Some pedons have medium to coarse prismatic structure that parts to subangular blocky structure. The BC horizon, where present, has hue of 7.5YR through 2.5Y, value of 5 through 7, and chroma of 2 through 6. Texture is silt loam, loam, clay loam or silty clay loam. It is 0 to 16 inches thick. The C horizon has hue of 7.5YR through 2.5Y, value of 4 through 7, and chroma of 1 through 8.
Texture is silt loam, loam, clay loam, or silty clay loam.
In some pedons the C horizon is stratified and may contain strata of silty clay. These are the Prout series. Closely similar are the Cavode , Evendale , Tygart , and Tyler series. Prout soils are moderately deep and have bedrock within 40 inches of the soil surface. Cavode, Evendale, and Tygart, soils have clayey particle-size control sections.