Klinesville soils are less than 20 inches to bedrock. Chalfont and Doylestown soils have redox depletions of chroma 2 or less directly below the surface layer. Bedington and Penn soils which do not have the thin loess mantle. Lansdale soils contain more sand and coarse fragments. Fountainville soils have a loess mantle less than 24 inches.
Surface runoff is slow to rapid.
Permeability is moderate. Wooded areas are mixed hardwoods. The series is of moderate extent. Bucks County, Pennsylvania, 1993. Soils were previously mapped as an inclusion with Pope, Duncannon, Readington, Bedington, Penn, Lawrenceville, and Doylestown series.