Natural Resources
Conservation Service
Ecological site F093BY007MI
Sandy Uplands
Last updated: 9/27/2023
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): 093B–Superior Stony and Rocky Loamy Plains and Hills
The Wisconsin portion of this MLRA is a mixture of high-relief moraines and flat till plains with interspersed glacial meltwater deposits. It is bordered on the north by glaciolacustrine deposits of Glacial Lake Duluth and on the south by extensive pitted and unpitted outwash plains. The approximate land area is just under 600,000 acres (935 sq miles).
The Penokee-Gogebic Iron Range runs through the middle of the Wisconsin portion of this MLRA and into Michigian. The range is a hilly, bedrock-controlled moraine. The bedrock outcropping is composed of igneous and metamorphic materials and was created by inland folding and faulting of the ancient Superior continent when it collided with the Marshfield continent about 1.8 billion years ago (Dott & Attig, 2004). Volcanic and intrusive bedrock occurs in some places. This bedrock is overlain by a thin layer of glacial till deposited by the Chippewa Lobe.
To the north of the range is a former spillway for Glacial Lake Ontonagon. The flowing meltwater cut deep channels into the morainal systems. Glaciofluvial landforms here include old beaches and dunes. South of the range, along the southern edge of this MLRA, are rolling collapsed end moraines, pushed to their extent by the Chippewa and Ontonagon Lobes. The landscape is dotted with abundant kettle lakes and swamps, especially in the eastern portion. Ice-walled lake plains and eskers are also found along these collapsed moraines.
The climate is influenced by Lake Superior in areas near the lake, resulting in cooler summers, warmer winters, and greater precipitation – especially snowfall – compared to more inland locations. Historically, mixtures of eastern hemlock (Tsuga canadensis), sugar maple (Acer saccharum), yellow birch (Betula alleghaniensis), eastern white pine (Pinus strobus), and red pine (Pinus resinosa) covered the area. In wetter pockets (such as the swamps that dot the moraines to the south) white cedar (Thuja occidentalis), black spruce (Picea mariana), and tamarack (Larix laricina) were common (Finley, R., 1976).
Classification relationships
Relationship to Established Frameworks and Classification Systems:
Habitat Types of N. Wisconsin (Kotar, 2002): Two sites key out to Acer saccharum – Tsuga canadensis/ Maianthemum canadense (ATM), though one is difficult to key and may also be represented by Pinus strobus – Acer rubrum/ Vaccinium angustifolium (PArV), and one site keys to Acer saccharum/ Vaccinium angustifolium – Viburnum acerifolium (AVVb).
Biophysical Setting (Landfire, 2014): This ES is mapped as Laurentian-Acadian Northern Pine(-Oak) Forest, Laurentian-Acadian Northern Hardwoods Forest – Hemlock, and Laurentian-Acadian Northern Hardwoods Forest; though, it is likely best represented by the latter.
WDNR Natural Communities (WDNR (2015): This ES is most similar to the Northern Dry-mesic, Mesic, and Boreal Forests.
Hierarchical Framework Relationships:
Major Land Resource Area (MLRA): Superior Stoney and Rocky Loamy Plains and Hills, Eastern Part (93B)
USFS Subregions: Winegar Moraines (212Jc)
Small sections occur in the Gogebic-Penokee Iron Range (212Jb) subregion
Wisconsin DNR Ecological Landscapes: North Central Forest
Ecological site concept
The Sandy Uplands ecological site found on outwash, till, and lake plains, moraines, hillslopes, and stream terraces. These sites are characterized by very deep, moderately well or well drained soils that formed in sandy glaciofluvial, alluvium, and outwash deposits. Precipitation and runoff from adjacent uplands are the primary sources of water. Soils range from very strongly acid to moderately acid.
Sandy Uplands lacks a layer of significant clay accumulation like those found in Alfic Sandy Uplands. These sites have a lower available water capacity than their Alfic counterparts, which limits the plant communities they can support. Other upland sites have loamy materials. Sandy materials often have a lower pH and available water capacity than loamy materials, which may limit vegetative growth.
Associated sites
F093BY004MI |
Wet Lowlands Wet Lowlands occur on depressions and drainageways and form in loamy till or loamy alluvium underlain by dense sandy till or sandy and gravelly outwash. These sites are poorly drained and occur lower on the drainage sequence than Sandy Uplands. |
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F093BY005MI |
Moist Lowlands Moist Lowlands occur on footslope positions across the landscape. They are not subject to flooding nor ponding. Soils form in till, lacustrine deposits, or outwash deposits and may be loamy to sandy. These sites are somewhat poorly drained and occur slightly lower on the drainage sequence than Sandy Uplands. |
F093BY011MI |
Dry Uplands Dry Uplands are found in the sandiest, most permeable soils on the driest landscape positions. They are very deep and excessively drained. These sites occur slightly higher on the drainage sequence than Sandy Uplands. |
Similar sites
F093BY011MI |
Dry Uplands Dry Uplands are found in the sandiest, most permeable soils on the driest landscape positions. While their landscape positions and textures are quite similar, the moderately well to somewhat excessively drained Sandy Uplands sometimes support mesic (ie. slightly wetter) vegetative communities than Dry Uplands. |
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F093BY006MI |
Alfic Sandy Uplands Alfic Sandy Uplands occur on upland sites in deep sandy drift deposits where and argillic horizon is either present or forming. These soils are well to somewhat excessively drained. Unlike Sandy Uplands, Alfic Sandy Uplands have a horizon of significant clay accumulation and can hold slightly more water than their Sandy counterparts. The vegetative community reflects this, with more mesic and slightly more nutrient-demanding species present on Alfic Sandy Uplands. |
F093BY010MI |
Loamy Uplands Loamy Uplands occur on upland sites in loamy till, sometimes with a mantle of loess. Like Sandy Uplands, these soils lack significant clay accumulation and are moderately well to well drained. The soil textures of Loamy Uplands are finer than those of Sandy Uplands. Species present on Loamy Uplands are slightly more nutrient-demanding than those present on Sandy Uplands. |
Table 1. Dominant plant species
Tree |
(1) Acer saccharum |
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Shrub |
(1) Acer saccharum |
Herbaceous |
(1) Pteridium aquilinum |
Click on box and path labels to scroll to the respective text.
T1A | - | Large scale disturbance |
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T1B | - | Clearing of site; agricultural production |
R2A | - | Abandon agricultural practices |
T2A | - | Clearing; agricultural production |
State 1 submodel, plant communities
1.1.A | - | Natural mortality in the oldest age classes, sporadic small-scale blow-downs and ice storms, create openings for entry of mid-tolerant species, such as red oak and red maple. |
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1.2.A | - | Time and natural succession |
State 2 submodel, plant communities
2.1.A | - | Red oak and red maple regenerate under aspen-paper birch canopy |
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2.2.A | - | Time and natural succession |