Major Land Resource Area 078B
Central Rolling Red Plains, Western Part
Accessed: 11/21/2024
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1
Select an ecological site
Select an ecological site using the list, keys, photos, briefcase, or quick search option located on this page. -
2
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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i
Key Characteristics
- Floodplains
- Water table >30 inches from surface
- Clay surface texture
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i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- >40 inches to claystone
- No ponding or depressional areas
- Clay surface
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- >40 inches to claystone
- No ponding or depressional areas
- Clay loam surface CL
-
i
Key Characteristics
- Floodplains
- Water table >30 inches from surface
- Loamy surface texture
- head of drainageways, rare flooding
-
i
Key Characteristics
- Uplands
- >30% surface gravel
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- <20 inches to restrictive layer
- Over gypsum
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- >40 inches to claystone
- Soils ponded / depressional areas
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- >40 inches to claystone
- No ponding or depressional areas
- Loamy surface
- Calcareous soils
-
i
Key Characteristics
- Floodplains
- Water table >30 inches from surface
- Loamy surface texture
- Commonly flooded bottomlands
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- >40 inches to claystone
- No ponding or depressional areas
- Loamy surface
- Non-calcareous soils
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- >40 inches to claystone
- No ponding or depressional areas
- Sandy surface FS, LFS
- With argillic horizon/lamellae
- Sandy surface less than 50cm
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- >20% slopes
- Not over claystone
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- >40 inches to claystone
- No ponding or depressional areas
- Sandy surface FS, LFS
- No argillic horizon/lamellae
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- >40 inches to claystone
- No ponding or depressional areas
- Sandy surface FS, LFS
- With argillic horizon/lamellae
- Sandy surface more than 50cm
-
i
Key Characteristics
- Floodplains
- Water table >30 inches from surface
- Sandy surface texture
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- >40 inches to claystone
- No ponding or depressional areas
- Sandy loam surface FSL
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- <20 inches to restrictive layer
- Over sandstone
- >10 inches to bedrock
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- >20 inches to restrictive layer
- <40 inches to claystone
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- <20 inches to restrictive layer
- Over limestone/caliche
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- <20 inches to restrictive layer
- Over claystone
-
i
Key Characteristics
- Floodplains
- Water table <30 inches from surface
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- >20% slopes
- Over claystone
-
i
Key Characteristics
- Uplands
- <30% surface gravel
- <20% slopes
- <20 inches to restrictive layer
- Over sandstone
- <10 inches to bedrock
Ecological site map
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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.