Soil Catenas, Plymouth County Massachusetts
The relationships between soils, landscapes, geology, and parent material

A Soil Catena DiagramSoil Catena Diagram, click for larger image.

There are approximately 55 major "types" of soils mapped in Plymouth County. Each "type," or series, is named for the geographical area where it was first described. Each soil series has definite relationships to landscapes, regional geology, and parent materials. Related soils of about the same age, derived from similar parent material and occurring under similar climatic conditions, can be arranged into a sequence of increasing wetness. This sequence is called a soil catena.

Soil Drainage Class

Parent
Material
Excessively Well Moderately
Well
Poorly Very
Poorly
A. Glacial Till (Dense or Basal Till)
Unsorted, unstratified, heterogeneous mixture of sand, silt, clay and rock.
Loamy dense till - mixed igneous bedrock   Paxton
Montauk
Woodbridge
Scituate
Ridgebury
Norwell
Whitman
Brockton
Sandy mantle underlain by dense till   Poquonock Birchwood Mattapoiset Brockton
Loamy dense till - carboniferous sedimentary bedrock   Newport Pittstown    
Eolian mantle - mixed igneous bedrock   Broadbrook Rainbow   Whitman
Brockton

 

Soil Drainage Class

Parent
Material
Excessively Well Moderately
Well
Poorly Very
Poorly
B. Glacial Till (Ablation and/or Ice Contact)
Unsorted, unstratified, heterogeneous mixture of sand, silt, clay and rock.
Loose sandy till on moraines Plymouth Barnstable Newfields    
Variable ice contact deposits Gloucester Canton Newfields    

 

Soil Drainage Class

Parent
Material
Excessively Well Moderately
Well
Poorly Very
Poorly
C. Glacial Fluvial
Stratified sand and/or gravel deposited in glacial melt water streams.
Gravelly fluvial deposits Hinckley
Quonset
Merrimac Sudbury Wareham
Walpole
Scarboro
Sandy fluvial deposits Carver
Windsor
Merrimac
Deerfield Wareham
Pipestone
Saugatuck
Scarboro
Berryland
Silty eolian mantle   Haven Tisbury    

 

Soil Drainage Class

Parent
Material
Excessively Well Moderately
Well
Poorly Very
Poorly
D. Glacial Lacustrine
Silty and clayey sediments deposited in glacial lakes.
Lake floor deposits     Scio Raynham Birdsall
Deltaic sands underlain by
lake floor deposits
Wampanu-
cket
Hinesburg Eldridge Enosburg Birdsall

 

Soil Drainage Class

Parent
Material
Excessively Well Moderately
Well
Poorly Very
Poorly
E. Post Glacial (Holocene) Deposits
Holocene underlain by Pleistocene deposits.
Alluvial (floodplain) soils     Winooski Limerick Saco
Organic soils - Tidal         Matunuck
Pawcatuck
Ipswich
Organic soils - Freshwater         Swansea
Freetown
Human Altered soils   Udisamment
Udorthents
Udi & Udo
wet
Tihonet Aquents
Coastal eolian soils Hooksan   Hooksan
wet sub.
   

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