Coxville soil and landscape
Soil profile: Coxville soils are very deep, clayey, poorly drained soils with moderately slow permeability.
Landscape: Coxville soils are commonly in Carolina Bays. Carolina bays are elliptical depressions concentrated along the Atlantic seaboard within coastal Delaware, Maryland, New Jersey, North Carolina, South Carolina, Virginia, Georgia, and north-central Florida. (Soil Survey of Lee County, South Carolina; by Charles M. Ogg, Natural Resources Conservation Service)
Depth Class: Very deep
Drainage Class (Agricultural): Poorly drained
Internal Free Water Occurrence: Very shallow to shallow, common to persistent
Flooding Frequency and Duration: None
Ponding Frequency and Duration: None
Index Surface Runoff: Negligible
Permeability: Moderately slow
Landscape: Lower to upper coastal plain
Landform: Flats, Carolina bays, and depressions
Geomorphic Component: Talfs, dips
Parent Material: Marine deposits or fluviomarine sediments
Slope: 0 to 2 percent
TAXONOMIC CLASS: Fine, kaolinitic, thermic Typic Paleaquults
Depth to Bedrock: Greater than 80 inches
Depth to Seasonal High Water Table: 0 to 12 inches, November to April
Rock Fragment content: 0 to 15 percent, by volume, throughout, but less than 5 percent in most pedons
Soil Reaction: Extremely acid to strongly acid, except where limed
USE AND VEGETATION: Where cultivated--corn, soybeans, and truck crops. Where wooded--loblolly and longleaf pine, sweetgum, blackgum, water oak, willow oak, water tupelo, elm, and hickory.
DISTRIBUTION AND EXTENT: Coastal Plain of North Carolina, Georgia, Florida, Alabama, Mississippi, and possibly Virginia and Louisiana with large extent.
For a detailed description, visit:
soilseries.sc.egov.usda.gov/OSD_Docs/C/COXVILLE.html
For acreage and geographic distribution, visit:
Coxville soil and landscape
Soil profile: Coxville soils are very deep, clayey, poorly drained soils with moderately slow permeability.
Landscape: Coxville soils are commonly in Carolina Bays. Carolina bays are elliptical depressions concentrated along the Atlantic seaboard within coastal Delaware, Maryland, New Jersey, North Carolina, South Carolina, Virginia, Georgia, and north-central Florida. (Soil Survey of Lee County, South Carolina; by Charles M. Ogg, Natural Resources Conservation Service)
Depth Class: Very deep
Drainage Class (Agricultural): Poorly drained
Internal Free Water Occurrence: Very shallow to shallow, common to persistent
Flooding Frequency and Duration: None
Ponding Frequency and Duration: None
Index Surface Runoff: Negligible
Permeability: Moderately slow
Landscape: Lower to upper coastal plain
Landform: Flats, Carolina bays, and depressions
Geomorphic Component: Talfs, dips
Parent Material: Marine deposits or fluviomarine sediments
Slope: 0 to 2 percent
TAXONOMIC CLASS: Fine, kaolinitic, thermic Typic Paleaquults
Depth to Bedrock: Greater than 80 inches
Depth to Seasonal High Water Table: 0 to 12 inches, November to April
Rock Fragment content: 0 to 15 percent, by volume, throughout, but less than 5 percent in most pedons
Soil Reaction: Extremely acid to strongly acid, except where limed
USE AND VEGETATION: Where cultivated--corn, soybeans, and truck crops. Where wooded--loblolly and longleaf pine, sweetgum, blackgum, water oak, willow oak, water tupelo, elm, and hickory.
DISTRIBUTION AND EXTENT: Coastal Plain of North Carolina, Georgia, Florida, Alabama, Mississippi, and possibly Virginia and Louisiana with large extent.
For a detailed description, visit:
soilseries.sc.egov.usda.gov/OSD_Docs/C/COXVILLE.html
For acreage and geographic distribution, visit: