

Natural Resources
Conservation Service
Ecological site R105XY018WI
Dry Mollic or Umbric Upland
Last updated: 2/23/2024
Accessed: 04/25/2025
General information
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
MLRA notes
Major Land Resource Area (MLRA): 105X–Upper Mississippi River Bedrock Controlled Uplands and Valleys
The Northern Mississippi Valley Loess Hills area corresponds closely to the Western Coulees and Ridges and Southwest Savanna Ecological Landscapes. Some of the following brief overview is borrowed from the Wisconsin Department of Natural Resources Ecological Landscape publication (2015).
Fifty-two percent of the Upper Mississippi River Bedrock Controlled Uplands and Valleys MLRA is in Wisconsin; Iowa, Minnesota, and Illinois contain the rest. This region is the only area in Wisconsin that has not been covered by glaciers within the past 2.4 million years. The Wisconsin portion of this MLRA is approximately 7.4 million acres (11,600 square miles). The landscape is characterized by dissected topography with deeply-incised, steep-walled valleys between bedrock controlled ridges.
Though it’s called the “Driftless Region”, some glacial drift is found in the major river valleys of this region in the form of outwash, deposited by proglacial streams of glacial meltwater. Wisconsin’s most recent glaciations also impacted the sediment of the area through the deposition of loess. After the glacier receded and before vegetation established, the bare surfaces of the glaciated areas were highly susceptible to wind erosion. As a result, a veneer of loess (wind-blown silt) was deposited over the entire region. The thickest deposits—nearly five meters—are on ridges near the Mississippi River and gradually thin moving eastward. The loess caps in Dane and Green counties are generally 0.5-1.5 meters deep. Much of the loess has eroded downslope and collected in floodplains.
Bedrock is shallow throughout this MLRA and is a major influence on topography and hydrology. Most of the MLRA has bedrock within two meters, except in the deep river valleys that are filled with outwash and alluvium materials. Sandstone is the dominant bedrock type in MLRA 105, but the southernmost portion is dominated by dolomite. Military Ridge is an escarpment that straddles the boundary between sandstone and dolomite bedrock. The sandstone north of the ridge is weaker than the erosion-resistant dolomite south of the ridge. The sandstone is deeply cut and dissected into steep slopes and valleys. The dolomite-controlled ridges tend to be less dissected and broader with more gentle, south sloping topography. Geomorphic and fluvial processes formed these landscapes by way of sheet wash, soil creep, and flowage. These processes eroded the hillslopes, cut into bedrock, and transported the debris to streams, forming floodplains and terraces.
Underfit streams are common in MLRA 105, especially in the southern portion. These streams currently occupy large river valleys—especially those of the Black, Chippewa, Mississippi, and Wisconsin Rivers—that were carved by proglacial meltwater streams carrying much larger quantities of water than what’s present today. As the climate dried, waterflow decreased and the valleys filled with alluvial sediment. Narrow meanders were formed by the shrinking streams and are often dissimilar to the meanders of the larger valleys they occupy. Fluvial landforms – including terraces, oxbow lakes, sandbars, eroding bluffs, and large floodplain complexes – are found within these large valleys and are subject to varying flooding frequencies, intensities, and durations.
Karst topography formed in this region from dissolution of carbonate bedrock by surface and groundwater. Dolomite and limestone are more easily affected by dissolution, but karst topography also formed in sandstone. Erosion by water (stream meanders, rain/runoff, and groundwater), wind, and frost weaken joints and bedding planes that can cause collapse. In addition, sandstone materials collapse into cavities in underlying dolomite or limestone.
Historically, MLRA 105 was dominated by oak forests and oak openings making up more than 50% of the area. Prairies were significant and covered 32% of the area south of Military Ridge. Maple-basswood forests covered 19% of the area north of Military Ridge. Dominant tree species were white oak (Quercus alba), bur oak (Quercus macrocarpa), black oak (Quercus velutina), and sugar maple (Acer saccharum).
Classification relationships
Relationship to Established Framework and Classification Systems:
Habitat Types of S. Wisconsin (Kotar, 1996): The sites in this ES likely key out to Pinus strobus/Vaccinium-Cornus racemose [PVCr] and Acer rubrum/Desmodium-Vaccinium [ArDe-V] if forested.
Biophysical Settings (Landfire, 2014): This ES is largely mapped as North-Central Interior Sand and Gravel Tallgrass Prairie, Paleozoic Plateau Bluff and Talus Woodland, Managed Tree Plantation-Northern and Central Hardwood and Conifer Plantation Group, Eastern Cool Temperate Row Crop, Eastern Cool Temperate Close Grown Crop, and Eastern Cool Temperate Developed Ruderal Grassland
WDNR Natural Communities (WDNR, 2015): This ES is best matches Dry Prairies as described by the Wisconsin DNR
Hierarchical Framework Relationships:
Major Land Resource Area (MLRA): Upper Mississippi River Bedrock Controlled Uplands and Valleys (105)
USFS Subregions: Menominee Eroded Pre-Wisconsin Till (222La), Melrose Oak Forest and Savannah (222Lb), Mississippi-Wisconsin River Ravines (222Lc)
Wisconsin DNR Ecological Landscapes: Western Coulee and Ridges
Ecological site concept
The Dry Mollic or Umbric Upland site occupies approximately 129,000 acres across MLRA 105, or about 1.9% of total land area. It is found in upland positions on sandstone valleys and hills and sandy outwash terraces throughout the MLRA, especially the wide outwash plains along the Chippewa, Mississippi, and Wisconsin rivers.
This site is characterized by somewhat excessively to excessively drained, sandy soils with deep, dark surfaces (mollic or umbric epipedons) resulting from long-term additions of organic materials, especially from fine, fibrous roots of grassy vegetation.
Historically, these sites were prairies, though modern fire suppression has resulted in the encroachment by woody species. Today, many sites are forested.
Associated sites
F105XY002WI |
Wet Sandy Floodplain These sites form in deep, sandy alluvium and outwash deposits in floodplains, especially those along the Chippewa, Black, and Wisconsin rivers. They support vegetation tolerant of seasonal flooding. They are sometimes saturated enough for hydric conditions to occur. They are found in floodplains adjacent to Dry Mollic or Umbric Upland. |
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F105XY006WI |
Moist Sandy Lowland These sites form in sandy outwash deposits along major waterways. They are somewhat poorly drained. They are sometimes found adjacent to adjacent to Dry Mollic or Umbric Upland in lower landscape positions. |
F105XY019WI |
Dry Upland These sites form in sandy materials deposited by wind, water, gravity, or weathered from sandstone bedrock. They are well drained to excessively drained. They are often found adjacent to adjacent to Dry Mollic or Umbric Upland. |
Similar sites
F105XY017WI |
Shallow Dry Upland These sites form in sandy materials deposited by wind, water, gravity, or weathered from sandstone bedrock. They have bedrock contact within one meter of the soil surface. They are somewhat excessively to excessively drained. They are similar to Dry Mollic or Umbric Upland but have shallower surfaces (ochric rather than mollic or umbric epipedons). |
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F105XY019WI |
Dry Upland These sites form in sandy materials deposited by wind, water, gravity, or weathered from sandstone bedrock. They are well drained to excessively drained. They are similar to Dry Mollic or Umbric Upland but have shallower surfaces (ochric rather than mollic or umbric epipedons). |
R105XY011WI |
Mollic Loamy-Silty Upland These sites form in loamy to silty materials, often silty loess and residuum. They have deep, dark surfaces. They are moderately well to somewhat excessively drained. They are similar to Dry Mollic or Umbric Upland but have slightly finer soil textures and are sometimes slightly wetter. |
Table 1. Dominant plant species
Tree |
Not specified |
---|---|
Shrub |
Not specified |
Herbaceous |
(1) Schizachyrium scoparium |
Click on box and path labels to scroll to the respective text.
Ecosystem states
States 2 and 5 (additional transitions)
T1A | - | Suppression of fire |
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R2A | - | Return of fire and/or large grazers to the landscape. |
T2A | - | Continued fire suppression for over 20 years |
T2B | - | Removal of forest/shrub cover and tilling for agricultural crop production. |
T3A | - | Cutting, fire, or blowdown removing existing tree canopy. |
R4A | - | Low intensity moderate return interval fire removing fire intolerant species and regeneration |
R4B | - | Deciduous forest community is slowly invaded by conifers. |
T5A | - | Removal of forest/shrub cover and tilling for agricultural crop production. |
State 1 submodel, plant communities
State 2 submodel, plant communities
State 3 submodel, plant communities
3.1A | - | Light to moderate intensity fires, blow-downs, ice storms. |
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3.2A | - | Disturbance-free period for 30+ years. |