Major Land Resource Area 108X
Illinois and Iowa Deep Loess and Drift
Accessed: 11/21/2024
Next steps
-
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
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock <1.5m (60")
- Bedrock is shale
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock <1.5m (60")
- Bedrock is sandstone
- Light surface (ochric epipedon) or dark surface <25cm (10")
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Loess (including loess over glacial till)
- Light surface (ochric epipedon) or dark surface <15cm (6")
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Outwash (including loess-capped outwash)
- Light surface (ochric epipedon) or dark surface <15cm (6")
-
i
Key Characteristics
- River Valleys
- Low stream terrace subject to rare flooding
-
i
Key Characteristics
- River Valleys
- Floodplain
- Flooded only
- Fine-silty alluvium
-
i
Key Characteristics
- River Valleys
- Floodplain
- Flooded only
- Fine-loamy to coarse-loamy alluvium
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock <1.5m (60")
- Bedrock is shale
- Light surface (ochric epipedon) or dark surface <25cm (10")
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock <1.5m (60")
- Bedrock is sandstone
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock >1.5m (60")
- Parent material is loess (>100cm thick)
- Linear to convex summits, shoulders, backslopes, and broad interfluve summits
- Light surface (ochric epipedon) or dark surface <15cm (6")
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock >1.5m (60")
- Parent material is till/paleosol/pedisediment (<100cm of loess)
- Light surface (ochric epiepdon) or dark surface <15cm (6")
-
i
Key Characteristics
- Outwash/lacustrine plains and terraces (includes dune topography)
- Outwash (including outwash with a loess cap 50-100cm)
- Linear to convex summits and backslopes
- light surface (ochric epipedon) or dark surface <25cm (10")
-
i
Key Characteristics
- Outwash/lacustrine plains and terraces (includes dune topography)
- Sandy eolian deposits
- Light surface (ochric epipedon)
-
i
Key Characteristics
- Floodplains and low terraces subject to flooding
- Water table is deeper than 30cm (12")
-
i
Key Characteristics
- Floodplains and low terraces subject to flooding
- Water table is within 30cm (12")
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Shallow (<100cm) silty or loamy sediments over bedrock
- <50cm to limestone bedrock
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Shallow (<100cm) silty or loamy sediments over bedrock
- >50cm to sandstone bedrock
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Loess
- Alfisol (or Inceptisol or Entisol)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Eolian sands (including <150cm loess over eolian sands)
- Alfisol (or Entisol with lamellic horizon)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Glacial till/paleosols/valley-fill sediments (including <50cm loess over glacial till)
- Alfisol
- Deep to water table (>30cm)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Glacial till/paleosols/valley-fill sediments (including <50cm loess over glacial till)
- Alfisol
- Shallow to water table (<30cm)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Broad Upland Flats and Depressions
- Upland flat, not ponded, loess parent material, shallow to water table (≤30cm), Somewhat Poorly to Very Poorly drained
- Alfisol
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Drainageways
- Located downslope from an Upland Woodland or Upland Forest ecological site
-
i
Key Characteristics
- River Valleys
- Valley Footslope, colluvial parent materials
-
i
Key Characteristics
- River Valleys
- Floodplains
- Flooded only
- Directly adjacent to stream chanel
- Fine, fine-silty alluvium, Poorly to Very Poorly drained
-
i
Key Characteristics
- River Valleys
- Floodplains
- Flooded only
- Directly adjacent to stream chanel
- Fine-loamy, fine-silty alluvium, Somewhat Poorly to Moderately Well drained
-
i
Key Characteristics
- River Valleys
- Floodplains
- Flooded only
- Directly adjacent to stream chanel
- Coarse-loamy alluvium, Well to Excessively drained
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction 20-40"
- <14% slope
- Sandstone residuum
-
i
Key Characteristics
- Upland (depressions, drainageways, footslopes) Loess sites
- Drainageway
- Well, Moderately Well drained
- Alfic
-
i
Key Characteristics
- Lowland (stream terrace, floodplain)
- Floodplain
- Adjacent to current/former channel
- Loamy, fine-loamy, fine-silty
-
i
Key Characteristics
- Lowland (stream terrace, floodplain)
- Floodplain
- Adjacent to current/former channel
- Sandy, coarse-loamy
-
i
Key Characteristics
- Lowland (stream terrace, floodplain)
- Floodplain
- Adjacent to current/former channel
- Flaggy Substratum
-
i
Key Characteristics
- Uplands
- Histosols
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock <1.5m (60")
- Bedrock is limestone
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock <1.5m (60")
- Bedrock is sandstone
- Dark surface (mollic epipedon) >25cm (10")
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Loess (including loess over glacial till)
- Dark surface (mollic epipedon) >25cm (10")
- Water table >30cm (12")
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Loess (including loess over glacial till)
- Dark surface (mollic epipedon) >25cm (10")
- Water table <30cm (12"), not ponded
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Loess (including loess over glacial till)
- Dark surface (mollic epipedon) >25cm (10")
- Water table <30cm (12"), ponded
- Recharge wetland, non-calcareous surface
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Loess (including loess over glacial till)
- Dark surface (mollic epipedon) >25cm (10")
- Water table <30cm (12"), ponded
- Discharge wetland, calcareous surface
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Loess (including loess over glacial till)
- Dark surface (mollic intergrade) 15-25cm (6-10")
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Outwash (including loess-capped outwash)
- Dark surface (mollic epipedon) >25cm (10")
- Water table >30cm (12")
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Outwash (including loess-capped outwash)
- Dark surface (mollic epipedon) >25cm (10")
- Water table <30cm (12")
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Outwash (including loess-capped outwash)
- Dark surface (mollic integrade) 15-25cm (6-10") --not described
-
i
Key Characteristics
- Uplands
- Mineral Soils
- Bedrock >1.5m (60")
- Eolian sands
-
i
Key Characteristics
- River Valleys
- Floodplain
- Flooded and ponded
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock <1.5m (60")
- Bedrock is limestone
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock >1.5m (60")
- Parent material is loess (>100cm thick)
- Linear to convex summits, shoulders, backslopes, and broad interfluve summits
- Dark surface (mollic epiepdon) >25cm (10")
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock >1.5m (60")
- Parent material is loess (>100cm thick)
- Linear to convex summits, shoulders, backslopes, and broad interfluve summits
- Dark surface (mollic intergrade) 15-25cm (6-10")
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock >1.5m (60")
- Parent material is loess (>100cm thick)
- Linear to concave footslopes, toeslopes, flats, and heads of drainageways
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock >1.5m (60")
- Parent material is loess (>100cm thick)
- Concave, closed depressions
-
i
Key Characteristics
- Uplands (bluffs, ground moraines, hills)
- Bedrock >1.5m (60")
- Parent material is till/paleosol/pedisediment (<100cm of loess)
- Dark surface (mollic epipedon) >25cm (10")
-
i
Key Characteristics
- Outwash/lacustrine plains and terraces (includes dune topography)
- Outwash (including outwash with a loess cap 50-100cm)
- Linear to convex summits and backslopes
- Dark surface (mollic epipedon) >25cm (10")
-
i
Key Characteristics
- Outwash/lacustrine plains and terraces (includes dune topography)
- Outwash (including outwash with a loess cap 50-100cm)
- Linear to concave footslopes, toeslopes, and heads of drainageways
-
i
Key Characteristics
- Outwash/lacustrine plains and terraces (includes dune topography)
- Sandy eolian deposits
- Dark surface (mollic epipedon) >25cm (10")
-
i
Key Characteristics
- Outwash/lacustrine plains and terraces (includes dune topography)
- Linear to concave lacustrine deposits, fine textured
-
i
Key Characteristics
- Outwash/lacustrine plains and terraces (includes dune topography)
- Concave to linear organic depostis
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Loess
- Mollisol (or Inceptisol with mollic epipedon)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Loess
- Mollic subgroup of an Alifisol
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Eolian sands (including <150cm loess over eolian sands)
- Mollisol
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Eolian sands (including <150cm loess over eolian sands)
- Mollic subgroup of an Alfisol
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Glacial till/paleosols/valley-fill sediments (including <50cm loess over glacial till)
- Mollisol
- Deep to water table (>30cm)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Glacial till/paleosols/valley-fill sediments (including <50cm loess over glacial till)
- Mollisol
- Shallow to water table (<30 cm)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Glacial till/paleosols/valley-fill sediments (including <50cm loess over glacial till)
- Mollic subgroup of an Alfisol (or contains mollic surface horizon 15-25cm thick)
- Deep to water table (>30cm)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Summits, Shoulders, and Backslopes
- Glacial till/paleosols/valley-fill sediments (including <50cm loess over glacial till)
- Mollic subgroup of an Alfisol (or contains mollic surface horizon 15-25cm thick)
- Shallow to water table (<30cm)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Broad Upland Flats and Depressions
- Depressions, ponded
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Broad Upland Flats and Depressions
- Upland flat, not ponded, loess parent material, shallow to water table (≤30cm), Somewhat Poorly to Very Poorly drained
- Mollisol
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Broad Upland Flats and Depressions
- Upland flat, not ponded, loess parent material, shallow to water table (≤30cm), Somewhat Poorly to Very Poorly drained
- Mollic subgroup of an Alfisol (or contains mollic surface horizon 15-25cm thick)
-
i
Key Characteristics
- Uplands and High Stream Terraces
- Drainageways
- Located downslope from an Upland Prairie or Upland Savanna ecological site
-
i
Key Characteristics
- River Valleys
- Low Stream Terraces
- Deep to water table (>30cm), Moderately Well to Somewhat Excessively drained
-
i
Key Characteristics
- River Valleys
- Low Stream Terraces
- Shallow to water table (<30cm), Somewhat Poorly to Poorly drained
-
i
Key Characteristics
- River Valleys
- Floodplains
- Flooded and ponded
- Organic soils (histic epipedon ≥20cm)
-
i
Key Characteristics
- River Valleys
- Floodplains
- Flooded and ponded
- Mineral soils
-
i
Key Characteristics
- River Valleys
- Floodplains
- Flooded only
- Not directly adjacent to stream channel
- Deep to water table (>30cm)
-
i
Key Characteristics
- River Valleys
- Floodplains
- Flooded only
- Not directly adjacent to stream channel
- Shallow to water table (<30cm)
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction 20-40"
- >14% slope
- Sandstone residuum
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction 20-40"
- <14% slope
- Limestone residuum
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction <20"
- Limestone residuum
-
i
Key Characteristics
- Upland (depressions, drainageways, footslopes) Loess sites
- Drainageway
- Well, Moderately Well drained
- Mollisol or Mollic intergrade
-
i
Key Characteristics
- Upland (depressions, drainageways, footslopes) Loess sites
- Drainageway
- Somewhat Poorly, Poorly Drained
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction >40"
- Little or no Loess
- >14% slope
- Till/Paleosol, >10" to carbonates and Mollisol or Mollic Integrade
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction 20-40"
- >14% slope
- Shale residuum
-
i
Key Characteristics
- Upland (depressions, drainageways, footslopes) Loess sites
- Footslope
- Mollisol or Mollic intergrade
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction 20-40"
- <14% slope
- Shale residuum
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction >40"
- Loess >12"
- <14% slope and Mollisol or Mollic intergrade
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction >40"
- Little or no Loess
- <14% slope
- Eolian Sands and Mollisol or Mollic intergrade
-
i
Key Characteristics
- Upland (summit, shoulder, backslope)
- Root Restriction >40"
- Little or no Loess
- <14% slope
- Till/Paleosol and Mollisol
-
i
Key Characteristics
- Upland (depressions, drainageways, footslopes) Loess sites
- Depression
-
i
Key Characteristics
- Lowland (stream terrace, floodplain)
- Floodplain
- Not adjacent to current/former channel
- Far from channel
-
i
Key Characteristics
- Lowland (stream terrace, floodplain)
- Low Terrace
- Somewhat Poorly, Poorly drained, Mollisol or Mollic intergrade
-
i
Key Characteristics
- Lowland (stream terrace, floodplain)
- High Terrace
- Loess
- Well, Moderately Well, Somewhat Poorly drained, Mollisol or Mollic intergrade
-
i
Key Characteristics
- Lowland (stream terrace, floodplain)
- Low Terrace
- Moderately Well, Well drained
-
i
Key Characteristics
- Lowland (stream terrace, floodplain)
- High Terrace
- Sand
-
i
Key Characteristics
- Lowland (stream terrace, floodplain)
- High Terrace
- Loess
- Poorly drained
Ecological site map
Basemap
Find me
Find point
Full screen
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
Ecological site photos
Print Options
Sections
Font
Other
Briefcase
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.