Major Land Resource Area 130B
Southern Blue Ridge
Accessed: 03/16/2025
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Viewing 13 of 13
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Key Characteristics
- Soil temperature regime is Frigid
- Parent material not transported material (weathered in-place) Residuum
- Soils otherwise (not of poorly drained, very deep, organic materials, and at higher elevations)
- Soils otherwise (not shallow) Frigid Residuum
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Key Characteristics
- Soil temperature regime is Frigid
- Parent material transported material - downslope by gravity/slopewash - Colluvium FrigidColluvium
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Key Characteristics
- Soil Temperature regime is Mesic
- Parent material not transported material (weathered in-place) Residuum
- Soils otherwise (not have redder subsoils with higher clays on gentle slopes)
- Soils otherwise (not shallow)
- Soils predominately with a north to east (protected) aspect Mesic Residuum Cool Aspect
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Key Characteristics
- Soil Temperature regime is Mesic
- Parent material not transported material (weathered in-place) Residuum
- Soils otherwise (not have redder subsoils with higher clays on gentle slopes)
- Soils otherwise (not shallow)
- Soils predominately with a south to west (exposed) aspect Mesic Residuum Warm Aspect
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i
Key Characteristics
- Soil Temperature regime is Mesic
- Parent material transported (not weathered in-place)
- Parent material transported material – not active alluvial floodplains
- Parent material transported material - downslope by gravity/slopewash on backslopes – backslope Colluvium
- Soils predominately with a north to east (protected) aspect Mesic Colluvium Cool Aspect
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i
Key Characteristics
- Soil Temperature regime is Mesic
- Parent material transported (not weathered in-place)
- Parent material transported material – not active alluvial floodplains
- Parent material transported material - downslope by gravity/slopewash on backslopes – backslope Colluvium
- Soils predominately with a south to west (exposed) aspect Mesic Colluvium Warm Aspect
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Key Characteristics
- Soil Temperature regime is Mesic
- Parent material not transported material (weathered in-place) Residuum
- Soils that tend to have redder subsoils with higher clays on gentle slopes Low Mountain Mesic Residuum
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i
Key Characteristics
- Soil Temperature regime is Mesic
- Parent material not transported material (weathered in-place) Residuum
- Soils otherwise (not have redder subsoils with higher clays on gentle slopes)
- Soils shallow <50 cm to restriction Shallow mesic Residuum
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i
Key Characteristics
- Soil temperature regime is Frigid
- Parent material not transported material (weathered in-place) Residuum
- Soils otherwise (not of poorly drained, very deep, organic materials, and at higher elevations)
- Soils shallow <50 cm to restriction Shallow Frigid Residuum
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i
Key Characteristics
- Soil Temperature regime is Mesic
- Parent material transported (not weathered in-place)
- Parent material transported material – not active alluvial floodplains
- Parent material transported material – relict floodplains terraces or other flatland Terraces
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i
Key Characteristics
- Soil Temperature regime is Mesic
- Parent material transported (not weathered in-place)
- Parent material transported material extensively by recent floodwaters and actively flooded by drainages, streams and rivers – Alluvial Floodplains
- Floodplain soils hydric – poorly drained to very poorly drained Hydric Floodplain
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i
Key Characteristics
- Soil Temperature regime is Mesic
- Parent material transported (not weathered in-place)
- Parent material transported material extensively by recent floodwaters and actively flooded by drainages, streams and rivers – Alluvial Floodplains
- Floodplain soils not hydric – somewhat poorly drained or less Non-hydric Floodplain
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Key Characteristics
- Soil temperature regime is Frigid
- Parent material not transported material (weathered in-place) Residuum
- Soils formed strictly of poorly drained, very deep, organic materials, and at higher elevations Frigid Mountain Bog
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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
MLRA130B PES Key
1a.
Soil temperature regime is Frigid
2a.
Parent material not transported material (weathered in-place) Residuum
3a.
Soils formed strictly of poorly drained, very deep, organic materials, and at higher elevations Frigid Mountain Bog
... F130BY013WV – Frigid Mountain Bog
3b.
Soils otherwise (not of poorly drained, very deep, organic materials, and at higher elevations)
4a.
Soils shallow <50 cm to restriction Shallow Frigid Residuum
... F130BY009WV – Shallow Frigid Residuum
2b.
Parent material transported material - downslope by gravity/slopewash - Colluvium FrigidColluvium
... F130BY002WV – Frigid Colluvium
1b.
Soil Temperature regime is Mesic
5a.
Parent material not transported material (weathered in-place) Residuum
6a.
Soils that tend to have redder subsoils with higher clays on gentle slopes Low Mountain Mesic Residuum
... F130BY007WV – Low Mountain Mesic Residuum
6b.
Soils otherwise (not have redder subsoils with higher clays on gentle slopes)
7a.
Soils shallow <50 cm to restriction Shallow mesic Residuum
... F130BY008WV – Shallow Mesic Residuum
7b.
Soils otherwise (not shallow)
8a.
Soils predominately with a north to east (protected) aspect Mesic Residuum Cool Aspect
... F130BY003WV – Mesic Residuum Cool Aspect
8b.
Soils predominately with a south to west (exposed) aspect Mesic Residuum Warm Aspect
... F130BY004WV – Mesic Residuum Warm Aspect
5b.
Parent material transported (not weathered in-place)
9a.
Parent material transported material extensively by recent floodwaters and actively flooded by drainages, streams and rivers – Alluvial Floodplains
10a.
Floodplain soils not hydric – somewhat poorly drained or less Non-hydric Floodplain
... F130BY012WV – Non-Hydric Floodplains
10b.
Floodplain soils hydric – poorly drained to very poorly drained Hydric Floodplain
... F130BY011WV – Hydric Floodplains
9b.
Parent material transported material – not active alluvial floodplains
11a.
Parent material transported material - downslope by gravity/slopewash on backslopes – backslope Colluvium
12a.
Soils predominately with a north to east (protected) aspect Mesic Colluvium Cool Aspect
... F130BY005WV – Mesic Colluvium Cool Aspect
12b.
Soils predominately with a south to west (exposed) aspect Mesic Colluvium Warm Aspect
... F130BY006WV – Mesic Colluvium Warm Aspect
11a.
Parent material transported material – relict floodplains terraces or other flatland Terraces
... F130BY010WV – Terraces
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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.
