PLYMOUTH COUNTY, MASSACHUSETTS SOIL SURVEY UPDATE
Plymouth Soils: Very deep, excessively drained soil formed in ice contact glacial outwash or loose sandy till. Plymouth soils are on undulating outwash plains, moraines, heads of outwash, and on low lying hills within areas of glacial lake deposits and ground moraine.
Link
to Official Series Description
Plymouth Pedon Description 2343801
Plymouth Pedon Description 2343501
Plymouth Pedon Description 2347805
Map
Unit (s): 435A,B,C,E, 436B,C,E, 437B,C,E, 438B,C,E.
Map
Phases:
Taxonomic
Classification: Mesic, coated Typic Quartzipsamments
Drainage
Class: Excessively drained.
Parent
Material: Mixed loose sandy till and ice contact outwash.
Permeability:
Rapid in the solum and rapid to very rapid in the substratum.
Available
Water Holding Capacity: Low.
Soil
Reaction: Extremely acid through strongly acid throughout
Depth
to Bedrock: Greater than 65 inches.
Seasonal
High Watertable: Greater than 6 feet.
Hydrologic
Group: A.
Hydric
Soil: No.
Flooding/Ponding
Potential: Frequency and Type: None
Duration and Months: None
Potential
Inclusions: Excessively drained Gloucester and Carver soils
are similar inclusions. Well drained Barnstable, Merrimac and
Canton soils are on concave and level slopes. Moderately well
drained Sudbury and Newfields soils are on lower elevations.
Soil Suitability:
Agriculture: Poorly suited for most agricultural uses due to droughtyness and low fertility, irrigation is needed for optimal yields.
Woodland: Poorly suited to woodland productivity due to droughtyness.
Development: Well suited for development, major limitations related large stones and boulders which may hinder small excavation equipment.