Major Land Resource Area 127X
Eastern Allegheny Plateau and Mountains
Accessed: 05/19/2025
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Ecological site list
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent material otherwise (not alluvium);
- Soil drainage: otherwise (not poorly drained, not very poorly drained);
- Frigid soil temperature regime;
- In Northern Unglaciated Allegheny Plateau - Pennsylvania and New York (cool frigid above 39°43′ N latitude) - Cold Uplands
- In Allegheny Mountains - other than Pennsylvania and New York (mostly WV)
- Soils Spodosols or of Spodic subgroup
- Soils not rubbly
- Soils a True Spodosol – Spodic Shale Upland Conifer Forest
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent material otherwise (not alluvium);
- Soil drainage: otherwise (not poorly drained, not very poorly drained);
- Frigid soil temperature regime;
- In Northern Unglaciated Allegheny Plateau - Pennsylvania and New York (cool frigid above 39°43′ N latitude) - Cold Uplands
- In Allegheny Mountains - other than Pennsylvania and New York (mostly WV)
- Soils Spodosols or of Spodic subgroup
- Soils not rubbly
- Soils of Spodic subgroup – Spodic Intergrade Shale Upland Hardwood and Conifer Forest
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent material otherwise (not alluvium);
- Soil drainage: otherwise (not poorly drained, not very poorly drained);
- Frigid soil temperature regime;
- Mesic soil temperature regime
- Soils otherwise (not colluvial)
- Soils skeletal and 100cm or less – Acid Shale Upland Oak/Heath
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent Material Alluvium;
- Flood frequency: frequent, occasional, or rare – Flood plains;
- Soil drainage: poorly-drained to VPD - Wet Alluvial Land
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent Material Alluvium;
- Flood frequency: frequent, occasional, or rare – Flood plains;
- Soil drainage: otherwise (not poorly-drained to VPD) - Alluvial Land
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent Material Alluvium;
- Flood frequency: none - Terraces
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent material otherwise (not alluvium);
- Soil drainage: poorly drained, very poorly drained - Wet Uplands
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i
Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent material otherwise (not alluvium);
- Soil drainage: otherwise (not poorly drained, not very poorly drained);
- Frigid soil temperature regime;
- In Northern Unglaciated Allegheny Plateau - Pennsylvania and New York (cool frigid above 39°43′ N latitude) - Cold Uplands
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i
Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent material otherwise (not alluvium);
- Soil drainage: otherwise (not poorly drained, not very poorly drained);
- Frigid soil temperature regime;
- In Northern Unglaciated Allegheny Plateau - Pennsylvania and New York (cool frigid above 39°43′ N latitude) - Cold Uplands
- In Allegheny Mountains - other than Pennsylvania and New York (mostly WV)
- if otherwise - Frigid High Elevation Uplands
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent material otherwise (not alluvium);
- Soil drainage: otherwise (not poorly drained, not very poorly drained);
- Frigid soil temperature regime;
- Mesic soil temperature regime
- Soils colluvial - Convergent Uplands
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent material otherwise (not alluvium);
- Soil drainage: otherwise (not poorly drained, not very poorly drained);
- Frigid soil temperature regime;
- Mesic soil temperature regime
- Soils otherwise (not colluvial)
- Soils not skeletal or > 100cm deep Divergent Uplands
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Key Characteristics
- Soils not Human Altered Transported Materials (HAHT) or Mine Spoils;
- Parent material otherwise (not alluvium);
- Soil drainage: otherwise (not poorly drained, not very poorly drained);
- Frigid soil temperature regime;
- In Northern Unglaciated Allegheny Plateau - Pennsylvania and New York (cool frigid above 39°43′ N latitude) - Cold Uplands
- In Allegheny Mountains - other than Pennsylvania and New York (mostly WV)
- Soils Spodosols or of Spodic subgroup
- Soils rubbly – Rubbly Upland Conifer Forest
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Key Characteristics
- Human Transported Materials (HTM) or Mine Spoils
- Mine Spoil (reserved)… Mine Spoil
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