It is silt loam. The E or AE horizon ranges from distinct to incipient. Clay depletions have value of 5 or 7, and chroma of 1 or 2. Some pedons have faint redoximorphic iron and manganese accumulations with value of 3 to 6 and chroma of 3 to 8. Individual subhorizons have between 25 and 45 percent clay.
Reaction ranges from very strongly acid in the upper horizons to neutral in the lower horizons.
The B horizon has hue of 10YR, 2.5Y, or 5Y, value of 4 to 6, and chroma of 2 to 6. Hue of 5Y, if present, is in the lower part. Redoximorphic iron and manganese accumulations and depletions have hue of 7.5YR, 10YR, or 2.5Y, value of 2 to 6, and chroma of 1 to 8. The Bt horizon is silty clay loam or silty clay in the upper part, and silty clay loam or silt loam in the lower part. Redoximorphic iron and manganese accumulations and depletions have colors similar to the range described in the B horizon.