Natural Resources
Conservation Service
Ecological site F103XY027MN
Loamy Wet Forests
Last updated: 10/04/2023
Accessed: 07/06/2026
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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): 103X–Central Iowa and Minnesota Till Prairies
MLRA 103 is in Minnesota (56 percent) and Iowa (44 percent) and consists of approximately 18 million acres. It is in the Western Lake Section of the Central Lowland Province of the Interior Plains in an area known as the "Des Moines Lobe" of the Wisconsin-age ice sheet.
The MLRA is mostly on a young, nearly level to gently rolling, glaciated till plain that has moraines and glacial lake plains in some areas. The plain is covered with glacial till, outwash, and glacial lake deposits. Recent alluvium consisting of clay, silt, sand, and gravel fill the bottoms of most of the major river valleys. Paleozoic bedrock sediments, primarily shale and limestone, underlie the glacial deposits in most of the area.
The annual precipitation increases from northwest to southeast. Most of the rainfall occurs as high-intensity, convective thunderstorms during the summer. Two-thirds or more of the precipitation falls during the freeze-free period. Snowfall is common in winter. Ground water supplies are adequate for the domestic, livestock, municipal, and industrial needs.
Nearly all of this area is farmland, and about four-fifths is cropland.Classification relationships
U.S. Department of Agriculture (USDA)
Land Resource Regions and Major Land Resource Areas (USDA_NRCS, 2006)
Major Land Resource Area (MLRA): Central Iowa and Minnesota Till Prairies (103)
U.S. Forest Service (USFS)
National Hierarchical Framework of Ecological Units (Cleland et al., 2007)
Section: North central Glaciated Plains (251B)
Subsections: Upper Minnesota River-Des Moines Lobe (251BA) and Southern Des Moines
Lobe (251Be)
International Vegetation Classification Hierarchy
Class: 1 Forest & Woodland
Subclass: 1.B Temperate & Boreal Forest & Woodland
Formation: 1.B.2 Cool Temperate Forest & Woodland
The reference state shares similarities to the Minnesota Department of Natural Resources MHs49 Southern Wet-Mesic Hardwood ForestEcological site concept
The Loamy Wet Forests ecological site occurs on loamy textured soils that have a seasonal depth to soil saturation of 0 to 30 cm. This site is located on end and lateral moraines in the Northeastern portion of MLRA 103. No flooding or ponding usually occurs. Landforms include lake plains and lateral end and ground moraines.
Associated sites
R103XY018MN Shallow Lakes
The Shallow Lakes ecological site is ponded in the natural state. Soils are poorly drained Histosols that are high in organic matter content and developed in shallow lakes.
F103XY025MN Loamy Upland Forests
The Loamy Upland Forests ecological site occurs on upland soils which are derived from loamy till and have a thin or moderately thick dark (mollic) surface layer. The drainage class ranges from somewhat poorly drained to well drained.
R103XY017MN Organic Wet Meadow/Carr
The Organic Wet Meadow/Carr ecological site occurs in low wetland areas. These sites are usually ponded, have a high water table (i.e. endosaturated), and are classified as very poorly drained. Water-tolerant vegetation such as cattails, bulrushes, and sedges are dominant.
F103XY036MN Depressional Wet Forests
The Depressional Wet Forests ecological site is characterized by a water table that is typically above the soil surface (ponded) during the spring months and may drop to as low as three feet later during dry periods. The included soils are classified as Cumulic Endoaquolls that developed under forest vegetation and have a thick accumulation of slope alluvium.
F103XY024MN Sandy Upland Forests
The Sandy Upland Forests ecological site is located on soils that have a surface texture of loam, sandy loam, or sand and have a layer of sandy or gravelly material below the surface horizon. These soils were formed predominantly under forest vegetation.
Similar sites
F103XY030MN Wet Footslope/Drainageway Forests
The Wet Footslope/Drainageway Forests ecological site is located on lower footslopes or in wet drainageways. The soils are derived from loamy or clayey colluvium, slope alluvium, alluvium, or a combination of these parent materials. Soil drainage class is somewhat poorly drained to poorly drained.
Table 1. Dominant plant species
Tree (1) Acer saccharum
(2) Fraxinus nigraShrub (1) Celtis occidentalis
Herbaceous (1) Laportea canadensis