It is silt loam in the fine-earth fraction. The B horizon has hue of 7.5YR through 5Y or is neutral, value of 3 through 6, and chroma of 0 through 4. Mottles occur at 10 to 18 inches below the soil surface. Low chroma and low value colors are inherited from the dark colored parent material of the soil, and the mottling is used to indicate reduction of iron. Texture is silt loam or silty clay loam in the fine-earth fraction.
Structure is moderate or strong, fine or medium subangular blocky.
The C horizon has hue of 10YR through 5Y or is neutral, value of 3 through 5, and chroma of 0 through 3. It is silt loam or silty clay loam in the fine-earth fraction. The Bogart , Centerburg , Conowingo , Haney , Mount Lucas , Reaville , Thackery , Tuscola , Vaughnsville , and Williamstown series are in the same family. Bogart, Centerburg, Thackery, Tuscola, Vaughnsville, and Williamstown soils are greater than 60 inches to bedrock. Haney and Mount Lucas soils do not have rock fragments of porcelanite.