PLYMOUTH COUNTY, MASSACHUSETTS SOIL SURVEY UPDATE
Scituate Soils: Very deep, moderately well drained soil formed in glacial till. Scituate soils are on summits, topslopes and depressions of drumlins and ground moraines.
Link
to Official Series Description
Water table Data for a Scituate Soil (Brant island)
| Water table Data for a Scituate Soil (Hiller
Field) | Water table Data for a Scituate Soil
(Marion) | Water table Data for a Scituate Soil
(Marsfield) | Water Table Data - Lakeville
Well Site |
Scituate Pedon Description 2331601 |
Scituate Pedon Description 2331602 |
Scituate Pedon Description 2331504
Map
Unit (s): 315A, 315B, 315C, 316A, 316B, 316C
Map
Phases:
Taxonomic
Classification: Coarse-loamy, mixed, mesic, Oxyaquic
Dystrochrepts.
Drainage
Class: Moderately well drained.
Parent
Material: Dense glacial till.
Permeability:
Moderate in the solum, slow in the dense substratum.
Available
Water Holding Capacity: Moderate.
Soil
Reaction: Extremely to moderately acid in the solum, strongly
to moderately acid in the substratum.
Depth
to Bedrock: Greater than 65 inches.
Seasonal
High Watertable: Depth: 1.5 to 3 feet. Type:
Perched. Months: November to May.
Hydrologic
Group: C.
Hydric
Soil: No (may have hydric inclusions).
Flooding/Ponding
Potential: Frequency and Type: None.
Potential
Inclusions: Woodbridge, Birchwood, and Newfields soils are
similar inclusions. Poorly drained Norwell, Ridgebury, and
Mattapoisett soils are along drainageways. Well drained Paxton,
Poquonock and Montauk soils are on higher elevations.
Soil Suitability:
Agriculture: Map units 315A and 315B are prime farmland soils. Map units 315C, 316C and 316B are important farmland soils.
Woodland: Well suited for woodland.
Development: Major limitations related to slow permeability in the dense till substratum and seasonal high watertables. Large surface and subsurface stones and boulders may interfere with excavation. Erosion hazards are likely during development, measures should be taken to prevent erosion.