Amostown and Pollux soils are underlain by stratified very fine sand or silt within a depth of 40 inches. Bernardston soils have more than 50 percent silt plus very fine sand throughout. Broadbrook and Paxton soils lack a loamy fine sand or coarser layer in the substratum. In addition, Broadbrook soils have a lithological discontinuity and a solum with more than 65 percent silt plus very fine sand. Nantucket soils lack a loamy fine sand or coarser layer in the substratum and have a stickness class of slightly sticky or moderately sticky in the substratum.
Scituate soils have redoximorphic features in the subsoil.
Wethersfield soils have 5YR or redder hue in the subsoil and substratum. No information is available at this time to differentiate the Mt. Zion series from Montauk. Montauk soils are on glaciated uplands and moraines. Slopes range form 0 to 35 percent. The landscape in some areas has many closed depressions, some of which are filled by perennial ponds or wet spots.