Brookfield, Canton, Gloucester, and Narragansett soils are well drained and do not have redoximorphic features. Chatfield and Hollis soils have bedrock within a depth of 10 to 20 and 20 to 40 inches respectively. Ridgebury and Whitman soils are poorly drained and very poorly drained, respectively and have a dense substratum. Scituate soils are moderately well drained with a dense substratum. Moderately well drained.
Surface runoff is slow to medium.
Permeability is moderate or moderately rapid throughout. Sutton soils have a seasonal high water table. Cleared areas are used for cultivated crops, hay, or pasture. Scattered areas are used for community development. Some areas are wooded.