The Blasdell, Chenango Hazleton, Itswoot, Parker, and Tunkhannock soils are deeper than 40 inches to bedrock. Lehew and Oquaga soils have less than 18 percent clay in the particle-size control sections. Cardiff soils have rock fragments dominated by slate. Deserter soils have rock dominated by basalt. Lippitt soils have been glaciated and formed in gneiss, schist, and granite.
Remote soils have clay loam textures in the B horizon.
Warwick soils formed in glacial outwash. Wyoming soils contain rounded rock fragments. Albrights , Gainesboro , Kedron , Klinesville , Leck Kill , Penn , and Ungers are in related families. Albrights, Gainesboro, Leck Kill, Penn, and Ungers soils have argillic horizons. Klinesville soils have a lithic contact at 10 to 20 inches.