Major Land Resource Area 144A
New England and Eastern New York Upland, Southern Part
Accessed: 10/07/2024
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Ecological site list
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material Alluvium; landform a floodplain
- Soils excessively drained to well drained
- Soils excessively drained – High Floodplain Levee
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i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils well drained to excessively drained
- Soils well drained
- Soils not nutrient rich; lower base saturation
- Soils moderately deep to densic contact -Well Drained Dense Till Uplands
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i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils moderately well to very poorly drained
- Soils moderately well drained
- Soils not nutrient rich; lower base saturation
- Soils deep to contact – Moist Till Uplands
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i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils moderately well to very poorly drained
- Soils poorly to very poorly drained
- Soils poorly drained
- Soils not nutrient rich; lower base saturation – Wet Till Depressions
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material Alluvium; landform a floodplain
- Soils excessively drained to well drained
- Soils well drained - Sandy High Floodplain
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material Alluvium; landform a floodplain
- Soils moderately well drained to very poorly drained
- Soils moderately well drained – Sandy Low Floodplain
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i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material Alluvium; landform a floodplain
- Soils moderately well drained to very poorly drained
- Soils poorly to very poorly drained
- Soils poorly drained
- Soil texture coarse-sandy – Wet Sandy Low Floodplain
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i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material Alluvium; landform a floodplain
- Soils moderately well drained to very poorly drained
- Soils poorly to very poorly drained
- Soils poorly drained
- Soil texture coarse-silty – Wet Silty Low Floodplain
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material Alluvium; landform a floodplain
- Soils moderately well drained to very poorly drained
- Soils poorly to very poorly drained
- Soils very poorly drained – Very Wet Low Floodplain F144AY016MA
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated lakewater deposits (glaciolacustrine)
- Soils well drained – Well Drained Lake Plain
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated lakewater deposits (glaciolacustrine)
- Soils moderately well drained to very poorly drained
- Soils moderately well drained and somewhat poorly drained – Moist Lake Plain
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated lakewater deposits (glaciolacustrine)
- Soils moderately well drained to very poorly drained
- Soils poorly or very poorly drained
- Soils poorly drained – Wet Lake Plain
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated lakewater deposits (glaciolacustrine)
- Soils moderately well drained to very poorly drained
- Soils poorly or very poorly drained
- Soils very poorly drained – Very Wet Coastal Lake Plain
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i
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 moderately acid to moderately alkaline
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils well-drained to excessively well drained
- Soils somewhat excessively drained to excessively drained
- Soils nutrient rich; higher base saturation - Semi-rich Dry Outwash
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils well-drained to excessively well drained
- Soils somewhat excessively drained to excessively drained
- Soils not nutrient rich; lower base saturation – Dry Outwash
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils well-drained to excessively well drained
- Soils well drained
- Soils not nutrient rich; lower base saturation
- Soils without eolian mantle (loess) – Well Drained Outwash
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i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils well-drained to excessively well drained
- Soils well drained
- Soils not nutrient rich; lower base saturation
- Soils with eolian mantle (loess) – Well Drained Eolian Outwash
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i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils well-drained to excessively well drained
- Soils well drained
- Soils nutrient rich; higher base saturation – Semi-rich Moist Outwash
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils moderately well-drained to very poorly drained
- Soils moderately well drained
- Soils nutrient rich; higher base saturation – Semi-rich Moist Outwash
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils moderately well-drained to very poorly drained
- Soils moderately well drained
- Soils not nutrient rich; lower base saturation
- Surface texture silty – Moist Silty Outwash
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils moderately well-drained to very poorly drained
- Soils moderately well drained
- Soils not nutrient rich; lower base saturation
- Surface texture sandy – Moist Sandy Outwash
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils moderately well-drained to very poorly drained
- Soils poorly to very poorly drained
- Soils poorly drained
- Soils not nutrient rich; lower base saturation – Wet Outwash
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils moderately well-drained to very poorly drained
- Soils poorly to very poorly drained
- Soils poorly drained
- Soils nutrient rich; higher base saturation – Semi-rich Wet Outwash
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils moderately well-drained to very poorly drained
- Soils poorly to very poorly drained
- Soils Very Poorly Drained
- Soils nutrient rich; higher base saturation – Semi-rich Very Wet Outwash
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated Parent material water-deposited (glaciofluvial, glaciolacustrine)
- Glaciated meltwater fluvial deposits (glaciofluvial/outwash)
- Soils moderately well-drained to very poorly drained
- Soils poorly to very poorly drained
- Soils Very Poorly Drained
- Soils not nutrient rich; lower base saturation – Very Wet Outwash
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils well drained to excessively drained
- Soils somewhat excessively to excessively drained
- Soils moderately deep or deep to bedrock – Dry Till Uplands
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils well drained to excessively drained
- Soils somewhat excessively to excessively drained
- Soils shallow (< 50cm) to bedrock – Shallow Dry Till Uplands
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils well drained to excessively drained
- Soils well drained
- Soils not nutrient rich; lower base saturation
- Soils deep to contact – Well Drained Till Uplands
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils well drained to excessively drained
- Soils well drained
- Soils nutrient rich; higher base saturation
- Soils shallow (< 50cm) to bedrock – Shallow Semi-rich Well Drained Till Uplands
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils well drained to excessively drained
- Soils well drained
- Soils nutrient rich; higher base saturation
- Soils moderately deep or deep to bedrock – Semi-rich Well Drained Till Uplands
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils moderately well to very poorly drained
- Soils moderately well drained
- Soils not nutrient rich; lower base saturation
- Soils moderately deep to densic contact – Moist Dense Till Uplands
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils moderately well to very poorly drained
- Soils moderately well drained
- Soils nutrient rich; higher base saturation – Semi-rich Moist Till Uplands
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils moderately well to very poorly drained
- Soils poorly to very poorly drained
- Soils poorly drained
- Soils nutrient rich; higher base saturation – Semi-rich Wet Till Depressions
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils moderately well to very poorly drained
- Soils poorly to very poorly drained
- Soils very poorly drained
- Soils nutrient rich; higher base saturation – Semi-rich Very Wet Till Depressions
-
i
Key Characteristics
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils without organic layer ("O" horizon) or organic layer < 40 cm (16") in thickness –Mineral Soils
- Parent material of glaciated nature; glaciolacustrine, glaciofluvial, or glacial till (not alluvium)
- Glaciated parent material ice-deposited (glacial till)
- Soils moderately well to very poorly drained
- Soils poorly to very poorly drained
- Soils very poorly drained
- Soils not nutrient rich; lower base saturation – Very Wet Till Depressions
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils with organic layer ("O" horizon) ≥ 40 cm (16") in thickness – Organic Soils
- Soils formed in freshwater environments
- Wetland mineralogy nutrient rich; euic soil reaction class – Semi-rich Organic Wetlands
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils with organic layer ("O" horizon) ≥ 40 cm (16") in thickness – Organic Soils
- Soils formed in freshwater environments
- Wetland mineralogy nutrient poor; dysic soil reaction class – Acid Organic Wetlands … F144AY043MA
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils with organic layer ("O" horizon) ≥ 40 cm (16") in thickness – Organic Soils
- Soils formed in salt/brackish environments
- Tidally flooded twice a month – Tidal High Marsh
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i
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
- Soils not permanently submerged in water
- Soils native, not anthropogenic (Not Human Altered Human Transported [HAHT]
- Soils with organic layer ("O" horizon) ≥ 40 cm (16") in thickness – Organic Soils
- Soils formed in salt/brackish environments
- Tidally flooded daily – Tidal Low Marsh
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i
Key Characteristics
- Soils permanently (>21hrs/day) submerged in water
- Soils formed in freshwater
- Soils formed in submerged mineral deposits
- Soils permanently (>21hrs/day) submerged in water - Subaqueous Soils
- Soils formed in freshwater
- Soils formed in submerged mineral deposits - Subaqueous Freshwater Mineral Deposits
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i
Key Characteristics
- Soils permanently (>21hrs/day) submerged in water
- Soils formed in freshwater
- Soils formed in submerged organic deposits
- Soils permanently (>21hrs/day) submerged in water - Subaqueous Soils
- Soils formed in freshwater
- Soils formed in submerged organic deposits - Subaqueous Freshwater Organic Deposits
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i
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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i
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)
- Soils permanently (>21hrs/day) submerged in water - Subaqueous Soils
- 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) - Subaqueous Haline Low Energy Basins
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i
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
- Soils permanently (>21hrs/day) submerged in water - Subaqueous Soils
- Soils formed in salt and/or brackish water
- Soils formed in submerged glacial deposits - Subaqueous Haline Glacial Deposits
- Soils permanently (>21hrs/day) submerged in water - Subaqueous Soils
- 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 - Subaqueous Haline Slopes
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i
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
- Soils permanently (>21hrs/day) submerged in water - Subaqueous Soils
- 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 - Subaqueous Haline Flats
Ecological site map
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Zoom in to display soil survey map units for an area of interest, and zoom out to display MLRAs. Select a map unit polygon to view ecological sites correlated to that map unit. View a brief description of an ecological site by clicking on its name in the map popup. Soil survey correlations may not be accurate, and ecological site classification of a location should always be verified in the field. Each selection may require the transfer of several hundred KB of data.
Ecological site keys
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key2. Key 2 is a strict dichotomous key w/ paired couplets. 7 HAHT PES were added as reserves to be developed in EDIT (NBarrett)
Ecological site photos
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Add ecological sites and Major Land Resource Areas to your briefcase by clicking on the briefcase () icon wherever it occurs. Drag and drop items to reorder. Cookies are used to store briefcase items between browsing sessions. Because of this, the number of items that can be added to your briefcase is limited, and briefcase items added on one device and browser cannot be accessed from another device or browser. Users who do not wish to place cookies on their devices should not use the briefcase tool. Briefcase cookies serve no other purpose than described here and are deleted whenever browsing history is cleared.
Ecological sites
Major Land Resource Areas
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.