Major Land Resource Area 144A
New England and Eastern New York Upland, Southern Part
Accessed: 03/23/2023
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Select an ecological site
Select an ecological site using the list, keys, photos, briefcase, or quick search option located on this page. -
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Explore the ecological site description
Next, learn more about the selected ecological site and its characteristic dynamics by browsing the ecological site description and exploring alternative state and transition model formats.
Ecological site list
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Key Characteristics
- Soils not permanently submerged in water
- Soils without organic layer ("O" horizon) or organic layer < 16" in thickness
- Parent material alluvium; landform a floodplain
- Soils execessively drained
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Key Characteristics
- Soils not permanently submerged in water
- Soils without organic layer ("O" horizon) or organic layer < 16" in thickness
- Parent material alluvium; landform a floodplain
- Soils well, moderately well, somewhat poorly, poorly or very poorly drained
- Soils not hydric; drainage class well, moderately well
- Soils well drained
- Soil texture coarse-loamy
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Key Characteristics
- Soils not permanently submerged in water
- Soils without organic layer ("O" horizon) or organic layer < 16" in thickness
- Parent material alluvium; landform a floodplain
- Soils well, moderately well, somewhat poorly, poorly or very poorly drained
- Soils not hydric; drainage class well, moderately well
- Soils moderately well drained
- Soil texture coarse-loamy
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Key Characteristics
- Soils not permanently submerged in water
- Soils without organic layer ("O" horizon) or organic layer < 16" in thickness
- Parent material alluvium; landform a floodplain
- Soils well, moderately well, somewhat poorly, poorly or very poorly drained
- Soils hydric; drainage class somewhat poorly, poorly or very poorly drained
- Soils very poorly drained
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Key Characteristics
- Soils not permanently submerged in water
- Soils without organic layer ("O" horizon) or organic layer < 16" in thickness
- Parent material glacial till, glaciofluvial, or glaciolacustrine; landform not a floodplain
- Parent material glaciolacustrine
- Soils well drained
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Key Characteristics
- Soils not permanently submerged in water
- Soils without organic layer ("O" horizon) or organic layer < 16" in thickness
- Parent material glacial till, glaciofluvial, or glaciolacustrine; landform not a floodplain
- Parent material glaciolacustrine
- Soils moderately well, somewhat poorly, poorly or very poorly drained.
- Soils moderately well and somewhat poorly drained
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Key Characteristics
- Soils not permanently submerged in water
- Soils without organic layer ("O" horizon) or organic layer < 16" in thickness
- Parent material glacial till, glaciofluvial, or glaciolacustrine; landform not a floodplain
- Parent material glaciolacustrine
- Soils moderately well, somewhat poorly, poorly or very poorly drained.
- Soils poorly or very poorly drained
- Soils poorly drained
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Key Characteristics
- Soils not permanently submerged in water
- Soils without organic layer ("O" horizon) or organic layer < 16" in thickness
- Parent material glacial till, glaciofluvial, or glaciolacustrine; landform not a floodplain
- Parent material glaciolacustrine
- Soils moderately well, somewhat poorly, poorly or very poorly drained.
- Soils poorly or very poorly drained
- Soils very poorly drained
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Key Characteristics
- Soils not permanently submerged in water
- Soils without organic layer ("O" horizon) or organic layer < 16" in thickness
- Parent material glacial till, glaciofluvial, or glaciolacustrine; landform not a floodplain
- Parent material glacial till or glaciofluvial
- Soils extremely to moderately acid
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Key Characteristics
- Soils not permanently submerged in water
- Soils with organic layer ("O" horizon) ≥ 16" in thickness
- Soils formed in freshwater environments
- Wetland mineralogy nutrient rich; Euic soil reaction class
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Key Characteristics
- Soils not permanently submerged in water
- Soils with organic layer ("O" horizon) ≥ 16" in thickness
- Soils formed in freshwater environments
- Wetland mineralogy nutrient poor; Dysic soil reaction class
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Key Characteristics
- Soils not permanently submerged in water
- Soils with organic layer ("O" horizon) ≥ 16" in thickness
- Soils formed in salt/brackish environments
- Tidally flooded daily
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Key Characteristics
- Soils not permanently submerged in water
- Soils with organic layer ("O" horizon) ≥ 16" in thickness
- Soils formed in salt/brackish environments
- Tidally flooded twice a month
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Key Characteristics
- Soils permanently (>21hrs/day) submerged in water
- Soils formed in freshwater
- Soils formed in submerged mineral deposits
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Key Characteristics
- Soils permanently (>21hrs/day) submerged in water
- Soils formed in freshwater
- Soils formed in submerged organic deposits
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Key Characteristics
- Soils permanently (>21hrs/day) submerged in water
- Soils formed in salt and/or brackish water
- Soils formed in submerged glacial deposits
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Key Characteristics
- Soils permanently (>21hrs/day) submerged in water
- Soils formed in salt and/or brackish water
- Soils formed in marine or estuarine deposits
- Soils formed in low energy environments (lagoon & bay bottoms, stream valleys, coves)
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Key Characteristics
- Soils permanently (>21hrs/day) submerged in water
- Soils formed in salt and/or brackish water
- Soils formed in marine or estuarine deposits
- Soils formed in high energy environments
- Landform a washover fan slope
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Key Characteristics
- Soils permanently (>21hrs/day) submerged in water
- Soils formed in salt and/or brackish water
- Soils formed in marine or estuarine deposits
- Soils formed in high energy environments
- Landform a washover fan flat or flood tidal delta flat
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The Ecosystem Dynamics Interpretive Tool is an information system framework developed by the USDA-ARS Jornada Experimental Range, USDA Natural Resources Conservation Service, and New Mexico State University.