lose water by evapotranspiration, saturation overland flow, and seepage to underlying ground water. They are distinguished from flat upland areas by their poor vertical drainage, often due to spodic horizons and hardpans, and low lateral drainage, usually due to low hydraulic\r\ngradients. Mineral soil flats that accumulate peat can eventually become the class ORGANIC SOIL FLATS. Pine flatwoods with hydric soils are a common example of MINERAL SOIL FLAT wetlands.","ColumnPhysicalName":"osdhgmclass","ColumnLogicalName":"osd_hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"organic soil flats","ChoiceLabel":"ORGANIC SOIL FLATS","ChoiceObsolete":0,"ChoiceDescription":"Organic soil flats , or extensive peatlands, differ from mineral soil flats , in part because their elevation and topography are controlled by vertical accretion of organic matter. They occur commonly on flat interfluves, but may also be located where depressions have become filled with peat to form a relatively large flat surface. Water source is dominated by precipitation, while water loss is by saturation overland flow and seepage to underlying ground water. Raised bogs share many of these characteristics, but may be considered a separate class because of their convex upward form and distinct edaphic conditions for plants. Portions of the Everglades and northern Minnesota peatlands are common examples of organic soil flat wetlands.","ColumnPhysicalName":"osdhgmclass","ColumnLogicalName":"osd_hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":6,"ChoiceValue":6,"ChoiceName":"estuarine fringe","ChoiceLabel":"ESTUARINE FRINGE","ChoiceObsolete":0,"ChoiceDescription":"Estuarine fringe wetlands occur along coasts and estuaries and are under the influence of sea level. They intergrade landward with Riverine wetlands where tidal currents diminish and riverflow becomes the dominant water source. Additional water sources may be ground water discharge and precipitation. The interface between the estuarine fringe and Riverine classes is where bidirectional flows from tides dominate\r\nover unidirectional ones controlled by flood plain slope of Riverine wetlands. Because estuarine fringe wetlands frequently flood and water table elevations are controlled mainly by sea surface elevation, estuarine fringe wetlands seldom dry for significant periods. estuarine fringe wetlands lose water by tidal exchange, by saturated overland flow to tidal creek channels, and by evapotranspiration. Organic matter\r\nnormally accumulates in higher elevation marsh areas where flooding is less frequent and the wetlands are isolated from shoreline wave erosion by intervening areas of low marsh. Spartina alterniflora salt marshes are common examples of estuarine fringe wetlands.","ColumnPhysicalName":"osdhgmclass","ColumnLogicalName":"osd_hgm_class"} {"DomainID":5168,"DomainName":"hgm_class","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":7,"ChoiceValue":7,"ChoiceName":"lacustrine fringe","ChoiceLabel":"LACUSTRINE FRINGE","ChoiceObsolete":0,"ChoiceDescription":"Lacustrine fringe wetlands are adjacent to lakes where the water elevation of the lake maintains the water table in the wetland. In some cases, these wetlands consist of a floating mat attached to land. Additional sources of water are precipitation and ground water discharge, the latter dominating where lacustrine fringe wetlands intergrade with uplands or SLOPE wetlands. Surface water flow is bidirectional, usually controlled by water-level fluctuations such as seiches in the adjoining lake. Lacustrine fringe wetlands are indistinguishable from depressional wetlands where the size of the lake becomes so small relative to fringe wetlands that the lake is incapable of stabilizing water tables. Lacustrine fringe wetlands lose water by flow returning to the lake after flooding, by saturation surface flow, and by evapotranspiration. Organic matter normally accumulates in areas sufficiently protected from shoreline wave erosion. Unimpounded marshes bordering the Great Lakes are a common example of lacustrine fringe wetlands.","ColumnPhysicalName":"osdhgmclass","ColumnLogicalName":"osd_hgm_class"} {"DomainID":5173,"DomainName":"injury_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none","ChoiceLabel":"None","ChoiceObsolete":0,"ColumnPhysicalName":"injurykind","ColumnLogicalName":"injury_kind"} {"DomainID":5173,"DomainName":"injury_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"animal","ChoiceLabel":"Animal","ChoiceObsolete":0,"ColumnPhysicalName":"injurykind","ColumnLogicalName":"injury_kind"} {"DomainID":5173,"DomainName":"injury_kind","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"chemical","ChoiceLabel":"Chemical","ChoiceObsolete":0,"ColumnPhysicalName":"injurykind","ColumnLogicalName":"injury_kind"} 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Remote alternative wate site present.","ColumnPhysicalName":"pcistreamshoreerosion","ColumnLogicalName":"pci_stream_shore_erosion"} {"DomainID":5196,"DomainName":"pci_stream_shore_erosion","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"4","ChoiceLabel":"4","ChoiceObsolete":0,"ChoiceDescription":"Streambanks are grazed but stable. Mix of pasture plants and native water's edge species. Muddy livestock stream crossing(s) or pond entrance(s) not used heavily. Alternative water sites present.","ColumnPhysicalName":"pcistreamshoreerosion","ColumnLogicalName":"pci_stream_shore_erosion"} {"DomainID":5196,"DomainName":"pci_stream_shore_erosion","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"5","ChoiceLabel":"5","ChoiceObsolete":0,"ChoiceDescription":"Streambanks ungrazed or grazed infrequently. Abundant streamband or shore loving vegetation. Gravelly or constructed stable livestock stream crossing(s) or watering ramp(s). 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Some dust deposition from offsite source. Minor wind damage to foliage.","ColumnPhysicalName":"pciwinderosion","ColumnLogicalName":"pci_wind_erosion"} {"DomainID":5198,"DomainName":"pci_wind_erosion","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"5","ChoiceLabel":"5","ChoiceObsolete":0,"ChoiceDescription":"No visible signs of windblown soil or trash. No wind related leaf damage.","ColumnPhysicalName":"pciwinderosion","ColumnLogicalName":"pci_wind_erosion"} {"DomainID":5199,"DomainName":"physical_data_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"Bigint","ChoiceLabel":"Big Integer","ChoiceObsolete":0,"ColumnPhysicalName":"colphydatatype","ColumnLogicalName":"physical_data_type"} {"DomainID":5199,"DomainName":"physical_data_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"Binary","ChoiceLabel":"Binary","ChoiceObsolete":0,"ColumnPhysicalName":"colphydatatype","ColumnLogicalName":"physical_data_type"} {"DomainID":5199,"DomainName":"physical_data_type","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"Bit","ChoiceLabel":"Bit","ChoiceObsolete":0,"ColumnPhysicalName":"colphydatatype","ColumnLogicalName":"physical_data_type"} 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{"DomainID":5211,"DomainName":"reference_yield_rank","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"4","ChoiceLabel":"4","ChoiceObsolete":0,"ChoiceDescription":"Reference quadrat 4 is located in an area which represents the midpoint between Reference 3 and Reference 5.","ColumnPhysicalName":"refyieldrank","ColumnLogicalName":"reference_yield_rank"} {"DomainID":5211,"DomainName":"reference_yield_rank","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"5","ChoiceLabel":"5","ChoiceObsolete":0,"ChoiceDescription":"Reference quadrat 5 is located in a high-yielding area which represents the high-yielding situations commonly encountered on the site, excluding unusually dense patches of vegetation which would have a rare chance of being sampled.","ColumnPhysicalName":"refyieldrank","ColumnLogicalName":"reference_yield_rank"} {"DomainID":5212,"DomainName":"reproduction_abundance_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none","ChoiceLabel":"None","ChoiceObsolete":0,"ChoiceDescription":"No reproduction occurring.","ColumnPhysicalName":"reprodabundanceclass","ColumnLogicalName":"reproduction_abundance_class"} {"DomainID":5212,"DomainName":"reproduction_abundance_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"light","ChoiceLabel":"Light","ChoiceObsolete":0,"ChoiceDescription":"An occasional sprout or seedling. More than 20 feet apart.","ColumnPhysicalName":"reprodabundanceclass","ColumnLogicalName":"reproduction_abundance_class"} {"DomainID":5212,"DomainName":"reproduction_abundance_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"medium","ChoiceLabel":"Medium","ChoiceObsolete":0,"ChoiceDescription":"Sprouts or seedlings 6 to 20 feet apart.","ColumnPhysicalName":"reprodabundanceclass","ColumnLogicalName":"reproduction_abundance_class"} {"DomainID":5212,"DomainName":"reproduction_abundance_class","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"heavy","ChoiceLabel":"Heavy","ChoiceObsolete":0,"ChoiceDescription":"Sprouts or seedlings 5 feet or less apart.","ColumnPhysicalName":"reprodabundanceclass","ColumnLogicalName":"reproduction_abundance_class"} {"DomainID":5213,"DomainName":"reproduction_source","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"coppice","ChoiceLabel":"Coppice","ChoiceObsolete":0,"ChoiceDescription":"Regeneration by sprouting from roots or suckers of a previous tree that was cut or otherwise removed.","ColumnPhysicalName":"reproductionsource","ColumnLogicalName":"reproduction_source"} {"DomainID":5213,"DomainName":"reproduction_source","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"direct seeded","ChoiceLabel":"Direct seeded","ChoiceObsolete":0,"ChoiceDescription":"Regeneration is the result of seeds being placed in the soil by human hands or mechanical means.","ColumnPhysicalName":"reproductionsource","ColumnLogicalName":"reproduction_source"} {"DomainID":5213,"DomainName":"reproduction_source","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"planted","ChoiceLabel":"Planted","ChoiceObsolete":0,"ChoiceDescription":"Regeneration by planting of seedlings or saplings.","ColumnPhysicalName":"reproductionsource","ColumnLogicalName":"reproduction_source"} {"DomainID":5213,"DomainName":"reproduction_source","DomainRanked":0,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"naturally seeded","ChoiceLabel":"Naturally seeded","ChoiceObsolete":0,"ChoiceDescription":"Regeneration is the result of seeds being produced by nearby plants and seeds falling in place, or moved by wind or animals.","ColumnPhysicalName":"reproductionsource","ColumnLogicalName":"reproduction_source"} {"DomainID":5214,"DomainName":"rhi_annual_production","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"Exceeds 80% of potential production.","ColumnPhysicalName":"rhiannualprod","ColumnLogicalName":"rhi_annual_production"} {"DomainID":5214,"DomainName":"rhi_annual_production","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"60 to 80% of potential production","ColumnPhysicalName":"rhiannualprod","ColumnLogicalName":"rhi_annual_production"} {"DomainID":5214,"DomainName":"rhi_annual_production","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"40 to 60% of potential production.","ColumnPhysicalName":"rhiannualprod","ColumnLogicalName":"rhi_annual_production"} {"DomainID":5214,"DomainName":"rhi_annual_production","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"20 to 40% of potential production.","ColumnPhysicalName":"rhiannualprod","ColumnLogicalName":"rhi_annual_production"} {"DomainID":5214,"DomainName":"rhi_annual_production","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Less than 20% of potential production.","ColumnPhysicalName":"rhiannualprod","ColumnLogicalName":"rhi_annual_production"} {"DomainID":5215,"DomainName":"rhi_bare_ground","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"Amount and size of bare areas nearly totally match that expected for the site.","ColumnPhysicalName":"rhibareground","ColumnLogicalName":"rhi_bare_ground"} {"DomainID":5215,"DomainName":"rhi_bare_ground","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Slightly to moderately higher than expected for the site. Bare areas are small and rarely connected.","ColumnPhysicalName":"rhibareground","ColumnLogicalName":"rhi_bare_ground"} {"DomainID":5215,"DomainName":"rhi_bare_ground","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Moderately higher than expected for the site. Bare areas are of moderate size and sporadically connected.","ColumnPhysicalName":"rhibareground","ColumnLogicalName":"rhi_bare_ground"} {"DomainID":5215,"DomainName":"rhi_bare_ground","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Moderately to much higher than expected for the site. Bare areas are large and occasionally connected.","ColumnPhysicalName":"rhibareground","ColumnLogicalName":"rhi_bare_ground"} {"DomainID":5215,"DomainName":"rhi_bare_ground","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Much higher than expected for the site. Bare areas are large and generally connected.","ColumnPhysicalName":"rhibareground","ColumnLogicalName":"rhi_bare_ground"} {"DomainID":5216,"DomainName":"rhi_compaction_layer","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"None to minimal; not restrictive to water movement and root penetration.","ColumnPhysicalName":"rhicompactionlayer","ColumnLogicalName":"rhi_compaction_layer"} {"DomainID":5216,"DomainName":"rhi_compaction_layer","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Rarely present or is thin and weakly restrictive to water movement and root penetration.","ColumnPhysicalName":"rhicompactionlayer","ColumnLogicalName":"rhi_compaction_layer"} {"DomainID":5216,"DomainName":"rhi_compaction_layer","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Moderately wide-spread; moderately restricts water movement and root penetration.","ColumnPhysicalName":"rhicompactionlayer","ColumnLogicalName":"rhi_compaction_layer"} {"DomainID":5216,"DomainName":"rhi_compaction_layer","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Widespread; greatly restricts water movement and root penetration.","ColumnPhysicalName":"rhicompactionlayer","ColumnLogicalName":"rhi_compaction_layer"} {"DomainID":5216,"DomainName":"rhi_compaction_layer","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Extensive; severely restricts water movement and root penetration.","ColumnPhysicalName":"rhicompactionlayer","ColumnLogicalName":"rhi_compaction_layer"} {"DomainID":5217,"DomainName":"rhi_erosion_resistance","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"Matches that expected for the site. Surface soil is stabilized by organic matter decomposition products and/or a biological crust.","ColumnPhysicalName":"rhierosionresistance","ColumnLogicalName":"rhi_erosion_resistance"} {"DomainID":5217,"DomainName":"rhi_erosion_resistance","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Some reduction in soil surface stability in plant interspaces or slight reduction throughout the site. Stabilizing agents reduced below expected.","ColumnPhysicalName":"rhierosionresistance","ColumnLogicalName":"rhi_erosion_resistance"} {"DomainID":5217,"DomainName":"rhi_erosion_resistance","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Significantly reduced in at least half of the plant canopy interspaces, or moderately reduced throughout the site.","ColumnPhysicalName":"rhierosionresistance","ColumnLogicalName":"rhi_erosion_resistance"} {"DomainID":5217,"DomainName":"rhi_erosion_resistance","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Significantly reduced in most plant canopy interspaces and moderately reduced beneath plant canopies. Stabilizing agents present only in isolated patches.","ColumnPhysicalName":"rhierosionresistance","ColumnLogicalName":"rhi_erosion_resistance"} {"DomainID":5217,"DomainName":"rhi_erosion_resistance","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Extremely reduced throughout the site. Biological stabilization agents including organic matter and biological crusts virtually absent.","ColumnPhysicalName":"rhierosionresistance","ColumnLogicalName":"rhi_erosion_resistance"} {"DomainID":5218,"DomainName":"rhi_functional_struct_groups","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"F/S groups and number of species in each group closely match that expected for the site.","ColumnPhysicalName":"rhifuncstructgroups","ColumnLogicalName":"rhi_functional_struct_groups"} {"DomainID":5218,"DomainName":"rhi_functional_struct_groups","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Number of F/S groups slightly reduced; and/or relative dominance of F/S groups has been modified from that expected for the site; and/or number of species within F/S groups slightly reduced.","ColumnPhysicalName":"rhifuncstructgroups","ColumnLogicalName":"rhi_functional_struct_groups"} {"DomainID":5218,"DomainName":"rhi_functional_struct_groups","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Number of F/S groups moderately reduced; and/or one or more sub-dominant F/S groups replaced by F/S groups not expected for the site; and/or number of species within F/S groups moderately reduced.","ColumnPhysicalName":"rhifuncstructgroups","ColumnLogicalName":"rhi_functional_struct_groups"} {"DomainID":5218,"DomainName":"rhi_functional_struct_groups","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Number of F/S groups reduced; and/or one dominant group and/or one or more sub-dominant groups replaced by F/S groups not expected for the site; and/or number of species within F/S groups significantly reduced.","ColumnPhysicalName":"rhifuncstructgroups","ColumnLogicalName":"rhi_functional_struct_groups"} {"DomainID":5218,"DomainName":"rhi_functional_struct_groups","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Number of F/S groups greatly reduced; and/or relative dominance of F/S groups has been dramatically altered; and/or number of species within F/S groups dramatically reduced.","ColumnPhysicalName":"rhifuncstructgroups","ColumnLogicalName":"rhi_functional_struct_groups"} {"DomainID":5219,"DomainName":"rhi_gullies","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"Drainages are represented as natural stable channels; no signs of erosion with vegetation common.","ColumnPhysicalName":"rhigullies","ColumnLogicalName":"rhi_gullies"} {"DomainID":5219,"DomainName":"rhi_gullies","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Uncommon with vegetation stabilizing the bed and slopes; no signs of active headcuts, nickpoints, or bed erosion.","ColumnPhysicalName":"rhigullies","ColumnLogicalName":"rhi_gullies"} {"DomainID":5219,"DomainName":"rhi_gullies","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Moderate in number with indications of active erosion; vegetation is intermittent on slopes and/or bed. Occasional headcuts may be present.","ColumnPhysicalName":"rhigullies","ColumnLogicalName":"rhi_gullies"} {"DomainID":5219,"DomainName":"rhi_gullies","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Moderate to common with indications of active erosion; vegetation is intermittent on slopes and/or bed. Headcuts are active; down-cutting is not apparent.","ColumnPhysicalName":"rhigullies","ColumnLogicalName":"rhi_gullies"} {"DomainID":5219,"DomainName":"rhi_gullies","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Common with indications of active erosion and down-cutting; vegetation is infrequent on slopes and/or bed. Nickpoints and headcuts are numerous and active.","ColumnPhysicalName":"rhigullies","ColumnLogicalName":"rhi_gullies"} {"DomainID":5220,"DomainName":"rhi_infiltration_runoff","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"Infiltration and run-off are equal to that expected for the site. Plant cover (distribution and amount) adequate for site protection.","ColumnPhysicalName":"rhiinfilrunoff","ColumnLogicalName":"rhi_infiltration_runoff"} {"DomainID":5220,"DomainName":"rhi_infiltration_runoff","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Infiltration is slightly to moderately affected by minor changes in plant community composition and/or distribution. Plant cover changes have only a minor effect on infiltration.","ColumnPhysicalName":"rhiinfilrunoff","ColumnLogicalName":"rhi_infiltration_runoff"} {"DomainID":5220,"DomainName":"rhi_infiltration_runoff","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Infiltration is moderately reduced due to adverse changes in plant community composition and/or distribution. Plant cover changes negatively affect infiltration.","ColumnPhysicalName":"rhiinfilrunoff","ColumnLogicalName":"rhi_infiltration_runoff"} {"DomainID":5220,"DomainName":"rhi_infiltration_runoff","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Infiltration is greatly decreased due to adverse changes in plant community composition and/or distribution. Detrimental plant cover changes have occurred.","ColumnPhysicalName":"rhiinfilrunoff","ColumnLogicalName":"rhi_infiltration_runoff"} {"DomainID":5220,"DomainName":"rhi_infiltration_runoff","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Infiltration is severely decreased due to adverse changes in plant community composition and/or distribution. Adverse plant cover changes have occurred.","ColumnPhysicalName":"rhiinfilrunoff","ColumnLogicalName":"rhi_infiltration_runoff"} {"DomainID":5221,"DomainName":"rhi_invasive_plants","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"Rarely present on the site.","ColumnPhysicalName":"rhiinvasiveplants","ColumnLogicalName":"rhi_invasive_plants"} {"DomainID":5221,"DomainName":"rhi_invasive_plants","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Present primarily on disturbed areas pf the site.","ColumnPhysicalName":"rhiinvasiveplants","ColumnLogicalName":"rhi_invasive_plants"} {"DomainID":5221,"DomainName":"rhi_invasive_plants","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Scattered through-out the site.","ColumnPhysicalName":"rhiinvasiveplants","ColumnLogicalName":"rhi_invasive_plants"} {"DomainID":5221,"DomainName":"rhi_invasive_plants","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Common through-out the site.","ColumnPhysicalName":"rhiinvasiveplants","ColumnLogicalName":"rhi_invasive_plants"} {"DomainID":5221,"DomainName":"rhi_invasive_plants","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Dominate the site.","ColumnPhysicalName":"rhiinvasiveplants","ColumnLogicalName":"rhi_invasive_plants"} {"DomainID":5222,"DomainName":"rhi_litter_amount","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"Amount is what is expected for the site potential and weather.","ColumnPhysicalName":"rhilitteramount","ColumnLogicalName":"rhi_litter_amount"} {"DomainID":5222,"DomainName":"rhi_litter_amount","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Slightly more or less relative to site potential and weather.","ColumnPhysicalName":"rhilitteramount","ColumnLogicalName":"rhi_litter_amount"} {"DomainID":5222,"DomainName":"rhi_litter_amount","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Moderately more or less relative to site potential and weather.","ColumnPhysicalName":"rhilitteramount","ColumnLogicalName":"rhi_litter_amount"} {"DomainID":5222,"DomainName":"rhi_litter_amount","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Greatly reduced or increased relative to site potential and weather.","ColumnPhysicalName":"rhilitteramount","ColumnLogicalName":"rhi_litter_amount"} {"DomainID":5222,"DomainName":"rhi_litter_amount","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Largely absent or dominant relative to site potential and weather.","ColumnPhysicalName":"rhilitteramount","ColumnLogicalName":"rhi_litter_amount"} {"DomainID":5223,"DomainName":"rhi_litter_movement","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"Matches that expected for the site with a fairly uniform distribution of litter.","ColumnPhysicalName":"rhilittermovement","ColumnLogicalName":"rhi_litter_movement"} {"DomainID":5223,"DomainName":"rhi_litter_movement","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Slightly to moderately more than expected for the site with only small size classes of litter being displaced.","ColumnPhysicalName":"rhilittermovement","ColumnLogicalName":"rhi_litter_movement"} {"DomainID":5223,"DomainName":"rhi_litter_movement","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Moderate to small size classes of litter have been displaced. Moderate movement of smaller size classes in scattered concentrations around obstructions and in depressions.","ColumnPhysicalName":"rhilittermovement","ColumnLogicalName":"rhi_litter_movement"} {"DomainID":5223,"DomainName":"rhi_litter_movement","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Moderate to extreme; loosely concentrated near obstructions.","ColumnPhysicalName":"rhilittermovement","ColumnLogicalName":"rhi_litter_movement"} {"DomainID":5223,"DomainName":"rhi_litter_movement","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Extreme; concentrated around obstructions. Most size classes of litter have been displaced.","ColumnPhysicalName":"rhilittermovement","ColumnLogicalName":"rhi_litter_movement"} {"DomainID":5224,"DomainName":"rhi_pedestals_terracettes","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":1,"ChoiceValue":1,"ChoiceName":"none to slight","ChoiceLabel":"None to slight","ChoiceObsolete":0,"ChoiceDescription":"Current or past evidence of pedestalled plants or rocks as expected for the site. Terracettes absent or uncommon.","ColumnPhysicalName":"rhipedastalsterracettes","ColumnLogicalName":"rhi_pedestals_terracettes"} {"DomainID":5224,"DomainName":"rhi_pedestals_terracettes","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":2,"ChoiceValue":2,"ChoiceName":"slight to moderate","ChoiceLabel":"Slight to moderate","ChoiceObsolete":0,"ChoiceDescription":"Active pedestalling or terracette formation is rare; some evidence of past pedestal formation, especially in water-flow patterns and/or on exposed slopes.","ColumnPhysicalName":"rhipedastalsterracettes","ColumnLogicalName":"rhi_pedestals_terracettes"} {"DomainID":5224,"DomainName":"rhi_pedestals_terracettes","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":3,"ChoiceValue":3,"ChoiceName":"moderate","ChoiceLabel":"Moderate","ChoiceObsolete":0,"ChoiceDescription":"Slight active pedestalling; most pedestals are in flow paths and interspaces and/or on exposed slopes. Occasional terracettes present.","ColumnPhysicalName":"rhipedastalsterracettes","ColumnLogicalName":"rhi_pedestals_terracettes"} {"DomainID":5224,"DomainName":"rhi_pedestals_terracettes","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":4,"ChoiceValue":4,"ChoiceName":"moderate to extreme","ChoiceLabel":"Moderate to extreme","ChoiceObsolete":0,"ChoiceDescription":"Moderate active pedestalling; terra-cettes common. Some rocks and plants are pedestalled with occasional exposed roots.","ColumnPhysicalName":"rhipedastalsterracettes","ColumnLogicalName":"rhi_pedestals_terracettes"} {"DomainID":5224,"DomainName":"rhi_pedestals_terracettes","DomainRanked":1,"DisplayLabel":0,"ChoiceSequence":5,"ChoiceValue":5,"ChoiceName":"extreme to total","ChoiceLabel":"Extreme to total","ChoiceObsolete":0,"ChoiceDescription":"Abundant active pedestalling and numerous terracettes. 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