Major Land Resource Area 039X
Mogollon Transition North
Accessed: 11/21/2024
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Explore the ecological site description
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Ecological site list
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ProvisionalF039XA001NM/F039XA001NMPseudotsuga menziesii-Populus tremuloides/Quercus gambelii-Robinia neomexicana
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ProvisionalF039XA002NM/F039XA002NMPinus ponderosa-Pseudotsuga menziesii/Quercus gambelii-Cercocarpus montanus
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ProvisionalF039XA003NM/F039XA003NMPinus edulis-Juniperus scopulorum/Quercus gambelii/Bouteloua gracilis
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ProvisionalF039XA004NM/F039XA004NMPinus ponderosa-Juniperus deppeana/Quercus gambelii/Festuca arizonica
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Key Characteristics
- 17” to 22” p.z.
- Forestland
- Slopes generally less than or equal to 15%
- Soils Moderately Deep or Deeper
- Soil surface loam. Subsurface clay loam, clay and/or sandy clay loam. Soil non-effervescent throughout the profile
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Key Characteristics
- 17” to 22” p.z.
- Forestland
- Slopes generally less than or equal to 15%
- Soils Moderately Deep or Deeper
- Soil surface loam, generally gravelly or very gravelly. Subsurface loam, clay loam, and/or clay, often gravelly. Soil surface littered with cinders
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Key Characteristics
- 17” to 22” p.z.
- Forestland
- Slopes generally less than or equal to 15%
- Soils Shallow or Very Shallow
- Soil surface stony loam to very cobbly loam. Subsurface cobbly clay loam to very cobbly clay. Soil is shallow to basalt bedrock
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Key Characteristics
- 17” to 22” p.z.
- Forestland
- Slopes generally less than or equal to 15%
- Soils Shallow or Very Shallow
- Soil surface very flaggy loam. Subsurface very flaggy loam. Soil is shallow to limestone bedrock and is slightly effervescent throughout
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Key Characteristics
- 17” to 22” p.z.
- Forestland
- Slopes generally greater than 15%. Soils Shallow or Very Shallow. Soil surface very stony loam. Subsurface clay loam and/or clay, generally cobbly. Soil is non-effervescent and shallow to basalt bedrock
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Uplands (does not receive additional run-in moisture)
- Slopes generally equal to or less than 15 percent
- Soils moderately deep and deep
- Soil surface silt loam to gravelly clay loam, two to three inches thick. Subsurface stony clay to clay
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Uplands (does not receive additional run-in moisture)
- Slopes generally equal to or less than 15 percent
- Soils moderately deep and deep
- Soil surface gravelly loam, cobbly loam, or gravelly silt loam, 4 to 10 inches thick. Subsurface gravelly clay loam to cobbly clay loam
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Uplands (does not receive additional run-in moisture)
- Slopes generally equal to or less than 15 percent
- Soils very shallow or shallow. Soil surface fine sandy loam, cobbly sandy loam, cobbly loam, sandy loam, or loam, about five inches thick. Subsurface loam, sandy clay loam, and/or clay loam with greater than 50 percent rock fragments. Soil is shallow to hard tuff
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Uplands (does not receive additional run-in moisture)
- Slopes generally equal to or less than 15 percent
- Soils moderately deep and deep
- Soil surface stony clay loam, cobbly silt loam, or cobbly clay loam, 2 to 5 inches thick
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Occurs in a bottom position (receives run-in moisture from surrounding ecological sites) and/or is Subirrigated
- Flooded at least rarely
- Soil surface sandy loam to clay loam, 2 to 15 inches thick. Subsurface fine sandy loam to clay
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Occurs in a bottom position (receives run-in moisture from surrounding ecological sites) and/or is Subirrigated
- Flooded at least rarely
- Soil surface clay, about 3 inches thick. Subsurface clay, silty clay and/or silt loam
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Occurs in a bottom position (receives run-in moisture from surrounding ecological sites) and/or is Subirrigated
- Flooded at least rarely
- Soil surface loam, about 3 inches thick. Subsurface clay loam, clay, and/or sandy clay, generally gravelly or very gravelly
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Occurs in a bottom position (receives run-in moisture from surrounding ecological sites) and/or is Subirrigated
- Soil Subirrigated
- Soil surface loam. Subsurface loam and/or clay loam, generally very stony or extremely stony. A water table is found at 0 to 5 inches from the soil surface
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Occurs in a bottom position (receives run-in moisture from surrounding ecological sites) and/or is Subirrigated
- Soil Subirrigated
- Soil surface cobbly loam. Subsurface clay loam, generally very cobbly or extremely cobbly
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Key Characteristics
- 17” to 22” p.z.
- Rangeland
- Uplands (does not receive additional run-in moisture)
- Slopes generally equal to or less than 15 percent
- Soils moderately deep and deep
- Soil surface is loam, generally gravelly, cobbly, or very stony. Subsurface is clay loam, clay and/or loam, generally gravelly, very gravelly, and/or cobbly
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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.