Natural Resources
Conservation Service
Ecological site F090AY021WI
Dry Loamy Upland
Last updated: 10/02/2023
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): 090A–Wisconsin and Minnesota Thin Loess and Till
MLRA 90A is part of the recently glaciated till and outwash plains of central Minnesota and northern Wisconsin. The area was covered with loamy alluvium or loess after glaciation. It is in Wisconsin (56 percent), Minnesota (40 percent), and Michigan (4 percent). It makes up about 21,967 square miles (56,901 square kilometers).
This MLRA has distinct boundaries to the north where it borders tills of a dissimilar origin on the less morainic landscapes of MLRAs 88, 92, and 93A. The boundary to the west is where the MLRA transitions to the calcareous tills of the Des Moines Lobe, in MLRA 57. To the south, MLRA 90A borders MLRA 90B, which has older soils and better-defined drainage patterns, and MLRA 91, which has the distinct lower landscape relief of an outwash channel.
The part of this area in Minnesota is mostly in the Western Lake section of the Central Lowland province of the Interior Plains. Nearly all the parts in Wisconsin and Michigan are in the Superior Upland province of the Laurentian Upland. Four distinct lobes of the Laurentide Ice Sheet (Rainy, Superior, Chippewa, and Green Bay) played major roles in shaping the landscape in this area. The landscape is characterized by gently undulating to rolling, loess-mantled till plains, drumlin fields, and end moraines mixed with outwash plains associated with major glacial drainageways, swamps, bogs, and fens. In some areas lake plains and ice-walled lakes are significant. Steeper areas occur mostly as valley side slopes along flood plains and as escarpments along the margins of lakes.
Lakes, ponds, and marshes are common throughout the area, and streams generally have a dendritic pattern. The major rivers in this area are the Chippewa, St. Croix, Mississippi, and Wisconsin Rivers. Elevation ranges from 1,100 to 1,950 feet (335 to 595 meters). Local relief is mainly less than 10 feet to 20 feet (3 to 6 meters), but some major valleys and hills are 200 feet (60 meters) above the adjacent lowland.
Precambrian-age bedrock underlies most of the glacial deposits in this MLRA. The bedrock is a complex of folded and faulted igneous and metamorphic rocks. The bedrock terrain has been modified by glaciation and is covered in most areas by Pleistocene deposits and windblown silts. The glacial deposits form an almost continuous cover in most areas. The drift is several hundred feet thick in many areas. Loess covered the area shortly after the glacial ice melted.
Ground water is abundant in deep glacial deposits in most of this area. It also occurs in sedimentary and volcanic rock in the western part of the area. It is scarce where the layer of drift is thin. The water meets the domestic, agricultural, municipal, industrial, rural, and irrigation needs of the area. The content of dissolved solids in the ground water from all the various aquifers in this area is low, and the water generally is moderately hard or hard. The level of total dissolved solids in some of the water can be much higher because of a high content of limestone in some of the glacial deposits. Most of this area obtains ground water from unconsolidated glacial sand and gravel deposits on or very near the surface. Some wells tap the Cambrian sandstone in the southwestern part of the area, in Wisconsin.
In northwest Wisconsin (Ashland and Bayfield Counties) where there are no glacial deposits and in much of the part of this area in Minnesota, ground water from sedimentary and volcanic rock aquifers is used. This water is of very good quality; however, many soils have very porous layers that are poor filters of domestic waste and agricultural chemicals, so there is a risk of contamination from development and agriculture. Minor water concerns are hardness and, in some areas, high concentrations of iron. Yields of water from the glacial deposits vary.
The dominant soil orders are Alfisols, Entisols, Histosols, and Spodosols. The soils in the area have a frigid temperature regime, a udic or aquic moisture regime, and mixed mineralogy.
This area has a significant acreage of public and private forestland used to support the paper and lumber industry Sap collection from sugar maple and syrup production are important forestry enterprises. Agricultural enterprises include row crops, dairy farms, and beef operations. Crops include corn, soybeans, oats, wheat, and alfalfa. Tourism, recreation, and wildlife management are important. Hunting, fishing, snowmobiling, hiking, and skiing are popular activities because of the area’s abundance of water, the many acres of national and county forests, and public hunting grounds. (United States Department of Agriculture, Natural Resources Conservation Service, 2022)
Classification relationships
Major Land Resource Area (MLRA 90A): Wisconsin and Minnesota Thin Loess and Till
USFS Subregions: Lincoln Formation Till Plain - Mixed Hardwoods (212Qb), St. Croix Moraine (212Qa), Rib Mountain Rolling Ridges (212Qd), Green Bay Lobe Stagnation Moraine (212Ta), Central-Northwest Wisconsin Loess Plains (212Xd)
Small sections occur in Rosemont Baldwin Plains and Moraines (222Md), Perkinstown End Moraine (212Xe), Hayward Stagnation Moraines (212Xf)
Wisconsin DNR Ecological Landscapes: North Central Forest, Forest Transition, Western Prairie
Ecological site concept
The Dry Loamy Upland ecological site is scattered across MLRA 90A, located on outwash plains, stream terraces, kames, and hills. These sites are characterized by very deep, somewhat excessively and excessively drained soils that formed in loamy deposits including outwash, alluvium, and drift. Some sites may have a sandy mantle or underlying sandy or deposits. Precipitation and runoff are the primary water sources. Soils range from very strongly acid to neutral.
Dry Loamy Upland is distinguished from other ecological sites by its deep loamy deposits and somewhat excessively and excessively drained soils. Other somewhat excessively and excessively drained sites have sandy deposits. The loamy material often has a higher pH and available water capacity than sandy material.
Associated sites
F090AY016WI |
Loamy Upland Loamy Upland consist of deep loamy till, alluvium, residuum, lacustrine, or eolian deposits. Sandy deposits of these parent materials, plus outwash, may also be present. The depth to the seasonally high water table ranges from as high as the surface to as low as almost two meters below the surface. A few sites are on floodplains and upland drainageways, where very brief flooding is rare but possible. They are wetter and occur lower on the drainage sequence than Dry Loamy Upland. |
---|---|
F090AY002WI |
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 Dry Loamy Upland. |
F090AY006WI |
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 much wetter and occur lower on the drainage sequence than Dry Loamy Upland. |
F090AY011WI |
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 occur lower on the drainage sequence than Dry Loamy Upland. |
Similar sites
F090AY020WI |
Dry Loamy Bedrock Upland Dry Loamy Bedrock Upland consist of silty loess, sometimes underlain by loamy till. Basalt or quartzite bedrock typically occurs within one meter of the surface. These soils show no evidence of a seasonally high water table. They are found in similar landscape positions and share both drainage class and particle size with Dry Loamy Upland but have bedrock contact within two meters of the surface. |
---|---|
F090AY019WI |
Dry Sandy Uplands Dry Sandy Uplands consist of primarily sandy deposits of various origin. Loamy deposits are also present in many soils. They may have a seasonally high water table within two meters of the surface, though they do not remain saturated for sustained periods. They are found in similar landscape positions and share their drainage class with Dry Loamy Upland but have coarser particle sizes. |
Table 1. Dominant plant species
Tree |
(1) Acer saccharum |
---|---|
Shrub |
(1) Corylus |
Herbaceous |
(1) Oligoneuron |
Click on box and path labels to scroll to the respective text.
T1A | - | Clear cutting or stand-replacing fire. |
---|---|---|
T1B | - | Removal of forest vegetation and tilling. |
R2A | - | Disturbance-free period 70+ years. |
T2A | - | Removal of forest vegetation and tilling. |
T3A | - | Stopping of agricultural practices and allowing to natural revegetation, or site is replanted. |
State 1 submodel, plant communities
1.1A | - | Light to moderate intensity fires, blow-downs, snow-ice breakage. |
---|---|---|
1.2A | - | Disturbance-free period 30+ years |
State 2 submodel, plant communities
2.1A | - | Red oak and red maple regenerating under aspen -- paper birch canopy |
---|---|---|
2.2A | - | Time and natural succession. |
2.3A | - | Major stand replacing disturbance e.g. blow-down and fire, or clear-cutting, followed by fire. |