PLYMOUTH COUNTY, MASSACHUSETTS SOIL SURVEY UPDATE
Canton Soils: This very deep, nearly level, well drained soil formed in a loamy mantle underlain by sandy, loose-to-firm ablation till. Canton soils are on slopes of uplands, ground moraines, ice contact deposits, and adjacent to plains and stream terraces.
Link
to Official Series Description
Canton Profile Description 2342401 |
2342102
Map
Unit (s): 420A, 420B, 420C, 421B, 421C, 424B, 424C
Map
Phases:
Taxonomic
Classification: Coarse - loamy over sandy or sandy skeletal,
mixed, mesic, Typic Dystrochrepts.
Drainage
Class: Well drained.
Parent
Material: Ablation till and ice-contact deposits.
Permeability:
Moderately rapid in the solum, moderately rapid to moderately
slow in the substratum.
Available
Water Holding Capacity: Moderate.
Soil
Reaction: Very strongly to moderately acid throughout. .
Depth
to Bedrock: Greater than 65 inches.
Seasonal
High Watertable: Depth: greater than 5 feet below the
surface.
Hydrologic
Group: B.
Hydric
Soil: No.
Flooding/Ponding
Potential: Frequency and Type: None.
Potential
Inclusions: Well drained Barnstable and Montauk soils are
similar inclusions. . Moderately well drained Newfields, Scituate,
and Birchwood soils are on lower elevations and concave slopes.
Poorly drained Norwell, Mattapoisett, and Ridgebury soils are in
depressions and along drainageways. Canton soils are mapped on
ice contact landforms which often consists of very variable
glacial deposits.
Soil Suitability:
Agriculture: Map unit 420A and 420B are prime farmland soil. Map units 420C, 421C and 421B are important farmland soils.
Woodland: Well suited for woodland.
Development: There are no major limitations associated with Canton soils. Large surface and subsurface stones and boulders may hinder excavation. Erosion may be a problem during disturbance. Canton soils are mapped in ice contact areas which generally consists of variable deposits. These areas may have a slowly permeable layer that may result in slow percolation rates for on-site sewage disposal systems.