PLYMOUTH COUNTY, MASSACHUSETTS SOIL SURVEY UPDATE
Paxton Soils: Very deep, well drained soil formed in sandy loam eolian mantled material underlain by compact (lodgement) glacial till derived mostly from schist, gneiss and granite. Paxton soils are on smooth convex side slopes and top slopes of glaciated hills and drumlins.
Link
to Official Series Description
Paxton Pedon Description
2330601 |
Paxton Pedon Description 2330602 |
Paxton Pedon Description 2330501
Map
Unit (s): 305B, 305C, 305D, 306B, 306C, 306D
Map
Phases:
Taxonomic
Classification: Coarse - loamy, mixed, nonacid, Oxyaquic
Dystrochrepts.
Drainage
Class: Well drained.
Parent
Material: Dense glacial till.
Permeability:
Moderate in the solum, slow or very slow in the dense substratum.
Available
Water Holding Capacity: Moderate.
Soil
Reaction: Very strongly acid to moderately acid throughout.
Depth
to Bedrock: Greater than 65 inches.
Seasonal
High Watertable: Depth: 2.5 to 4 feet.
Type: Perched.
Months: January to May.
Hydrologic
Group: C.
Hydric
Soil: No.
Flooding/Ponding
Potential: Frequency and Type: None.
Potential
Inclusions: Poquonock and Montauk soils are similar
inclusions. Poorly drained Norwell, and Ridgebury soils are along
drainageways. Moderately well drained Scituate, Birchwood, and
Woodbridge soils are on concave slopes.
Soil Suitability:
Agriculture: Map unit 305B is a prime farmland soil. Map units 305C, 306C and 306B are important farmland soils.
Woodland: Well suited for woodland.
Development: Major limitations related to slow permeability in the dense till substratum. Large surface and subsurface stones and boulders may interfere with excavation. Erosion hazards are likely during development, measures should be taken to prevent erosion.