The BC horizon, where present, has hue of 2.5YR to 10YR, value of 3 to 6, and chroma of 2 to 8 or is mottled in shades of these colors. Weathered Triassic C material is evident in this horizon. It is sandy clay loam, loam, clay loam, sandy clay, silty clay, silty clay loam or clay. The C horizon, where present, is multicolored or similar in color to the BC horizon. It is saprolite weathered from Triassic sandstone, mudstone, shale, and siltstone.
Texture is variable but is typically loamy.
Series in the same family are Albertville , Appomattox , Badin , Brockroad , Catharpin , Coghill , Corryton , Luverne , Masada , McQueen , Sweatman , Townley , and Vance series. Albertville, soils have bedrock within a depth of 40 to 60 inches. Badin and Townley soils have bedrock within 20 to 40 inches. Brockroad and Catharpin soils have lithologic discontinuity within the series control section. Luverne soils have formed in marine sediments.