It is clay loam or silty clay loam with 28 to 35 percent clay. Some pedons have subhorizons that are silty clay. It has moderate or strong, medium or coarse blocky or subangular blocky or very coarse prismatic structure. Consistence is friable or firm. Redoximorphic accumulations may be present.
Reaction ranges from moderately acid to neutral in the upper part and pH increases with depth.
Some pedons have carbonates in the lower part of the B horizon. The Cd horizon has hue of 2.5YR through 7.5YR, value of 3 through 5, and chroma of 2 through 4. Texture ranges from loam to silty clay loam in the fine-earth fraction. It is massive and may have plate-like divisions. It is firm or very firm consistence.