| 
 Soil Catenas, Plymouth
County Massachusetts 
The relationships
between soils, landscapes, geology, and parent material 
 Soil 
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. 
    
        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. | 
     
 
 
  
    
        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. | 
     
 
 
  
    
        Parent 
        Material | 
        Excessively | 
        Well | 
        Moderately 
        Well | 
        Poorly | 
        Very 
        Poorly | 
     
 
 
    
        | Stratified sand and/or gravel
        deposited in glacial melt water streams. | 
     
 
 
  
    
        Parent 
        Material | 
        Excessively | 
        Well | 
        Moderately 
        Well | 
        Poorly | 
        Very 
        Poorly | 
     
 
 
    
        | Silty and clayey sediments deposited
        in glacial lakes. | 
     
 
 
  
    
        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 | 
     
 
 
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