It is silt loam or loam in the fine-earth fraction. The B horizons have hue of 10YR or 7.5YR, value of 4 or 5, and chroma of 3 through 6. Some pedons have hue of 2.5Y in the lower B horizon. The B horizons are silt loam or silty clay loam in the fine-earth fraction. The C horizon, where present, is commonly multicolored in shades of brown, yellow, green, and black.
Texture is silty clay loam, silt loam, or loam in the fine-earth fraction.
These are the Blair , Fishhook , Freeburg , Glenford , Lykens , Muren , Sardinia , Stoy , Henshaw , Ingersoll , Keene , and Xenia . All of these series are formed in materials other than serpentine. They have developed in residuum weathered from serpentine. Most areas are recessional forest brush and residential developments. Native vegetation is black oak, red oak, white oak, and Virginia pine.