Pores range from none to few. Gray mottles occur in lower part of this horizon in some pedons. The BC horizon is mottled in hue of 2.5YR through 10YR, value of 4 through 7 and chroma of 6 or 8 with common gray mottles, or the matrix has hue of 2.5YR through 10YR, value of 4 through 6 and chroma of 6 or 8 and has common to many gray mottles. It is sandy clay loam or sandy loam. Pockets and thin strata of loamy sand, sandy loam, sandy clay loam and sandy clay, may occur in some pedons.
Consistency ranges from firm to friable.
The C horizon is mottled in hue of 2.5YR through 10YR, value of 4 through 7 and chroma of 1 through 8. It has the same texture range as the BC horizon. These are the Appling , Bethlehem , Cecil , Madison , Pacolet , Tumbleton , and Wedowee series of the same family and the Aragon , Cataula , Chestatee , Georgeville , Herndon , Hulett , Kolomoki , Nector, Neeses , and Spotsylvania series of closely related families. Appling, Bethlehem, Cecil, Chestatee, Georgeville, Herndon, Hulett, Madison, Pacolet, and Wedowee series formed in residual parent material in the Piedmont . In addition Argon, Georgeville, and Herndon soils have Bt horizons with silt content of more than 30 percent.