Natural Resources
Conservation Service
Ecological site F090BY016WI
Loamy Upland
Last updated: 11/16/2023
Accessed: 11/13/2024
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): 090B–Central Wisconsin Thin Loess Dissected Till Plain
The Wisconsin and Minnesota Thin Loess MLRA, Northern and Southern Parts (90A and 90B) correspond closely to the North Central Forest and the Forest Transition Ecological Landscapes, respectively. Some of the following brief overview is borrowed from the Wisconsin Department of Natural Resources ecological landscape publications (2015).
The Wisconsin and Minnesota Thin Loess MLRA, Northern and Southern Parts (90A and 90B) is an extensive glacial landscape that comprised of over 11.1 million acres (17,370 sq mi) throughout central and northern Wisconsin – about 27% of the total land area in the state. This glacial landscape is comprised of a heterogenous mix of loess-capped ground moraines, end moraines with eskers and ice-walled lake plains, and pitted, unpitted, and collapsed outwash plains sometimes interspersed with drumlins from the Illinoian and Pre-Illinoian glaciations. The entire area has been glaciated and nearly all of it is underlain by dense glacial till that impedes drainage. An extensive morainal system – the Perkinstown end moraine – spans most of the width of northern Wisconsin and divides the Northern and Southern Parts of this large landscape. This moraine, which has been sliced by outwash in many places, marks the southernmost extent of the Wisconsin glaciation (Wisconsin’s most recent glacial advance).
North of the Perkinstown morainal system is a loess plain, with a loess mantle 6-24 inches thick. The northernmost edge of this landscape is an undulating till and outwash plain with materials deposited by the Chippewa Lobe. Drumlins are common in the northern and northeastern portions. The drumlins are oriented towards the southwest and formed during a glacial episode prior to the most recent glacial advance. Some are covered with glacial till. Pitted, unpitted, and collapsed outwash plains fill the spaces between drumlins. Detached from the major land mass to the northeast is the hummocky Hayward collapsed end moraines, where swamps, ice-walled lake plains, and eskers are common.
Most of the MLRA to the south of the Perkinstown morainal system is an extensive ground moraine with some proglacial stream features including pitted outwash plains, terraces, and fans. A layer of loess 6-47 inches thick covers much of the area. Like the Northern Part, all areas of the Southern Part of this MLRA were glaciated, although the southcentral portion is a relatively older till plain with materials from the Illinoian and pre-Illinoian glaciations, not the most recent Wisconsin glaciation. The landforms in the southcentral portion are highly variable. Much of the area topography is controlled by underlying bedrock. Sandstone outcrops and pediments can be found here. Some of the most southern portions of the MLRA are mixed glacial deposits and residuum.
The land surface of the southeastern portion was formed by many small glacial advances and retreats. Morainal ridges protrude through an erosional, pitted outwash-mantled surface. These parallel ridges run in a northeast to southwest orientation and are dissected by many steams.
The continental climate of this MLRA is typical of northcentral Wisconsin, with cold winters and warm summers. The southern boundary of this MLRA straddles Wisconsin’s Tension Zone, a zone of transition between Wisconsin’s northern and southern ecological landscapes. Historically, the mesic forests were dominated by eastern hemlock (Tsuga canadensis), sugar maple (Acer saccharum), and yellow birch (Betula alleghaniensis).
Classification relationships
Major Land Resource Area (MLRA): Wisconsin and Minnesota Thin Loess and Till (Northern and Southern Parts – 90A and 90B)
USFS Subregions: Central-Northwest Wisconsin Loess Plains (212Xd), Glidden Loamy Drift Plain (212Xa), Hayward Stagnation Moraines (212Xf), St. Croix Moraine (212Qa), Lincoln Formation Till Plain - Mixed Hardwoods (212Qb), Lincoln Formation Till Plain - Hemlock Hardwoods (212Qc), Brule and Paint Rivers Drumlinized Ground Moraine (212Xc), Perkinstown End Moraine (212Xe), Mille Lacs Uplands (212Kb), Rosemont Baldwin Plains and Moraines (222Md), Rib Mountain Rolling Ridges (212Qd)
Small sections occur in Bayfield Sand Plains (212Ka)
Wisconsin DNR Ecological Landscapes: North Central Forest, Forest Transition, Western Prairie, Northwest Lowlands, Northwest Sands
Ecological site concept
The Loamy Upland ecological site is extensive. It’s found across MLRAs 90A and 90B, located on outwash, lake, and till plains, glacial lake basins, moraines, stream terraces, kames, eskers, and drumlins. These sites are characterized by very deep, moderately well and well drained soils that formed in loamy deposits including till, alluvium, lacustrine, colluvium, and residuum. Some sites may have a sandy mantle or underlying sandy or clayey deposits. Precipitation and runoff are the primary water sources. Soils range from very strongly acid to moderately alkaline.
Loamy Upland is distinguished from other ecological sites by its deep loamy deposits and moderately well and well drained soils. This site lacks the high level of carbonates found in Loamy Upland with Carbonates. Other moderately well and well drained sites have sandy or clayey deposits. The loamy material often has a higher pH and available water capacity than sandy material, but less than clayey material. The moderately well and well drained soils differentiates this site from other loamy sites.
Associated sites
F090BY002WI |
Mucky Swamp Mucky Swamp sites consist of deep, highly decomposed herbaceous organic materials. Some sites have mineral soil contact. They are very poorly drained and are neutral to slightly acid. These sites are permanently saturated wetlands. They are much wetter and occur lower on the drainage sequence than Loamy Upland. |
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F090BY006WI |
Wet Loamy Lowland Wet Loamy Lowland consist primarily of deep loamy deposits derived from a mixture of outwash, alluvium, loess, and lacustrine sources. Some sites may have bedrock contact within two meters of the surface. These sites are seasonally ponded depressions that remain saturated for sustained periods, allowing hydric conditions to occur. They are wetter and occur lower on the drainage sequence than Loamy Upland. |
F090BY011WI |
Moist Loamy Lowland Moist Loamy Lowland consist of deep sandy and loamy deposits derived from a mixture of alluvium, residuum, till, or lacustrine sources. The finer textures allow the soil to stay moist - but not saturated - for sustained periods during the growing season. They are wetter and lower higher on the drainage sequence than Loamy Upland. |
F090BY021WI |
Dry Loamy Upland Dry Loamy Upland consist of deep sandy to loamy outwash, alluvium, or till. The water table is deeper than two meters year-round. They are drier and occur higher on the drainage sequence than Loamy Upland. |
Similar sites
F090BY014WI |
Loamy Bedrock Upland Loamy Bedrock Upland consist of loamy till, alluvium, or eolian deposits underlain by sandy to loamy residuum. Some sites may also contain sandy outwash or clayey pedisediment. Bedrock contact occurs within two meters of the surface. They have a seasonally high water table within one meter of the surface, though they don't remain saturated for extended periods of time. They occur in similar landscape positions and share both particle size and drainage class with Loamy Upland but have bedrock contact within two meters. |
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F090BY015WI |
Loamy Upland with Carbonates Loamy Upland with Carbonates consist of deep loamy till, colluvium, alluvium, residuum, or eolian deposits. Some sites may also have sandy outwash or eolian deposits. Carbonates are present in these soils. They have a seasonally high water table within one meter of the surface, though they don't remain saturated for extended periods of time. They occur in similar landscape positions and share both particle size and drainage class with Loamy Upland but have free carbonates within two meters. |
F090BY017WI |
Clayey Upland Clayey Upland consist of loamy to clayey residuum or lacustrine deposits overlain by loess or sandy outwash. Bedrock contact may occur within two meters of the surface. These sites have a seasonally high water table within one meter of the surface, though they are not saturated for sustained periods. They occur in similar landscape positions and share drainage class with Loamy Upland but have finer particle sizes. |
Table 1. Dominant plant species
Tree |
(1) Acer saccharum |
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Shrub |
Not specified |
Herbaceous |
(1) Eurybia macrophylla |
Click on box and path labels to scroll to the respective text.
T1A | - | Clear cutting or stand-replacing fire. |
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T1B | - | Removal of forest vegetation and tilling. |
R2A | - | Disturbance-free period 70+ years. |
T2A | - | Removal of forest cover and tilling for agricultural crop production. |
T3A | - | Removal of forest vegetation and tilling. |
State 1 submodel, plant communities
1.1A | - | Light to moderate intensity fires, blow-downs, snow-ice breakage. |
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1.2A | - | Disturbance-free period for 30+ years. |
State 2 submodel, plant communities
2.1A | - | Immigration and establishment of red oak and red maple. |
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2.2A | - | Immigration and establishment of red oak and red maple. |
2.3A | - | Clear cutting or stand-replacing fire. |