Texture is mainly sandy clay loam but includes sandy loam, fine sandy loam, or clay loam. In some pedons, the Bt horizon below 40 inches includes layers of sandy clay or clay textures. The lower Bt horizon is commonly mottled. Iron depletions that have chroma of 2 or less are at depths of 4 to 6 feet. The BC horizon, where present, has hue of 5YR to 2.5Y, value of 4 to 7, and chroma of 1 to 8 or it is mottled with these colors.
Texture is sandy loam, fine sandy loam, sandy clay loam, clay loam, sandy clay or clay.
In some pedons, this horizon contains firm, brittle, strong brown to or nodules of plinthite, but no horizon within 60 inches of the surface has as much as 5 percent plinthite. The C horizon, where present, has hue of 2.5YR to 5Y, value of 4 to 8, and chroma of 1 to 8 or is mottled with these colors. Texture is commonly sandy but it ranges to clay in some pedons. These are the Orangeburg series in the same family and the Addielou , Allen , Avilla , Bama , Bonneau , Etowah , Holston , Leesburg , Minvale , Nella , Noboco , Octavia , Pikeville , Ruston , and Smithdale series in closely related families. Bonneau and Addielou soils are in an arenic subgroup.