Natural Resources
Conservation Service
Ecological site FX053A99X756
Woody Draw (WD)
Last updated: 11/22/2023
Accessed: 11/23/2024
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): 053A–Northern Dark Brown Glaciated Plains
The Northern Dark Brown Glaciated Plains, MLRA 53A, is a large, agriculturally and ecologically significant area. It consists of approximately 6.1 million acres and stretches 140 miles from east to west and 120 miles from north to south, encompassing portions of 8 counties in northeastern Montana and northwestern North Dakota. This region represents part of the southern edge of the Laurentide Ice Sheet during maximum glaciation. It is one of the driest and westernmost areas within the vast network of glacially derived prairie pothole landforms of the Northern Great Plains and falls roughly between the Missouri Coteau to the east and the Brown Glaciated Plains to the west. Elevation ranges from 1,800 feet (550 meters) to 3,300 feet (1,005 meters).
Soils are primarily Mollisols, but Inceptisols and Entisols are also common. Till from continental glaciation is the predominant parent material, but alluvium and bedrock are also common. Till deposits are typically less than 50 feet thick (Soller, 2001). Underlying the till is sedimentary bedrock largely consisting of Cretaceous shale, sandstone, and mudstone (Vuke et al., 2007). The bedrock is commonly exposed on hillslopes, particularly along drainageways. Significant alluvial deposits occur in glacial outwash channels and along major drainages, including portions of the Missouri, Poplar, and Big Muddy Rivers. Large eolian deposits of sand occur in the vicinity of the ancestral Missouri River channel east of Medicine Lake (Fullerton et al., 2004). The northwestern portion of the MLRA contains a large unglaciated area containing paleoterraces and large deposits of sand and gravel known as the Flaxville gravel.
Much of this MLRA was glaciated towards the end of the Wisconsin age, and the maximum glacial extent occurred approximately 20,000 years ago (Fullerton and Colton, 1986; Fullerton et al., 2004). Subsequent erosion from major stream and river systems has created numerous drainageways throughout much of the MLRA. The result is a geologically young landscape that is predominantly a dissected till plain interspersed with alluvial deposits and dominated by soils in the Mollisol and Inceptisol orders. Much of this area is typic ustic, making these soils very productive and generally well suited to production agriculture.
Dryland farming is the predominant land use, and approximately 50 percent of the land area is used for cultivated crops. Winter, spring, and durum varieties of wheat are the major crops, with over 48 million bushels produced annually (USDA-NASS, 2017). Areas of rangeland typically are on steep hillslopes along drainages. The rangeland is mostly native mixed-grass prairie similar the Stipa-Agropyron, Stipa-Bouteloua-Agropyron, and Stipa-Bouteloua faciations (Coupland, 1950; 1961). Cool-season grasses dominate and include rhizomatous wheatgrasses, needle and thread, western porcupine grass, and green needlegrass. Woody species are generally rare; however, many of the steeper drainages support stands of trees and shrubs such as green ash and chokecherry. Seasonally ponded, prairie pothole wetlands may occur throughout the MLRA, but the greatest concentrations are in the east and northeast where receding glaciers stagnated and formed disintegration moraines with hummocky topography and numerous areas of poorly drained soils.
Classification relationships
NRCS Soil Geography Hierarchy
• Land Resource Region: Northern Great Plains
• Major Land Resource Area (MLRA): 053A Northern Dark Brown Glaciated Plains
National Hierarchical Framework of Ecological Units (Cleland et al., 1997; McNab et al., 2007)
• Domain: Dry
• Division: Temperate Steppe
• Province: Great Plains-Palouse Dry Steppe Province 331
• Section: Glaciated Northern Grasslands Section 331L
• Subsection: Glaciated Northern Grasslands Subsection 331La
• Landtype association/Landtype phase: N/A
National Vegetation Classification Standard (Federal Geographic Data Committee, 2008)
• Class: Forest and Woodland Class (1)
• Subclass: Temperate and Boreal Forest and Woodland Subclass (1.B)
• Formation: Cool Temperate Forest and Woodland Formation (1.B.2)
• Division: North American Great Plains Forest and Woodland Division (1.B.2.Ne)
• Macrogroup: Great Plains Forest and Woodland Macrogroup (1.B.2.Ne.1)
• Group: Great Plains Mesic Forest and Woodland Group (1.B.2.Ne.1.b)
• Alliance: Great Plains Ash - Elm Ravine Forest
EPA Ecoregions
• Level 1: Great Plains (9)
• Level 2: West-Central Semi-Arid Prairies (9.3)
• Level 3: Northwestern Glaciated Plains (42)
• Level 4: Glaciated Dark Brown Prairie (42i)
Glaciated Northern Grasslands (42j)
Ecological site concept
Woody Draw is an extensive ecological site occurring on moderately steep to very steep landscapes where the till plain has been dissected by streams or rivers. It typically occurs in the narrowest, most sheltered swales and is most common on northerly aspects. The distinguishing characteristic of this site is that it receives additional moisture via surface runoff from adjacent sites and that it supports a predominantly woody plant community. Soils for this ecological site are typically very deep (more than 60 inches), well drained, and derived from alluvium or till. Characteristic vegetation is green ash (Fraxinus pennsylvanica), American elm (Ulmus americana), chokecherry (Prunus virginiana), and serviceberry (Amelanchier alnifolia).
Associated sites
FX053A99X062 |
Swale (Se) The Swale ecological site is found adjacent to the Woody Draw ecological site on similar landforms. It is typically downslope from the Woody Draw ecological site and generally occurs on broader, less sheltered swale microfeatures. |
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FX053A99X032 |
Loamy (Lo) The Loamy ecological site is found upslope from and commonly surrounding the Woody Draw ecological site. It is typically found in summit positions where the upper 4 inches of soil contains 18 to 35 percent clay. |
FX053A99X040 |
Loamy Steep (LoStp) The Loamy Steep ecological site is found on slopes of 15 percent or greater upslope from the Woody Draw ecological site. It occurs on backslope positions whereas the Woody Draw ecological site occurs on toeslopes on swale microfeatures. |
FX053A99X029 |
Limy Steep (LyStp) The Limy Steep ecological site is found on slopes of 15 percent or greater upslope from the Woody Draw ecological site. It occurs on convex backslope positions whereas the Woody Draw ecological site occurs on swale microfeatures. |
Similar sites
FX053A99X062 |
Swale (Se) This site differs from the Woody Draw ecological site in that it is dominated by herbaceous species. Bunchgrasses dominate the site in terms of cover and production. |
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FX053A99X061 |
Riparian Woodland (RW) This site differs from the Woody Draw ecological site in that it is on flood plains rather than upland swales. It generally is on stream terraces adjacent to a perennial stream reach. Woody vegetation typically contains riparian species such as sandbar willow and plains cottonwood. |
FX053A99X032 |
Loamy (Lo) This site differs from the Woody Draw ecological site in that it is in higher topographical positions that do not receive additional moisture and it does not support woody vegetation whereas the Woody Draw ecological site is in the bottoms of coulees or swales and receives additional moisture. |
Table 1. Dominant plant species
Tree |
(1) Fraxinus pennsylvanica |
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Shrub |
(1) Prunus virginiana |
Herbaceous |
Not specified |
Legacy ID
R053AY723MT
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Ecosystem states
T1A | - | Introduction of non-native grass species, such as Kentucky bluegrass, smooth brome, etc. |
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T2A | - | Stand-replacing fire in combination with prolonged improper grazing management |
T2B | - | Prolonged improper grazing management |
R3A | - | Proper grazing management, tree/shrub planting, intensive weed management (management intensive and costly) |
R4A | - | Proper grazing management, tree/shrub planting, intensive weed management (management intensive and costly) |
State 1 submodel, plant communities
State 2 submodel, plant communities
P2.1a | - | Stand-replacing fire |
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P2.1b | - | Improper grazing management |
P2.2a | - | Lack of disturbance, tree regeneration, and woody plant regrowth |
P2.3a | - | Proper grazing management |