Texture is silt loam, loam, clay loam, or silty clay loam. Small iron and manganese concretions are common in the lower part of the Bt horizon. The Bt horizon has weak to moderate, medium to coarse subangular blocky structure. 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.