Fine-earth texture is silt loam, loam, or very fine sandy loam. It is firm or very firm. Amostown soils are underlain by stratified very fine sand or silt within a depth of 40 inches. Broadbrook soils have a lithologic discontinuity at the top of the substratum. Horseneck soils do not have dense materials in the substratum.
Scituate soils have sandy substrata.
Nantucket soils have a lithologic discontinuity and formed in till mixed with Pleistocene Age silts and clays. Paxton soils have less than 65 percent silt plus very fine sand in the solum. Wethersfield soils have hues of 2.5YR or 5YR in the B horizon. Bernardston soils are nearly level to very steep and are on glaciated uplands and drumlins. Slope is commonly 8 to 25 percent, but ranges from 0 to 50 percent.