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Flatwood is a soil series with impaired drainage that occurs in the southeastern United States. Flatwood soils are upland soils formed from marine sediments. A shallow water table plays a role in soil formation; typically the water table is only a few feet deep and fluctuates during the year.[1] Flatwood soils are classified in USDA soil taxonomy as fine, mixed, semiactive, mesic Aquic Hapludults.[2]

See also[edit]


  1. ^ "Archived copy". Archived from the original on September 29, 2006. Retrieved September 14, 2007.CS1 maint: archived copy as title (link)
  2. ^ Official Series Description - FLATWOODS Series Archived 2008-09-28 at the Wayback Machine