These are the Clyde , Colwood , Faxon , Gansner , Kossuth , Letri , Reddick , Selma , Tripoli , Webster , and Wolcott soils in the same family and the Biscay and Westland series. Clyde, Kossuth, Letri, Tripoli, and Wolcott soils contains less gravel in the lower part of the solum and have the lower part of the solum formed in loam till. Colwood and Webster soils contain less medium and coarse sand and less gravel. Faxon soils have bedrock at depths of less than 40 inches. Gansner soils contain less gravel, formed in alluvium, and are at higher elevations.
Reddick soils have more clay in the lower part of the solum.
Selma soils contain less gravel in the lower part of the solum. Westland soils have argillic horizons. Free soils are on terraces. The slope gradient is 0 to 2 percent. Free soils formed in loamy and gravelly outwash.