The well drained Charlton and the poorly drained Leicester soils are associated in a drainage sequence. Broadbrook, Essex, Montauk, and Paxton soils are well drained and have a dense substratum. 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.