

Natural Resources
Conservation Service
Ecological site R055AY045ND
Loamy Savannah
Last updated: 5/08/2025
Accessed: 05/21/2025
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): 055A–Northern Black Glaciated Plains
The Northern Black Glaciated Plains MLRA is an expansive and agriculturally important region consisting of 8,200,000 acres and including all or a portion of 16 counties in north-central and northeast North Dakota.
Nearly all MLRA 55A is covered by till: material that was moved and redeposited by the glaciers. Pre-glaciated bedrock (shale) is exposed in some of the deeper valleys and at the edges of some hills; but what covers the bedrock is glacial sediment, known as drift. These areas have the Late Wisconsin age till plain integrated drainage system in contrast to the closed drainage of the majority of the till plain and moraines. The Drift Prairie Region consists of nearly level to gently rolling glacial till plains dissected by glacial outwash channels. Five rivers flow through parts of the MLRA. The Souris (also known as Mouse) River meanders across the Canadian border through Renville and Ward counties; it then loops east through McHenry County and north through Bottineau County returning to Canada. The Des Lacs River flows southward from Canada through Burke, southwest Renville, and Ward counties where it joins the Souris River. Along the eastern edge of the MLRA the Pembina River, Park River, and Forest River flow eastward to join the Red River. Some soils along these rivers have weathered shale beds in the substratum.
This region is utilized mostly by farms and ranches; about 80 percent is cropland that is dry-farmed. Cash-grain, bean and oil production crops are the principal enterprise on many farms, but other feed grains and hay are also grown. The vegetation on the steeper slopes and thinner (or sandy) soils is still native rangeland. About 3 percent of this area is forested. The most extensive areas of forest are in Turtle Mountain, Pembina Gorge and Hills, and on the moraines in proximity to Devils Lake.
Classification relationships
Level IV Ecoregions of the Conterminous United States: 46a – Pembina Escarpment; 46b – Turtle Mountains; 46f – End Moraine Complex; and 46g – Northern Black Prairie.
Ecological site concept
The Loamy Savanna ecological site is located on linear side slopes of moraines and escarpments. The soils generally are very deep, but on escarpments, some soils have weathered shale as shallow as 5 feet. These soils, typically, have indicators of forming under both forested and prairie conditions – in particular, uncoated sand grains or grayish silt coats on ped surfaces in the subsoil. The soils commonly have a thin layer or undecomposed organic materials on the surface. The dark-colored surface soil is more than 7 inches thick. Typically, the surface texture is loam and the subsoil is clay loam (<35% clay). The subsoil forms a ribbon 1-2 inches long. Soil on this site is moderately well drained or well drained. Generally, calcium carbonate has been leached into the lower subsoil. Slopes range from 0 to 25 percent. On the landscape, this site is below the Thin Loamy ecological site and above the Loamy Overflow, Limy Subirrigated, and Shallow Marsh sites. The Upland Hardwood Forest and Loamy ecological sites occur on similar landscape positions. The Upland Hardwood Forest site developed under densely forested conditions and typically has >35% clay in the subsoil (forms a ribbon >2 inches long).
This is the ecotone or tension zone between forested areas and the adjacent prairie. On both temporal and spatial scales, this state would have historically supported a mosaic of woody vegetation and/or open grassland resulting from the variability in precipitation, fire, and other disturbances. There will be variations in the plant community depending on the disturbance. Common disturbances include drought, excessive rain, early or late frost, disease, fire, insect infestation, weather fluctuations and/or management actions. Management actions like grazing systems and exclusion of the area will impact the vegetation vigor and composition as a result of the disturbances.
To see a full copy of the ecological site description with all tables and the full version 5 rangeland health worksheet, please use the following hyperlink:
https://efotg.sc.egov.usda.gov/references/public/ND/55A_Loamy_Savannah_Narrative_FINAL_Ref_FSG.pdf
Associated sites
F055AY058ND |
Upland Hardwood Forest This site is on similar landscape positions in the Turtle Mountain and Pembina Gorge areas. It is more densely forested. It typically has >35% clay (forms a ribbon >2 inches long) in the subsoil. |
---|---|
R055AY041ND |
Loamy Overflow This site occurs on lower, concave slopes – a run-on position – it does not have ‘alfic’ properties. It formed under prairie vegetation. |
R055AY052ND |
Thin Loamy This site occurs on shoulder slopes and tops of ridges. It formed under prairie vegetation – it does not have ‘alfic’ properties. It has strong or violent effervescence within a depth of 8 inches. |
R055AY054ND |
Shallow Marsh This site occurs in deep depressions which have frequent ponding through most of the growing season. |
R055AY040ND |
Limy Subirrigated This site occurs lower on the landscape. It is highly calcareous in the upper subsoil and has redoximorphic features at a depth of 18 to 30 inches. |
Similar sites
R055AY047ND |
Loamy This site occurs on similar landscape positons. It formed under prairie vegetation – it does not have ‘alfic’ properties. |
---|---|
F055AY058ND |
Upland Hardwood Forest This site is on similar landscape positions in the Turtle Mountain and Pembina Gorge areas. It is more densely forested. It typically has >35% clay (forms a ribbon >2 inches long) in the subsoil. |

Figure 1. Mosaic of woody and grassland vegetation typical of Loamy Savannah ecological site.
Table 1. Dominant plant species
Tree |
(1) Quercus macrocarpa |
---|---|
Shrub |
(1) Corylus |
Herbaceous |
(1) Pascopyrum smithii |
Physiographic features
This site occurs on moraines and escarpments. It is associated with native forests on the escarpment of Turtle Mountain, areas on the south side of Devils Lake, and the Pembina Escarpment and Pembina River Gorge, and on moraines in proximity to Devils Lake. Turtle Mountain moraine rises about 600-800 feet (183-244 meters) above the surrounding ground moraine and has numerous lakes and deep marshes scattered throughout. Coupled with elevation, the moraine located on the southeast side of Devils Lake, benefited from large body of water as a natural fire shield from prevailing winds (north and west) reducing the fire frequency allowing for woody vegetation to dominate. The Pembina Escarpment separates the ground moraine to the west from Glacial Lake Agassiz (Red River Valley) lying 300-400 feet (91-122 meters) below and to the east. This area is marked by steep, forested uplands which are dissected by numerous streams and drainageways flowing from the till plain towards the Red River of the North (e.g. Pembina River Gorge). Slope on the Loamy Savanna site ranges from 0 to 25 percent.
Table 2. Representative physiographic features
Landforms |
(1)
Moraine
(2) Escarpment |
---|---|
Runoff class | Low to high |
Flooding frequency | None |
Ponding frequency | None |
Elevation | 950 – 2,525 ft |
Slope | 25% |
Water table depth | 42 – 80 in |
Aspect | Aspect is not a significant factor |
Climatic features
MLRA 55A is considered to have a continental climate with cold winters and hot summers, low humidity, light rainfall, and much sunshine. Extremes in temperature are common and characteristic of MLRA 55A. The continental climate is the result of the location of this MLRA in the geographic center of North America. There are few natural barriers on the northern Great Plains, so air masses move unobstructed across the plains and account for rapid changes in temperature.
The average annual precipitation is 17 to 19 inches (432 to 483 millimeters). The normal average annual temperature is 36⁰ to 41⁰ F (2⁰ to 5⁰ C). January is the coldest month with an average low temperature of about ⁻ 3⁰ F (⁻19⁰ C). July is the warmest month with an average high temperature of about 80⁰ F (27⁰ C).
About 75 percent of the rainfall occurs as high-intensity, convective thunderstorms during the growing season. Winter precipitation is typically snow. The annual snowfall is 25 to 50 inches (635 to 1,270 millimeters). The frost-free period averages 101 days and ranges from 108 days to 92 days. The freeze-free period averages 124 days and ranges from 128 to 119 days.
Growth of native cool-season plants begins in mid-April and continues to mid-July. Native warm-season plants begin growth in late May and continue to the end of August. Green-up of cool-season plants can occur in September and October when adequate soil moisture is present.
Long-term climate data is lacking for Turtle Mountain, however, annual precipitation for the International Peace Garden averaged 27.7 inches (704 millimeters) from 1967-1970 while that for Boissevain, Manitoba averaged 17.1 inches (434 millimeters). Turtle Mountain likely has greater precipitation, cooler temperatures and less evapotranspiration than the adjacent plains.
Table 3. Representative climatic features
Frost-free period (characteristic range) | 92-109 days |
---|---|
Freeze-free period (characteristic range) | 119-128 days |
Precipitation total (characteristic range) | 17-19 in |
Frost-free period (actual range) | 88-112 days |
Freeze-free period (actual range) | 116-132 days |
Precipitation total (actual range) | 17-20 in |
Frost-free period (average) | 101 days |
Freeze-free period (average) | 124 days |
Precipitation total (average) | 18 in |
Figure 2. Monthly precipitation range
Figure 3. Monthly minimum temperature range
Figure 4. Monthly maximum temperature range
Figure 5. Monthly average minimum and maximum temperature
Figure 6. Annual precipitation pattern
Figure 7. Annual average temperature pattern
Climate stations used
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(1) CROSBY [USC00321871], Crosby, ND
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(2) BOWBELLS [USC00320961], Bowbells, ND
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(3) BOTTINEAU [USC00320941], Bottineau, ND
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(4) DRAKE 9 NE [USC00322304], Drake, ND
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(5) EDMORE 1NW [USC00322525], Edmore, ND
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(6) GRANVILLE [USC00323686], Granville, ND
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(7) HANSBORO 4 NNE [USC00323963], Hansboro, ND
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(8) LANGDON EXP FARM [USC00324958], Langdon, ND
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(9) LEEDS [USC00325078], Leeds, ND
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(10) MINOT EXP STN [USC00325993], Minot, ND
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(11) MOHALL [USC00326025], Mohall, ND
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(12) ROLLA 1NE [USC00327664], Rolla, ND
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(13) RUGBY [USC00327704], Rugby, ND
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(14) TOWNER 2 NE [USC00328792], Towner, ND
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(15) UPHAM 3 N [USC00328913], Upham, ND
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(16) VELVA 3NE [USC00328990], Velva, ND
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(17) WESTHOPE [USC00329333], Westhope, ND
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(18) WILLOW CITY [USC00329445], Willow City, ND
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(19) DEVILS LAKE KDLR [USW00014912], Devils Lake, ND
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(20) MINOT INTL AP [USW00024013], Minot, ND
Influencing water features
Most areas of this site receive no significant additional water from a seasonal high water table or as run-on from adjacent slopes; typically, the site is in a run-off landscape position. Typically, the water table is below 4 feet during April through June and below 6 feet the remainder of the growing season. However, nearly level areas associated with wetter soils may have saturation as shallow as 3 feet early in the growing season. Surface infiltration is moderately slow to moderately rapid. Saturated hydraulic conductivity is moderately high in the subsoil. Water loss is through evapotranspiration and percolation below the root zone.
Soil features
Soils associated with Loamy Savannah are in the Alfisol and Mollisol orders. The Alfisols are classified further as Mollic Hapludalfs. The Mollisols are classified further as Alfic Argiudolls. Typically, these soils formed in fine-loamy till; however, some may have weathered shale beds below a depth of 5 feet. The common features of soils in this site are the medium textures throughout the profile and soil properties which indicate periodic forested and prairie conditions.
These indicators occur in the subsurface and upper subsoil layers. In some areas there is a thin albic (gray, leached) horizon with an argillic horizon immediately below. More commonly, there is an argillic horizon with uncoated sand grains or grayish silt coats on the ped surfaces. Where not cleared for cultivation, soils in the Loamy Savannah site commonly have a thin layer of undecomposed organic materials at the surface.
These soils, typically, are well drained, but some are moderately well drained; redoximorphic features, where present, are deeper than 3.5 feet. Typically, the surface texture of the mineral soil is loam, but sandy loam and coarse sandy loam are included. The subsoil is, typically, clay loam (< 35% clay) but loam and sandy clay loam are included.
Soil salinity is none to very slight (E.C. <2 dS/m). Sodicity is none or very low (SAR <1). Soil reaction is slightly acid to neutral (pH 6.1 to 7.3) in the surface soil; slightly acid to slightly alkaline (pH 6.1 to 7.8) in the subsoil; and slightly or moderately alkaline (pH 7.4 to 8.4) in the lower part of the soil. Calcium carbonate content is none in the surface and upper subsoil layers; it may increase to as much as 25 percent in the lower subsoil and substratum.
Major soil series correlated to the Loamy Savannah site are Bottineau and Waukon. Included in the site are some areas of Metigoshe soils (see Site Development and Testing Plan).
Access Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) for specific local soils information.
Table 4. Representative soil features
Parent material |
(1)
Till
(2) Outwash |
---|---|
Surface texture |
(1) Loam (2) Sandy loam (3) Coarse sandy loam |
Family particle size |
(1) Loamy (2) Clayey |
Drainage class | Moderately well drained to well drained |
Permeability class | Very slow to moderately rapid |
Depth to restrictive layer | 60 – 80 in |
Soil depth | 60 – 80 in |
Surface fragment cover <=3" | 5% |
Surface fragment cover >3" | 3% |
Available water capacity (0-40in) |
7 – 12 in |
Calcium carbonate equivalent (0-40in) |
25% |
Electrical conductivity (0-40in) |
2 mmhos/cm |
Sodium adsorption ratio (0-40in) |
1 |
Soil reaction (1:1 water) (0-40in) |
5.6 – 8.4 |
Subsurface fragment volume <=3" (Depth not specified) |
1 – 11% |
Subsurface fragment volume >3" (Depth not specified) |
3% |
Ecological dynamics
This ecological site description is based on nonequilibrium ecology and resilience theory and utilizes a State-and-Transition Model (STM) diagram to organize and communicate information about ecosystem change as a basis for management. The ecological dynamics characterized by the STM diagram reflect how changes in ecological drivers, feedback mechanisms, and controlling variables can maintain or induce changes in plant community composition (phases and/or states). The application of various management actions, combined with weather variables, impact the ecological processes which influence the competitive interactions, thereby maintaining or altering plant community structure.
The site developed under Northern Great Plains climatic conditions. The historical disturbance regime for the region included frequent fires, both natural and anthropogenic. Most fires, however, were anthropogenic fires set by Native Americans. Native Americans set fires in all months except perhaps January. These fires occurred in two peak periods, one from March-May with the peak in April and another from July-November with the peak occurring in October. Most of these fires were scattered and of small extent and duration. The grazing history would have involved grazing and browsing by elk, whitetail deer, and American bison.
This site may be characterized as a tension zone or ecotone between forest and grassland in areas around Devils Lake, the Pembina Escarpment, and along the escarpment of Turtle Mountain. Turtle Mountain lies roughly 600-800 feet (183-244 meters) above the surrounding plain. An orographic effect, in combination with other environmental factors, has resulted in the mountain supporting a mixed hardwood forest consisting primarily of quaking aspen, green ash, and bur oak. The surrounding plain, however, is grassland. Historically, disturbances by ungulates including elk, deer, and American bison, and particularly variations in precipitation and natural and anthropogenic fires, created a tension zone or ecotone along the escarpment of Turtle Mountain. The ecotone is where the Bottineau soils formed. As a result, the site likely would have supported a dynamic mix of wooded and grass dominated communities that shifted in response to the temporal and spatial variations in these disturbances. Similar topographical and ecological factors exist along the Pembina Escarpment, Pembina River Gorge, and in areas around Devils Lake. Unlike the Bottineau soils, the presence of an albic horizon in the Waukon and Metigoshe soils suggest they developed under a long-term forested state (see Site Development and Testing Plan).
The soils associated with the Loamy Savannah ecological site also supports the hypothesis of a vegetatively dynamic site because it has characteristics indicative of formation under both forested and grassland conditions (e.g., Bottineau series: Fine-loamy, mixed, superactive frigid Alfic Argiudolls). The Loamy Savannah ecological site typifies the escarpment of Turtle Mountain. Turtle Mountain may be characterized by the Upland Hardwood Forest ecological site which is largely composed of soil series formed under forested conditions (e.g., Kelvin: Fine, smectitic, frigid Chromic Vertic Hapludalfs and Rolla: Very-fine, smectitic, frigid Vertic Hapludalfs). Where grassland and forestland are intermingled, the grassland occurs on higher convex landscape position (ridgetops).
This ecological site has also been subject to varied amounts of timber harvesting since settlement. This harvesting was conducted by small commercial sawmills as well as harvesting for personal use. The effects of this harvesting on the structure and composition of the plant community may be quite variable depending upon the species harvested and the methodology.
Four vegetative states have been identified for the site (Reference, Native/Invaded, Grassland, and Go-Back). Within each state, one or more community phases have been identified. These community phases are named based on the more dominant and visually conspicuous species; they have been determined by study of historical documents, relict areas, scientific studies, and ecological aspects of plant species and plant communities. Transitional pathways and thresholds have been determined through similar methods.
State 1: Reference State represents the natural range of variability that dominated the dynamics of this ecological site prior to European influence. It is thought to have shifted temporally and spatially between woody vegetation and/or open grassland resulting from the variability in precipitation, fire, and other disturbances. Three community phases have been identified.
Since European influence, however, fires have been significantly reduced while other disturbances, such as timber harvesting and grazing by domestic livestock, have increased. As a result, the historical disturbance regime no longer exists; communities representing the Reference State are considered to no longer exist. Thus, the presence of exotic plants on the site precludes it from being placed in the Reference State. It must then be placed in one of the other states, commonly State 2: Native/Invaded State (T1A).
State 2: Native/Invaded State. This state forms outside the historical disturbance regime, largely because of the long-term elimination of fire and the introduction of exotic plants, particularly exotic cool-season grasses. The elimination of fire also allowed for an increase in tree density which reduced the Savannah-like appearance of State 1.0, thus resembling State 3.0 of the Upland Harwood Forest ecological site. This state may be described as a bur oak dominated woodland with green ash and quaking aspen as the principal associates. Kentucky bluegrass and smooth brome are the main cool-season exotic grasses.
Presently, the distribution of common buckthorn in MLRA 55A has been relatively limited. However, it is spreading and, due to its invasive nature and habit of displacing native understory species, is a threat to biodiversity. As a result, periodic monitoring for the species is recommended; if the plant is encountered, control measures implemented.
Clear cutting/brush management will lead to State 3: Grassland State (T2A). Clear cutting/brush management for annual cropping followed by cropland abandonment will lead to State 4: Go-Back State (T2B).
Colonization of the site by exotic species results in a transition from State 1: Reference State to State 2: Native/Invaded State (T1A). This transition was inevitable; it often resulted from colonization by exotic cool-season grasses (e.g., Kentucky bluegrass, smooth brome) which have been particularly and consistently invasive under extended periods of non-use or light grazing, and no fire. Other exotic plants (e.g., leafy spurge) are also known to invade the site.
Three community phases have been identified for this state; they are similar to the community phases in the Reference State but have now been invaded by exotic cool-season grasses. These exotic cool- season grasses can be expected to increase. As that increase occurs, native plant diversity declines. A decline in forb diversity can also be expected.
State 3: Invaded Grassland State. This state results from clearing of woody vegetation (regardless of technique) and perhaps followed by a successful seeding of the site to native and/or introduced grasses, with or without introduced legumes or native forbs. It is often composed of a mixture of native grasses and exotic cool-season grasses in association with both exotic and native forbs. A successful tree/shrub planting or secondary succession will lead to State 2: Native/Invaded State (R3A).
State 4: Go-Back State often results from cropland abandonment and consists of only one community phase. This weedy assemblage may include noxious weeds that need control. Initially, due to extensive bare ground and a preponderance of shallow rooted annual plants, the potential for soil erosion is high. Plant species richness may be high, but overall diversity (i.e., equitability) is typically low with the site dominated by a relatively small assemblage of species. Due to the lack of native perennials and other factors, restoring the site with the associated ecological processes is difficult.
A successful tree/shrub planting (forestry planting) or secondary succession will lead to State 2: Native/Invaded State (R4A) while a successful pasture or hayland planting or secondary succession will lead to State 3: Grassland State (R4B).
The following state and transition model diagram illustrates the common states, community phases, community pathways, and transition and restoration pathways that can occur on the site. These are the most common plant community phases and states based on current knowledge and experience; changes may be made as more data are collected. Pathway narratives describing the site’s ecological dynamics reference various management practices (e.g., prescribed grazing, prescribed burning, brush management, herbaceous weed treatment) which, if properly designed and implemented, will positively influence plant community competitive interactions. The design of these management practices will be site specific and should be developed by knowledgeable individuals; based upon management goals and a resource inventory; and supported by an ongoing monitoring protocol.
When the management goal is to maintain an existing plant community phase or restore to another phase within the same state, modification of existing management to ensure native species have the competitive advantage may be required. To restore a previous state, the application of two or more management practices in an ongoing manner will be required. Whether using prescribed grazing, prescribed burning, or a combination of both with or without additional practices (e.g., brush management), the timing and method of application needs to favor the native species over the exotic species. Adjustments to account for variations in annual growing conditions and implementing an ongoing monitoring protocol to track changes and adjust management inputs to ensure desired outcome will be necessary.
The plant community phase composition table(s) has been developed from the best available knowledge including research, historical records, clipping studies, and inventory records. As more data are collected, plant community species composition and production information may be revised.
State and transition model
More interactive model formats are also available.
View Interactive Models
Click on state and transition labels to scroll to the respective text
Ecosystem states
T1A | - | Introduction of exotic cool-season grasses, outside of historic disturbance regime |
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T2A | - | Clear cutting and brush management |
State 1 submodel, plant communities
1.1A | - | Long-term drought, fire return interval more frequent |
---|---|---|
1.1B | - | Long-term above average precipitation, fire return interval less frequent |
1.2A | - | Return to average growing conditions, fire return interval returns to normal |
1.3A | - | Return to average growing conditions, fire return interval returns to normal |
State 2 submodel, plant communities
2.1A | - | Introduction of livestock grazing. Long-term light to moderate use |
---|---|---|
2.2B | - | Removal of livestock |
2.2A | - | Increased livestock grazing. Long-term season long heavy use |
2.3A | - | Long-term light to moderate use |
State 3 submodel, plant communities
State 4 submodel, plant communities
State 1
Reference State
The Reference State represents the historical natural range of variability that dominated the dynamics of this ecological site. Since European settlement, however, fires have been significantly reduced, while other disturbances such as timber harvesting and grazing by domestic livestock have increased. As a result, the historical disturbance regime no longer exists, and communities representing the Reference State are no longer present. On both temporal and special scales, this state would have historically supported woody vegetation and/or open grassland resulting from the variability in precipitation, fire, and other disturbances. The tree most characteristic of the wooded communities was bur oak, known for its fire and drought tolerance. Associated trees included quaking aspen and green ash. Common shrubs included both beaked hazel and American hazel, chokecherry, Saskatoon serviceberry, rose, and western snowberry. Graminoids were predominantly cool-season species, such as green needlegrass, needleandthread, western wheatgrass, bearded wheatgrass, prairie Junegrass, Canada wildrye, and sedges. Big bluestem, little bluestem, and blue grama were common associated warm season grasses. American vetch, veiny pea, Canada anemone, candle anemone, northern bedstraw, and blackeyed Susan constitute the more common forbs.
Characteristics and indicators. (i.e. Characteristics and indicators that can be used to distinguish this state from others). Because of changes in disturbances and other environmental factors (particularly the widespread occurrence of exotic species), the Reference State is considered to no longer exist.
Resilience management. (i.e. management strategies that will sustain a state and prevent a transition). If intact, the reference state should probably be managed with current disturbance regimes which has permitted the site to remain in reference condition as well as maintaining the quality and integrity of associated ecological sites. Maintenance of the reference state is contingent upon a monitoring protocol to guide management.
Community 1.1
Bur Oak/ Western Wheatgrass-Needlegrasses (Quercus macrocarpa/ Pascopyrum smithii-Nasella viridula-Hesperostipa comata)
Community Phase 1.1 is considered the Reference Plant Community upon which most interpretations are based. This community evolved with frequent fires and grazing/browsing by native ungulates. It may be described as an oak Savannah, consisting of bur oak and open grassland with perhaps scattered patches of woody vegetation. Associated trees and shrubs would include green ash, quaking aspen, American and beaked hazel, western snowberry, rose, chokecherry, Saskatoon serviceberry, and others. The grass component would have been predominantly cool-season (such as western wheatgrass, green needlegrass, and needle and thread) along with other cool-season graminoids (such as prairie Junegrass, Canada wildrye, bearded wheatgrass, and sedges). Warm-season grasses included little bluestem, big bluestem, and blue grama. American vetch, veiny pea, Canada anemone, candle anemone, northern bedstraw, and blackeyed Susan were common associated forbs.
Figure 8. Annual production by plant type (representative values) or group (midpoint values)
Table 5. Annual production by plant type
Plant type | Low (lb/acre) |
Representative value (lb/acre) |
High (lb/acre) |
---|---|---|---|
Grass/Grasslike | 1150 | 1700 | 2250 |
Shrub/Vine | 140 | 288 | 450 |
Tree | 25 | 158 | 300 |
Forb | 140 | 216 | 300 |
Total | 1455 | 2362 | 3300 |
Community 1.2
Western Wheatgrass-Needlegrasses/ Bur Oak (Pascopyrum smithii-Nasella viridula-Hesperostipa comata/ Quercus macrocarpa)
This community phase occurred during extended drought periods or periods of more frequent or intense fires compared to the conditions of Community Phase 1.1. The community may be described as a western wheatgrass-needlegrass dominated grassland with scattered small amounts of bur oak. Important associated graminoids would include prairie Junegrass, Canada wildrye, bearded wheatgrass, and sedges, as well as little and big bluestem and blue grama. American vetch, veiny pea, Canada anemone, candle anemone, northern bedstraw, and blackeyed Susan were common associated forbs.
Community 1.3
Bur Oak/ Wild Sarsaparilla/ Sedges (Quercus macrocarpa/ Aralia nudicaulis/ Carex spp.)
This community occurred during extended periods of long-term increased precipitation and lower fire frequency and/or intensity compared to the other community phases. This plant community phase is dominated by bur oak with associates of green ash and perhaps quaking aspen while wild sarsaparilla, early meadow-rue, and yellow vetchling make up the bulk of the forb component. Graminoids are largely limited to sedges and rough ricegrass. Hazel (American and beaked) and chokecherry are present where areas of tree canopy gaps allow enough sunlight for these species to flourish.
Pathway 1.1A
Community 1.1 to 1.2
Plant Community Phase 1.1 to 1.2 occurred during extended drought periods or periods of more frequent and/or intense fires, sufficient to cause significant mortality and reduction in recruitment of woody species. As a result, vegetation shifted to a more open grassland. Bur oak, however, known for its drought tolerance, remained a conspicuous but rather minor component of the community.
Pathway 1.1B
Community 1.1 to 1.3
Plant Community Phase 1.1 to 1.3 occurred during extended periods of increased precipitation or less frequent and/or intense fires sufficient to shift the community from bur oak savanna to a bur oak dominated woodland with a hazel understory. Due to increased shading the herbaceous understory is predominantly shade tolerant forbs with few graminoids.
Pathway 1.2A
Community 1.2 to 1.1
Plant Community Phase 1.2 to 1.1 would have occurred during extended periods of increased precipitation or less frequent/intense fires compared to that of 1.2, sufficient to enable bur oak to increase in importance relative to grassland.
Pathway 1.3A
Community 1.3 to 1.1
Plant Community Phase 1.3 to 1.1 occurs during an extended period of decreased precipitation or more frequent/intense fires sufficient to enable a significant decrease in woody species and corresponding increase in the grassland, creating a bur oak savanna.
State 2
Native/Invaded State
This state forms outside the historical disturbance regime, largely because of the long-term elimination of fire sufficient to establish a bur oak dominated forest similar to that of 1.3, and the introduction of exotic cool-season grasses. This state may be described as a bur oak dominated woodland with green ash and quaking aspen as the principal associates. The shrub component may include American and beaked hazel, chokecherry, Saskatoon serviceberry, rose, and snowberry. Kentucky bluegrass and/or smooth brome are the main cool-season exotic grasses, while the native graminoid component is largely limited to Sprengel’s sedge and perhaps rough ricegrass. Common associated forbs include wild sarsaparilla, early meadow-rue, veiny pea, and starry false lily of the valley. Presently the distribution of common buckthorn in MLRA 55A has been relatively limited. However, it is spreading, and due to its invasive nature and habit of displacing native understory species is a threat to biodiversity. As a result, periodic monitoring for the species is recommended, and if the plant is encountered, control measures implemented.
Characteristics and indicators. The presence of trace amounts of exotic cool-season grasses. The presence of exotic biennial or perennial forbs (e.g. common dandelion, red clover, white clover, and black medic may not, on their own, indicate a transition from State 1: Reference State to State 2: Native/Invaded State but may facilitate that transition.
Resilience management. The invasion of these exotic grasses is associated with long-term elimination of fire allowing bur oak and green ash to dominate. These fire tolerant species will not be significantly impacted by implementation of prescribed fire. To maintain State 2.0 Native/Invaded State prescribed fire and prescribed grazing should be implemented.
Community 2.1
Bur Oak-Green Ash/Wild Sarsaparilla/Sedges (Quercus macrocarpa-Fraxinus pennsylvanica/Aralia nudicaulis/Carex spp.)

Figure 9. Community Phase 2.1. Note wild sarsaparilla understory.
This community may be described as a bur oak-green ash forest with a canopy coverage of around 80-90%. Hazel and other shrubs (such as chokecherry, Saskatoon serviceberry, rose, and snowberry) may be present but not prominent components of the community. Exotic cool season grasses, largely Kentucky bluegrass and/or smooth brome, have been introduced to the community while the native herbaceous understory is largely composed of wild sarsaparilla and sedges (e.g., Sprengel’s, Pennsylvania).
Community 2.2
Bur Oak-Green Ash/Hazel/Sedges/Exotic Grasses Quercus macrocarpa-Fraxinus pennsylvanica/Corylus spp./Carex spp./Exotic Cool-Season Grasses)

Figure 10. Community Phase 2.2. Note open canopy allows for shrub and herbaceous understory.

Figure 11. Community Phase 2.2. Note hazel understory and livestock trailing and Kentucky bluegrass.
This community is similar to community phase 2.1 with the development of a shrub component composed largely of American and beaked hazel along with chokecherry and Saskatoon serviceberry in response to long-term, light to moderate grazing by livestock. Shorter shrubs, such as snowberry and rose, may also be prominent. The main native graminoids are sedges (e.g., Sprengel’s, Pennsylvania); however, exotic cool-season grasses, such as Kentucky bluegrass and smooth brome, are also prominent species.
Community 2.3
Bur Oak-Green Ash/Exotic Cool-Season Grasses (Quercus macrocarpa-Fraxinus pennsylvanica/Exotic Cool-Season Grasses)

Figure 12. Community Phase 2.3. : Bur Oak-Green Ash/Exotic Grasses. Note open canopy and over grazing removes shrubs allows for exotic cool-season grasses and forbs to dominate the herbaceous understory.
Long-term, season-long heavy grazing has eliminated the recruitment of trees and shrubs. Exotic grasses and forbs dominate the herbaceous component. This community phase may be characterized as a sparse stand of bur oak and green ash dominated woodland with an herbaceous understory dominated by exotic cool season grasses in response to long-term, season-long grazing by livestock. Recruitment of trees and shrubs has been severely reduced or eliminated. The herbaceous component is largely composed of Kentucky bluegrass, smooth brome, and perhaps creeping bentgrass. The forb component is also dominated by exotics (such as black medic, white clover, red clover, dandelion, and plantain).
Pathway 2.1A
Community 2.1 to 2.2


Community Phase 2.1 to 2.2 occurs with introduction of long-term, light to moderate grazing by domestic livestock during which time a distinct shrub layer composed of hazel forms and cool season exotic grasses increase.
Pathway 2.2B
Community 2.2 to 2.1


Community Phase Pathway 2.2 to 2.3 occurs with removal of livestock resulting in the reduction of hazel, an increase in wild sarsaparilla, and a decrease in the importance of exotic cool-season grasses.
Pathway 2.2A
Community 2.2 to 2.3


Community Phase Pathway 2.2 to 2.1 occurs when herbivory and associated disturbances associated with long-term, season-long heavy grazing by livestock severely reduces or eliminates recruitment of woody species, opens-up the woody species canopy, and may eventually eliminate the taller and weaker stemmed shrubs. Herbaceous exotic grasses and forbs become predominant.
Pathway 2.3A
Community 2.3 to 2.2


Community Phase Pathway 2.3 to 2.2 occurs with prescribed gazing which may lead to an increase in native herbaceous species, particularly wild sarsaparilla. The use of prescribed burning may need to be considered. Recruitment of woody species also increases.
State 3
Invaded Grassland State
This state results from clearing of woody vegetation on the site regardless of technique, and perhaps followed by a successful seeding of the site to native and/or introduced grasses, with or without introduced legumes or native forbs.
Characteristics and indicators. The plant community is a result of successful woody vegetation clearing or after pasture and hayland or rangeland planting. Exotic grasses, native grasses, exotic legumes, and or native forbs are used for grazing or forage production.
Resilience management. To slow or limit the invasion woody species, it is imperative that managerial options (e.g. prescribed grazing, prescribed burning) be carefully constructed and evaluated with respect to that objective). Grazing management should be applied that enhances the competitive advantage of native grass and forb species. This may include: (1) grazing when exotic cool-season grasses are actively growing and native cool-season grasses are dormant; (2) applying proper deferment periods allowing native grasses to recover and maintain or improve vigor; (3) adjusting overall grazing intensity to reduce excessive plant litter (above that needed for rangeland health indicator #14 – see Rangeland Health Reference Worksheet); (4) incorporating early heavy spring utilization which focuses grazing pressure on exotic cool-season grasses and reduces plant litter provided that livestock are moved when grazing selection shifts from exotic cool-season grasses to native grasses. Prescribed burning should be applied in a manner that maintains or enhances the competitive advantage of native grass and forb species. Prescribed burns should be applied as needed to adequately reduce/remove excessive plant litter and maintain the competitive advantage for native species. Timing of prescribed burns (spring vs. summer vs. fall) should be adjusted to account for differences in annual growing conditions and applied during windows of opportunity to best shift the competitive advantage to the native species.
Community 3.1
Exotic Cool-Season Grasses-Native Grasses/Exotic Legumes/Native Forbs
This community phase can be quiet variable. It may result from clear cutting/brush management via T2A (perhaps followed by a successful pasture or hayland planting). It may also result from a successful pasture or hayland planting with prescribed burning and prescribed grazing via R4B. Regardless of origin, the use of prescribed grazing, prescribed burning, haying, and/or the use of herbicides will likely be necessary to achieve management objectives.
State 4
Go-Back State
This state typically results from the abandonment of cropland, hayland, or residences/farmsteads. Vegetation is typically dominated by Kentucky bluegrass and smooth brome. Common associates include western snowberry, wild rose, northern bedstraw, common dandelion, Canada goldenrod, common yarrow, and Canada thistle. Sprouts from adjacent stands of aspen or beaked hazel often encroach onto the site, as well as seedlings of adjacent green ash.
Characteristics and indicators. Tillage has destroyed the native plant community, altered soil structure and biology, reduced soil organic matter, and resulted in the formation of a tillage induced compacted layer which is restrictive to root growth. Noxious weeds, if present, will need to be managed.
Resilience management. Continued tillage will maintain the state. Control of noxious weeds will be required.
Community 4.1
Annual/Pioneer-Perennial/Exotic Herbaceous Plants/Shrubs
This community phase is highly variable depending on the level and duration of disturbance related to the T2B and T5A transitional pathways. In this MLRA, the most probable origin of this phase is cropland abandonment or forestland clearing. This plant community will initially include a variety of annual forbs and grasses, including noxious weeds (e.g. Canada thistle) which may need control.
State 5
Any Plant Community
This plant community is most commonly associated with the cessation of cropping without the benefit of pasture/forest seeding or planting, resulting in a “go-back” situation
Transition T1A
State 1 to 2
This is the transition from State 1: Reference State to State 2: Native/Invaded State due to the introduction and establishment of exotic cool-season grasses. This transition is partially attributable to decades of fire suppression and other environmental factors outside the historical disturbance regime.
Constraints to recovery. Current knowledge and technology will not facilitate a successful restoration to Reference State.
Transition T2A
State 2 to 3
This transition from State 2: Native/Invaded State to State 3: Grassland State may be initiated by the clearing cutting/brush management and allowing grasses and other herbaceous vegetation to dominate site.
Constraints to recovery. Labor and financial cost of removal/control of woody species. Exotic herbaceous species, resprouting shrubs and stumps, and annual/pioneering exotics will quickly populate the site.
Transition T2B
State 2 to 4
This transition from State 2: Native/Invaded State to State 4: Go-Back State may be initiated by the clearing of the woody vegetation and stump removal for annual cropping followed by cropland abandonment.
Constraints to recovery. Labor and financial cost of removal/control of woody species to cropland will be dependent on the conversion duration. Time constraints and cost factors make restoration improbably. Technology limitations will also play a role.
Restoration pathway R3A
State 3 to 2
This restoration pathway from State 3: Grassland State to State 2: Native/Invaded State may be accomplished with a successful forestry planting or secondary succession.
Context dependence. Labor, time, and expense, along with long term management needs via forest plantings may limit success.
Restoration pathway R4A
State 4 to 2
This restoration from State 4: Go-Back State to State 2: Native/Invaded State may be initiated when a forest planting is conducted, or secondary succession occurs to restore the Native/Invaded
Context dependence. Labor, time, and expense, along with long term management needs via R4A may limit success.
Restoration pathway R4B
State 4 to 3
This restoration from State 4: Go-Back State to State 3: Grassland State may be initiated when a successful pasture or hayland planting is completed. Prescribed grazing and/or prescribed burning will be necessary to complete the restoration.
Context dependence. A successful pasture and hayland or range planting will include proper seedbed preparation, weed control (both prior to and after the planting), selection of adapted native species, and proper seeding technique. Management (e.g. prescribed grazing, prescribed burning) during and after establishment must be applied in a manner that maintains the competitive advantage for the seeded species. The method or methods of herbaceous weed treatment will be site specific to each situation; but generally, the goal would be to apply the pesticide, mechanical control or biological control - either singularly or in combination - in a manner that shifts the competitive advantage from the targeted species to the native grasses and forbs. The control method(s) should be as specific to the targeted species as possible to minimize impacts to non-target species.
Restoration pathway T5A
State 5 to 4
his transition from any plant community to State 4: Go-Back State. It is most commonly associated with the cessation of cropping without the benefit of range planting, resulting in a “go-back” situation. Soil conditions can be quite variable on the site, in part due to variations in the management/cropping history (e.g., development of a tillage induced compacted layer (plow pan), erosion, fertility, and/or herbicide/pesticide carryover). Thus, soil conditions should be assessed when considering restoration techniques.
Additional community tables
Table 6. Community 1.1 plant community composition
Group | Common name | Symbol | Scientific name | Annual production (lb/acre) | Foliar cover (%) | |
---|---|---|---|---|---|---|
Grass/Grasslike
|
||||||
1 | Cool-Season Grasses | 144–1725 | ||||
western wheatgrass | PASM | Pascopyrum smithii | 29–575 | – | ||
green needlegrass | NAVI4 | Nassella viridula | 29–575 | – | ||
needle and thread | HECO26 | Hesperostipa comata | 29–288 | – | ||
slender wheatgrass | ELTRS | Elymus trachycaulus ssp. subsecundus | 29–144 | – | ||
prairie Junegrass | KOMA | Koeleria macrantha | 29–144 | – | ||
Canada wildrye | ELCA4 | Elymus canadensis | 29–144 | – | ||
2 | Warm-Season Grasses | 29–719 | ||||
big bluestem | ANGE | Andropogon gerardii | 29–288 | – | ||
little bluestem | SCSC | Schizachyrium scoparium | 29–144 | – | ||
blue grama | BOGR2 | Bouteloua gracilis | 29–144 | – | ||
prairie sandreed | CALO | Calamovilfa longifolia | 29–144 | – | ||
3 | Other Native Grasses | 29–288 | ||||
Grass, perennial | 2GP | Grass, perennial | 0–290 | – | ||
4 | Grass-Likes | 29–144 | ||||
sedge | CAREX | Carex | 29–144 | – | ||
Forb
|
||||||
5 | Forbs | 144–288 | ||||
candle anemone | ANCY | Anemone cylindrica | 29–288 | – | ||
American vetch | VIAM | Vicia americana | 29–144 | – | ||
veiny pea | LAVE | Lathyrus venosus | 29–144 | – | ||
Canadian anemone | ANCA8 | Anemone canadensis | 29–144 | – | ||
northern bedstraw | GABO2 | Galium boreale | 29–144 | – | ||
blackeyed Susan | RUHI2 | Rudbeckia hirta | 29–144 | – | ||
Forb (herbaceous, not grass nor grass-like) | 2FORB | Forb (herbaceous, not grass nor grass-like) | 29–144 | – | ||
wild sarsaparilla | ARNU2 | Aralia nudicaulis | 29 | – | ||
Shrub/Vine
|
||||||
6 | Shrubs | 144–431 | ||||
hazelnut | CORYL | Corylus | 144–431 | – | ||
Saskatoon serviceberry | AMAL2 | Amelanchier alnifolia | 29–144 | – | ||
chokecherry | PRVI | Prunus virginiana | 29–144 | – | ||
Woods' rose | ROWO | Rosa woodsii | 29–144 | – | ||
western snowberry | SYOC | Symphoricarpos occidentalis | 29–144 | – | ||
hawthorn | CRATA | Crataegus | 29–144 | – | ||
Shrub (>.5m) | 2SHRUB | Shrub (>.5m) | 29–144 | – | ||
Tree
|
||||||
7 | Trees | 29–288 | ||||
bur oak | QUMA2 | Quercus macrocarpa | 29–144 | – | ||
green ash | FRPE | Fraxinus pennsylvanica | 29–144 | – | ||
quaking aspen | POTR5 | Populus tremuloides | 29–144 | – |
Interpretations
Animal community
Animal Community – Wildlife Interpretations
Landscape:
The MLRA 55A landscape is characterized by mostly nearly level to gently rolling till plains with some steep slopes adjacent to streams. The MLRA includes areas of kettle holes, kames, and moraines. MLRA 55A is considered to have a continental climate with cold winters and hot summers, low humidity, light rainfall, and much sunshine. Extremes in temperature are common and characteristic of MLRA 55A. This area supports mid- to tall-grass prairie vegetation with quaking aspen, bur oak, green ash, and willow species growing on the higher elevations in Turtle Mountain, on moraines in proximity south of Devils Lake, Pembina River Gorge, and various drainageways throughout the MLRA. Numerous depressional wetlands are ringed with quaking aspen. Complex, intermingled ecological sites create diverse grass/shrub land habitats interspersed with varying densities of linear, slope, depressional, and in-stream wetlands associated with headwater streams and tributaries of the Mouse and Pembina Rivers. MLRA 55A is located entirely within North Dakota and within the boundaries of the Prairie Pothole Region. The primary land use is cropland. Glacial Lake Souris and the Devils Lake Basin are known for exceptional fertility with major crops including corn, canola, soybeans, and small grains. Together, these two areas make up 73% of the MLRA (Glacial Lake Souris 5500 mi2, 43%; and the Devils Lake Basin 3810 mi2, 30%).
Turtle Mountain (1000 mi2 of which 405 mi2 are found in America), in the north-central part of the MLRA on the Canadian border, is approximately 1,950 to 2,541 feet (595 to 775 meters) in elevation, rising approximately 600 to 800 feet (150 meters) above the adjacent till plain. Home to an extensive forest of quaking aspen, bur oak, green ash, and willows, it has an understory of beaked hazel, with associates of chokecherry, Saskatchewan serviceberry, downy arrowwood, and rose. Turtle Mountain comprises the largest area of quaking aspen forest in North Dakota.
The Pembina Escarpment extends from the Canadian border southeast to Walhalla where the Pembina River enters the floor of the Red River Valley in MLRA 56. Mainly found on steep slopes along the Pembina River, the Pembina Gorge is in a rugged and sheltered setting with bur oak, green ash, cottonwood, and American elm. Encompassing approximately 12,500 acres, the Pembina Gorge is one of the largest uninterrupted blocks of woodlands in North Dakota. This segment of the Pembina River is the longest segment of unaltered river valley in the North Dakota.
Two major Hydrologic Unit Areas make up this MLRA. 56% of the MLRA drains into the Mouse (also known as Souris) River while 44% drains into the Red River via the Pembina or into Devils Lake (out-letting to Sheyenne River via a pump, pipeline, canal system). The North Dakota portion of the Mouse River watershed is in this MLRA. The Mouse River basin drains nearly 23,600 square miles and has a long history of flooding.
By the mid-19th century, over 75% of the MLRA had been converted from mid- to tall-grass prairie or woodland to annual crop production. To alleviate crop production loss from wetlands and overland flow, a system of shallow surface ditches, judicial ditches, and road ditches removes surface water in spring and during high rainfall events. Tile drainage systems have been or are being installed extensively throughout MLRA 55A for sub-surface field drainage to enhance annual crop production.
Historic Communities/Conditions within MLRA 55A:
The northern tall- and mixed-grass prairie along with the quaking aspen forest were disturbance-driven ecosystems with fire, herbivory, and climate functions as the primary ecological drivers - either singly or often in combination. American bison roamed MLRA 55A wintering along the Mouse River and migrating through MLRA 55A into MLRAs 56 and 55B. Many species of grassland birds, small mammals, insects, reptiles, amphibians, elk, moose, pronghorn and large herds of American bison were historically among the inhabitants adapted to this region. Roaming herbivores, as well as several small mammal and insect species, were the primary consumers linking the grassland resources to large predators such as the wolf, American black bear, grizzly bear, and smaller carnivores such as the coyote, bobcat, red fox, and raptors. Extirpated species include free-ranging American bison and gray wolf (breeding). Extinct is the Rocky Mountain locust.
Present Communities/Conditions within MLRA 55A:
This area supports natural prairie vegetation characterized by western wheatgrass, green needlegrass, needle and thread, and blue grama. Little bluestem is an important species on the more sloping and shallower soils. Prairie cordgrass, northern reedgrass, big bluestem, and wheat sedge are important species on soils with higher water tables. Western snowberry, leadplant, and prairie rose are commonly interspersed throughout the area. Native forests occur in Turtle Mountain, Pembina Gorge, moraines south of Devils Lake, woody draws, scattered tracts along the Mouse River, and in the sand dunes in west central region of the MLRA.
Over 75% of MLRA 55A has been converted to annual crop production. European influence has impacted remaining grassland, forestland, and shrubland by domestic livestock grazing, elimination of fire, tree harvest, removal of surface and subsurface hydrology via artificial drainage, and other anthropogenic factors influencing plant community composition and abundance.
Hydrological manipulation is extensive throughout the MLRA. Extensive wetland and subsurface tile drainage have taken place. Ephemeral and intermittent streams and the Mouse River have been straightened - removing sinuosity, creating isolated oxbows, and converting riparian zones to annual crop production. These anthropogenic impacts have reduced flood water detention and retention on the landscape. The results have been increasing storm water runoff sediment and nutrient loading impacting the Mouse and Des Lacs Rivers and their tributaries along with Devils Lake and other lakes within the MLRA. The installation of instream structures has reduced aquatic species movement within the MLRA. Two large dams in Saskatchewan, Canada (Rafferty on the Mouse River and the Alameda on Moose Mountain Creek, a major tributary to the Mouse River) were built, in part, to reduce flood peaks on the Mouse River. In addition, three USFWS National Wildlife Refuges were created by building two low-head dams on the Mouse River and one on the Des Lacs River in North Dakota. Numerous low-head dams are located on the Mouse and Des Lacs Rivers in North Dakota. The Eaton Irrigation Project low-head dam, located in the vicinity of Towner, North Dakota, provides flood irrigation to approximately 6,700 acres of hayland and pastureland.
The loss of the American bison and fire, as primary ecological drivers, greatly influenced the character of the remaining native plant communities and the associated wildlife moving towards a less diverse and more homogeneous landscape. Annual cropping is the main factor contributing to habitat fragmentation, reducing habitat quality for area-sensitive species. These influences fragmented the landscape, reduced or eliminated ecological drivers (fire), and introduced exotic species including smooth brome, Kentucky bluegrass, and leafy spurge further impacting plant and animal communities.
Included in this MLRA are over 121,000 acres of National Wildlife Refuges and over 77,000 acres of waterfowl production areas owned and managed by the United States Fish and Wildlife Service. White Horse Hill National Game Preserve is a 1,674-acre national wildlife refuge sitting on the south shores of Devils Lake, about 10 miles south of the city of Devils Lake. Numerous state-owned parks, state wildlife management areas, North Dakota Forest Service and Department of Trust Lands are found in the MLRA. Wakopa Wildlife Management Area is the largest WMA covering approximately 6,739 acres.
Some characteristic wildlife species in this area are:
Birds: Common loon, common goldeye, bufflehead, ruffed grouse, broad-winged hawk, alder flycatcher, mourning warbler, mallard, blue-winged teal, red-tailed hawk, American kestrel, killdeer, eastern and western kingbird, American crow, common yellowthroat, clay-colored sparrow, vesper sparrow, red-necked grebe, Savannah sparrow, downy and hairy woodpeckers, black-capped chickadee, white-breasted nuthatch, and brown-headed cowbird.
Mammals: Northern short-tailed shrew, water shrew, beaver, muskrat, mink, long-tailed weasel, American martin, fisher, white-tailed jackrabbit, snowshoe hare, Franklin’s ground squirrel, thirteen-lined ground squirrel, northern pocket gopher, plains pocket gopher, western harvest mouse, deer mouse, meadow vole, meadow jumping mouse, western jumping mouse, coyote, red fox, racoon, American badger, striped skunk, white-tailed deer, elk, moose, and woodchuck, red squirrel, porcupine, and northern flying squirrel.
Reptiles/Amphibians: American toad, Great Plains toad, northern leopard frog, chorus frog, tiger salamander, plains garter snake, smooth green snake, wood frog, and common garter snake.
Presence of wildlife species is often determined by ecological site characteristics including grass and forb species, tree and shrub species, hydrology, aspect, and other associated ecological sites. The home ranges of a majority species are usually larger than one ecological site or are dependent on more than one ecological site for annual life requisites. Ecological sites offer different habitat elements as the annual life requisites change. Habitat improvement and creation must be conducted within the mobility limits of a known population for the species.
Insects play an important role providing ecological services for plant community development. Insects that are scavengers or aid in decomposition provide the food chain baseline sustaining the carnivorous insects feeding upon them. Many insects provide the ecological services necessary for pollination, keeping plant communities healthy and productive. Insects provide a protein food source for numerous species including grassland-nesting birds, woodpeckers, woodland edge and interior species and their young. Extensive use of insecticides for specialty crops such as soybeans, corn, and other crops has greatly reduced insects within this MLRA.
Species of Concern within MLRA 55A:
The following is a list of species considered “species of conservation priority” in the North Dakota State Wildlife Action Plan (2015) and “species listed as threatened, endangered, or petitioned” under the Endangered Species Act within MLRA 55A at the time this section was developed:
Invertebrates: Dakota skipper, monarch butterfly, and regal fritillary. Within the MLRA, the United States Fish and Wildlife Service lists 5 areas (in Rolette and McHenry Counties) as critical habitat for the Dakota skipper.
Birds: American avocet, American bittern, American kestrel, American white pelican, Baird’s sparrow, bald eagle, black tern, black-billed cuckoo, bobolink, canvasback, chestnut-collared longspur, ferruginous hawk, Franklin’s gull, grasshopper sparrow, horned grebe, LeConte’s sparrow, lesser scaup, loggerhead shrike, marbled godwit, Nelson’s sparrow, northern harrier, northern pintail, piping plover, sharp-tailed grouse, short-eared owl, Sprague’s pipit, Swainson’s hawk, upland sandpiper, western meadowlark, whooping crane, willet, Wilson’s phalarope, and yellow rail.
Mammals: American martin, Arctic shrew, big brown bat, gray fox, little brown bat, northern long-eared bat, plains pocket mouse, pygmy shrew, Richardson’s ground squirrel, river otter, and Townsend’s big-eared bat.
Amphibians/Reptiles: Canadian toad, common snapping turtle, plains hog-nosed snake, and smooth green snake.
Fish: Finescale dace, hornyhead chub, largescale stoneroller, logperch, northern pearl dace, and trout-perch.
Mussels: Black sandshell, creek heelsplitter, creeper, mapleleaf, and pink heelsplitter.
Grassland and Woodland Management for Wildlife in the MLRA 55A
Management activities within the community phase pathways impact wildlife but are essential for maintenance of healthy grassland ecosystems. Community phase, transitional, and restoration pathways are keys to long-term management within each State and between States. Timing, intensity, and frequency of these inputs can have dramatic positive or negative effects on local wildlife species. Ranchers and other land managers must always consider the long-term beneficial management effects of grassland and woodland resources in comparison to typically short-term negative effects to the habitats of individual species.
Ecological sites occur as intermingled complexes on the landscape with gradual or sometimes abrupt transitions. Rarely do ecological sites exist in large enough acreage to manage independently for wildlife. Conversion to annual cropping and fragmentation due to transportation and electrical transmission corridors and to rural housing are main causes of fragmentation. This MLRA supports ecological sites that are dominated by woody vegetation and can be located adjacent to ecological sites that support tall- to mid-statured grasses (Thin Loamy/Shallow Loamy) or are adjacent to ecological sites that support wetland vegetation (Shallow Marsh and Wet Meadow).
Management of these ecological site complexes challenges managers to properly manage the entire landscape. A management strategy for one ecological site may negatively impact an adjacent site. For example, grazing Upland Hardwood Forest or Loamy Savanna ecological sites along with herbaceous dominated Loamy Overflow ecological sites may degrade one site by under-use, favoring woody vegetation or increasing exotic cool-season grasses.
Life requisites and habitat deficiencies are determined for targeted species. Deficiencies need to be addressed along community phase, transitional, and restoration pathways as presented in specific state-and-transition models. Ecological sites should be managed and restored within the site’s capabilities to provide sustainable habitat for targeted species or species guilds. Managers also need to consider vegetative associations provided by adjacent/intermingled ecological sites for species with home ranges or life requisites that may not be provided by one ecological site. Understanding specific grassland species’ sensitivity to woody encroachment and preferred vegetative structure enables managers to determine which grassland-nesting bird species will avoid grassland habitats adjacent to Upland Hardwood Forest or Loamy Savanna ecological sites or woody dominated, Plant Community Phase 5, Loamy ecological site.
Many passerine species utilize MLRA 55A as a major migratory travel corridor. Grassland species sensitive to woody associations during nesting and brooding may utilize the woodier fragmented sites such as the Wooded State 5.0 in the Loamy ecological site during migration.
Grassland-nesting birds use various grass heights for breeding, nesting, foraging, or winter habitat. While most species use varying heights, many have a preferred vegetative stature height or sensitivity to woody vegetation. Understanding the sensitivity of grassland species to woody vegetation and preferred vegetative structure enables managers to determine which grassland-nesting bird species avoid grassland habitats adjacent to Upland Hardwood Forest or Loamy Savanna ecological sites.
The following chart provides sensitivity to woody vegetation and preferred vegetative stature heights. To see the chart please follow the hyperlink:
https://efotg.sc.egov.usda.gov/references/public/ND/55A_Loamy_Savannah_Narrative_FINAL_Ref_FSG.pdf
Loamy Savanna Wildlife Habitat Interpretation:
Loamy Savanna ecological sites are located on moraines (Turtle Mountain and south of Devils Lake), and escarpments (Pembina Gorge). Loamy Savanna ecological sites are a tension zone. No significant water table or surface run-on influencing vegetation production occurs on this site. Associated ecological sites include Limy Subirrigated, Loamy Overflow, Thin Loamy, Shallow Marsh, and Upland Hardwood Forest. Loamy Savanna sites are located adjacent to wetlands, grasslands (native and introduced), and cropland.
Dependent upon the density of trees and shrubs, Loamy Savanna habitat features and components support woodland edge and interior birds and other wildlife species to meet their life requisites. Grassland-nesting birds avoid these ecological sites unless converted to herbaceous vegetation. Grassland-nesting birds that commonly avoid woody vegetation may have their habitat needs met depending on the degree of woody vegetation. They may also avoid adjacent ecological sites dominated by grassland vegetation when located in juxtaposition with woody vegetation. A reduction in nesting success by grassland nesting birds is likely to occur due to an increase in avian predation on adjacent herbaceous sites within or adjacent to Loamy Savanna ecological sites. These sites provide for many migratory passerines and year-round habitat for ruffed grouse and excellent winter cover for eastern screech owl, great horned owl, wild turkey, and non-migrating passerine birds such as black-capped chickadee and white-breasted nuthatch.
These forested sites provide excellent loafing, escape, and winter cover for small and large herbivores and excellent year-round habitat for American marten, snowshoe hare, elk, moose, and white-tailed deer.
Loamy Savanna ecological sites may be found in four plant community states (1.0 Reference State, 2.0 Invaded State, 3.0 Go-Back, and 4.0 Grassland state) within a local landscape. Multiple plant community phases exist within State 1.0 and 2.0. Today, these states occur primarily in response to precipitation (extended periods of above normal precipitation or drought), fire, grazing, clear cutting, hay or pasture plantings, non-use (lack of management), and other anthropogenic disturbances.
It is unlikely that plant communities with State 1.0 exist due to the invasion of exotic cool-season grasses. There is no known restoration pathway from any State back to State 1.0. Managers need to be aware of Community Pathways within State 2.0, if their goal is to maintain an oak savanna landscape.
Quaking aspen is generally not a major component of this site and is not typically managed for ruffed grouse.
1.0 Reference State – The Reference State no longer exists within MLRA 55A.
2.0 Invaded State:
Community Phase 2.1: Bur Oak-Green Ash/Wild Sarsaparilla/Sprengle’s Sedge: This plant community develops through Transition Pathway T1, due to introduction and establishment of exotic cool-season grasses such as Kentucky bluegrass and smooth brome and long-term elimination of fire. The transition to a bur oak dominated overstory with shade tolerant tree species such as green ash creates a closed canopy forest (80%-90%) with an understory of cool-season exotic grasses in conjunction with native wild sarsaparilla and Sprengle’s sedge. Shrub species such as chokecherry, American hazel, rose, Saskatoon serviceberry, and snowberry may be present but not prominent. Quaking aspen may still be present.
Invertebrates: Dense overstory of bur oak and green ash provide shade with little sunlight reaching flowering plants such as forbs and shrubs. Pollen and nectar sources are limited; day long shade limits use by pollinating insects. However, insects do play a role in maintaining the limited forb community and provide a forage base for woodland birds, reptiles, and rodents. Plant materials and dung in contact with mineral soil are used by lower trophic level consumers such as invertebrate decomposers, scavengers, shredders, predators, herbivores, dung beetles, and fungal feeders.
Loamy Savanna ecological sites provide habitat for a variety of butterflies. Forest openings are important areas for sunlight to reach the soil surface for forbs to produce pollen and nectar. Knutson and Post (1963) and Royer (2003) list several butterfly species associated with Turtle Mountain and found in Bottineau county, ND. Included are Arctic skipper, Hobomok skipper, roadside skipper, black swallowtail, tiger swallowtail, coral hairstreak, Edward’s hairstreak, banded hairstreak, stripped hairstreak, great spangled fritillary, Atlantis fritillary, mourning cloak, American painted lady, white admiral, Viceroy, northern pearly eye, and little wood satyr.
Birds: This plant community provides quality woodland edge and interior nesting, foraging, and escape habitats. The closed canopy provides excellent nesting opportunities for canopy nesters but limited habitat for shrub nesting birds. This site provides good hunting opportunities for woodland raptors and owls. The presence of woody plant species may increase mammalian and avian predation and may also increase brood parasitism by brown-headed cowbirds on adjacent grassland ecological sites.
Depending on the size of the plant community, bird species that occupy both woodland edge and interior habitats can benefit. These species include American crow, American goldfinch, American kestrel, American redstart, black-billed cuckoos, blacked-capped chickadee, blue jay, brown-headed cowbird, brown thrasher, eastern bluebird, eastern and western kingbird, eastern screech-owl, gray catbird, great horned owl, house wren, black-billed magpie, mourning dove, northern flicker, oven bird, red-eyed vireos, red-headed woodpecker red-tailed hawk, scarlet tanager, sharp-shinned hawk, wild turkey, and yellow warbler.
Older trees provide cavity nesting sites for forest birds. An increase in mast producing trees provide food for wild turkey, blue jays, and woodpeckers. Limited flowering shrubs provide insect populations for birds and their young and berries from late summer to early winter. Ruffed grouse use will be somewhat dependent upon the amount of shrub and sapling layer prevalent on the site.
Mammals: Trees and shrubs provide security and thermal cover used by elk and white-tailed deer for foraging, loafing, and rearing young-of-the-year. Multi-layer shrub/tree communities provide concealment protection from predators during parturition. Plant species provide highly nutritious forage during peak lactation, one of the most energy-demanding time periods of the year for female ungulates. Shrub and herbaceous cover may become limited, reducing thermal, protective, and escape cover for small and large herbivores including voles, mice, snowshoe hare, white-tailed deer, and elk. Hollow tree cavities provide denning and resting sites for American martens. Dead and mature trees provide cavities and loose bark for big brown bat, northern long-eared bat, and Townsend’s big-eared bat. Dependent upon adjacency to permanent water, beaver will use these sites for foraging and woody material for lodge building.
Amphibians and Reptiles: This ecological site provides foraging opportunities for the northern leopard frog and Canadian toad since this site is frequently found adjacent to Wet Meadow and Shallow Marsh ecological sites.
Community Phase 2.2: Bur Oak-Green Ash/Hazel spp./Sprengle’s Sedge/Exotic Grasses: Long-term, light to moderate domestic livestock grazing leads to the decline in vigor and increased mortality of forest canopy species. Reduction in shade allows for an increased shrub component of American hazel, chokecherry, Saskatoon serviceberry, rose, and western snowberry and an increase in exotic cool-season grasses. Continued long-term grazing may cause eventual loss of taller shrubs. Western snowberry and rose may become dominant.
Invertebrates: The decrease in shade allows an increase in flowering shrubs providing pollen and nectar sources for pollinating insects. Pollinator insect diversity will be increased with an increase in flowering shrubs. However, early- and mid-season flowering shrubs will be the main source of nectar and pollen. Late season pollen sources may be limited. Fly population associated with livestock production increase in association with livestock dung.
Birds: This site mainly will be used by woodland edge bird species such as American robin, house sparrow, brown-headed cowbird, etc. Livestock grazing will reduce forest canopy, limiting use by forest interior and edge nesting birds but will not open-up the canopy for use by grassland nesting birds. Use by ruffed grouse is limited due to the lack of quaking aspen.
Mammals: This site provides limited cover for both small and large mammals. Extensive grazing limits tree regeneration, opening up the forest canopy for invasion of cool-season exotic grass and exotic forbs. Depending on the degree of grazing, limited small mammal habitat may be available. Winter thermal cover is beginning to become limited for large ungulates.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 2.1.
Fish and Mussels: Soil compaction and trailing increases bare soil and weakens tree roots leading to increased runoff and erosion. Nutrient and sediment loading increase to adjacent waterbodies.
Community Phase 2.3: Bur Oak-Green Ash/Exotic Grasses: Long-term, season-long livestock grazing eliminates recruitment of trees and shrubs and allows for cool-season exotic grasses to dominate the herbaceous component of the site. A sparse stand of bur oak and green ash allow for a forb community dominated by exotics such as black medic, white clover, red clover, common dandelion, and plantain.
Invertebrates: Pollen and nectar sources transition from flowering shrubs found in Community Phase 2.2 to exotic forbs. Exotic forbs early- and mid-season bloom periods provide pollinating insects ample pollen and nectar sources during that time. Clovers will provide nectar and pollen for a diverse pollinator insect population; however, nectar and pollen sources will be limited during late season bloom period. Fly populations associated with livestock production increase in association with livestock dung.
Birds: Provides similar life requisites as Community Phase 2.2. Ruffed grouse use will be limited due to long-term grazing removing the shrub and tree sapling layer within this plant community.
Mammals: Loss of shrub canopy limits cover for both small and large mammals. Extensive grazing eliminates tree and shrub regeneration opening the forest canopy for invasion of cool-season exotic grass and exotic forbs. Long-term, season-long grazing remove small mammal cover. Winter thermal cover is limited to nonexistent for large ungulates.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 2.2.
Fish and Mussels: Soil compaction and trailing increases bare soil and weakens tree roots leading to increased runoff and erosion. Sod forming exotic grasses contribute to increased runoff, increasing nutrient and sediment loading to adjacent waterbodies.
3.0 Grassland State:
Community Phase 3.1 Exotic Grasses-Native Grasses/Exotic Legumes/Native Forbs: Successful establishment of native or tame species along Transition Pathway R4B results in an herbaceous grass and forb community in State 3.0. Depending on distance to existing forested areas, tree and shrub seedlings may become established. The response by wildlife species will be dependent upon the success of the planted grasses and forbs, vegetative stature, patch size, and management activities (such as prescribed burning, inter-seeding, haying, grazing, or noxious weed control).
4.0 Go-Back State:
Community Phase 4.1: Annual/Pioneer-Perennial/Exotic Herbaceous Plants/Shrubs: This plant community phase can have a variety of herbaceous and shrub species. It is mainly derived from abandoned cropland or hayland; but clear-cutting and brush management can also result in this plant community phase. Following cessation of disturbances, the resulting plant community is dominated by early pioneer annual and perennial plant species. Plant species composition and production are highly variable. A sapling tree and shrub component may be present. Weedy plants can provide pollinator habitat along with spring and summer cover for many mammals and birds and their young. Dense weed cover can keep soils moist, increasing insect presence. Tall vegetative stature provided by weeds such as marsh elder and ragweed offer thermal cover and seeds throughout winter.
Through successful seeding and management of tame or native species along Transition Pathway R4b, this plant community can transition to a Grassland State 3.0.
Animal Community – Grazing Interpretations:
This site is not particularly well suited to managed grazing by cattle, mainly because the dense tree and shrub canopy limit light penetration necessary for forage production. Furthermore, the dense hazel underbrush discourages livestock access. However, in combination with grass dominated sites, tame pastures, or other areas of herbaceous vegetation, the site may provide important seasonal forage (i.e. early and late season), loafing areas, thermal protection, and the like.
As a result, various efforts to increase forage production have been explored. For example, to increase forage production, 100 feet along the pasture perimeter fence is cleared; not only does this clearing increase forage production this also helps to reduce fence maintenance. Once cleared, the area may be seeded (grasses/legumes), or simply allowed to grow back. Depending upon vegetation and pasture size, this perimeter clearing may produce a major portion of the forage for livestock. However, invasion of these cleared areas by exotic grasses such as Kentucky bluegrass or smooth brome may be expected. These clearings may also be colonized by noxious weeds such as Canada thistle, absinth wormwood, and leafy spurge. As a result, weed control efforts may be necessary.
Invaded State is best managed for livestock production when existing States 3.0 Go-Back State and 4.0 Grassland State or other existing non-wooded sites are incorporated into a prescribed grazing plan. It is strongly recommended that stocking rates, days of grazing, and season of use are based on site-specific inventory data since forage availability and quality varies greatly among all states on this ecological site.
NRCS defines prescribed grazing as “managing the harvest of vegetation with grazing and/or browsing animals with the intent to achieve specific ecological, economic, and management objectives.” As used in this site description, the term ‘prescribed grazing’ is intended to include multiple grazing management systems (e.g. rotational grazing, twice-over grazing, conservation grazing, targeted grazing, etc.) provided that, whatever management system is implemented, it meets the intent of prescribed grazing definition.
The basic grazing prescription addresses balancing forage demand (quality and quantity) with available forage, varying grazing and deferment periods from year-to-year, matching recovery/deferment periods to growing conditions when pastures are grazed more than once in a growing season, implementation of a contingency (e.g. drought) plan, and a monitoring plan. When the management goal is to facilitate change from one plant community phase or state to another, then the prescription needs to be designed to shift the competitive advantage to favor the native grass and forb species.
Grazing levels are noted within the plant community narratives and pathways in reference to prescribed grazing management. “Degree of utilization” is defined as the proportion of the current year’s forage production that is consumed and/or destroyed by grazing animals (may refer to a single plant species or a portion or all the vegetation). “Grazing utilization” is classified as slight, moderate, full, close, and severe (see the following table for description of each grazing use category). The following utilization levels are also described in the Ranchers Guide to Grassland Management IV. Utilization levels are determined by using the landscape appearance method as outlined in the Interagency Technical Reference “Utilization Studies and Residual Measurements” 1734-3.
Utilization Levels % Use Description
Slight (light) 0-20 Appears practically undisturbed when viewed obliquely. Only choice areas and forage utilized
Moderate 20-40 Almost all of accessible range shows' grazing. Little or no used of poor forage. Little evidence of trailing to grazing.
Full 40-60 All fully accessible areas are grazed. The major sites have key forage species properly utilized (about half taken, half left). Points of concentration with overuse limited to 5 to 10 percent of accessible area.
Close (Heavy) 60-80 All accessible range plainly shows use and major sections closely cropped. Livestock forced to use less desirable forage, considering seasonal preference.
Severe >80 Key forage species completely used. Low-value forages are dominant.
Hydrological functions
Available water is the principal factor limiting forage production on this site. This site is dominated by soils in hydrologic group B. Infiltration varies from moderately slow to moderately rapid; runoff potential varies from low to high depending upon surface texture, slope percent, slope shape, and ground cover. In many cases, areas with greater than 75% ground cover have the greatest potential for high infiltration and lower runoff. An exception would be where short grasses form a strong sod and dominate the herbaceous layer of the site. Areas where ground cover is less than 50% have the greatest potential to have reduced infiltration and higher runoff (refer to Section 4, NRCS National Engineering Handbook for runoff quantities and hydrologic curves).
Recreational uses
Over 113,000 acres of National Wildlife Refuges and over 77,000 acres of Waterfowl Production Areas owned and managed by the United States Fish and Wildlife Service are available for public hunting and bird watching. In addition, over 22,000 acres of North Dakota Wildlife Management Areas (WMAs), approximately 8,000 acres of North Dakota Forest Service, and thousands of acres of Department of Trust Lands are scattered throughout the central and western portions of the MLRA; these areas are available for hunting and bird watching. MLRA 55A provides a unique ruffed grouse hunting opportunity in North Dakota on wildlife management areas managed by the North Dakota Game and Fish Department and forest service lands managed by North Dakota Forest Service within the Turtle Mountain.
Camping: Three state parks are located within the MLRA including Lake Metigoshe State Park (Turtle Mt.), Grahams Island State Park (Devils Lake), and the newly designated Pembina Gorge State Park (formerly Pembina Gorge Recreation Area). These Parks provide hiking, biking, birding, canoeing, and wildlife viewing opportunities. Many local parks and private parks provide modern and primitive camping opportunities. The approximately 8,000 acres of North Dakota Forest Service provides primitive camping (no electric or water hookups) as well as fishing and canoeing access at various lakes. These forests and lakes provide access to swimming beaches, picnicking, and an extensive trail system open to hiking, mountain biking, horseback riding, snowmobiling, and cross-country skiing (not groomed). Limited primitive camping is also available on North Dakota Game and Fish Department Wildlife Management Areas.
Hiking/Biking/Horseback Riding: Hiking is permitted on most state and federally owned lands. Developed hiking and biking trails can be found on North Dakota Forest Service lands (18.6 miles), Upper Souris NWR (4.25 miles), Des Lacs NWR (8.5 miles), J. Clark NWR (3.3 miles), White Horse Hill National Game Preserve (3.6 miles), Lake Metigoshe State Park (16 miles), and Grahams Island State Park (2.1 miles; 3 miles cross country skiing). In addition, extensive biking and walking trails are found in local county and city parks. The Turtle Mountain State Recreation Area (ND Forest Service) is located six miles northwest of Bottineau. This recreation area has over 12 miles of trails open to hiking, biking, snowshoeing, horseback riding, and OHV’s.
The Pembina Gorge State Park encompasses over 2,800 acres of public land in the Pembina River Gorge. Steep valley cliffs towering over small, isolated prairies and pocketed wetlands surrounded by the largest continuous, undisturbed forest in North Dakota provide opportunities for canoeing, kayaking, hiking, biking, horseback riding, hunting, wildlife observing, birding, and downhill and cross- country skiing. Thirty miles of trails provide snowmobiling, mountain biking, and off-highway vehicles (OHV) opportunities.
Canoeing/Kayaking: Designated canoe and kayaking trails are available within the MLRA. J. Clark Sayler NWR has 12.75 miles of designated trails on the Souris River and Pembina Gorge State Park has 14.25 miles on the Pembina River. The Pembina Gorge State Park offers kayak rentals along with kayak transportation. Lake Metigoshe State Park offers canoe and kayak rentals along with standup paddleboards, pontoons, cross country skis, snowshoes, etc.
Downhill Skiing: Downhill skiing is available at Bottineau Winter Park within Turtle Mountain and Frost Fire Park at the Pembina Gorge. Full-service rental shops are available along with alpine trails ranging from beginner to expert. Conveyor lifts on the beginner hills to chairlifts are available for skiers.
International Peace Garden: The only peace garden located on the United States/Canada border, the International Peace Garden is a 2,339-acre botanical garden commemorating peace between the United States and Canada along the world’s longest unfortified border. It blooms with more than 155,000 flowers and showcases the Peace Chapel, Peace Towers, and Floral Clock. The North American Game Wardens Museum if also located within the boundaries of the International Peace Garden.
Wood products
Several small commercial sawmills have operated in the area in the past, and limited harvesting of timber for personal use may occur (e.g. fence posts, firewood). However, at the present time commercial timber harvesting is generally considered to be uneconomical. Commercial harvesting of quaking aspen has not been economically viable largely due to heart rot (e.g. Phellinus igniarius) and distance to commercial sawmills.
Other products
Seed harvest of native plant species can provide additional income on this site.
Other information
• Additional documentation from areas of this site in the Pembina Gorge and Hills and in the moraine near Devils Lake (Spirit Lake Reservation, Graham’s Island, Camp Grafton, and Pembina Gorge areas) would be useful to confirm that all plant community states, phases, and transition pathways are adequately represented. All the required Tier 3 data has been collected in the Turtle Mountains. MLRA map units in these areas are:
Hamerly-Wyard-Bottineau loams, 0 to 3 percent slopes (map unit 2q4g7)
Bottineau loam, 0 to 3 percent slopes (map unit 2q3wv)
Bottineau loam, 3 to 6 percent slopes (map unit 2q3ww)
Bottineau loam, 6 to 9 percent slopes (map unit 2q3wx)
Bottineau loam, 9 to 15 percent slopes (map unit 2q3wy)
Brantford-Bottineau-Buse loams, 15 to 60 percent slopes (map unit 2q5lr)
Waukon loam, 0 to 3 percent slopes (map unit 2q3x5)
Waukon loam, 3 to 6 percent slopes (map unit 2q3x6)
Waukon loam, 6 to 9 percent slopes (map unit 2q3x7)
• Further investigation is needed on the Waukon soils (fine-loamy, mixed, Mollic Hapludalfs). The soil has more highly developed ‘alfic properties’ than the Bottineau soils which are most representative of the Loamy Savannah ecological site. Areas of Waukon that have not been cleared should determine whether these soils would better fit the Upland Hardwood Forest ecological site.
• Further investigation is needed on the Metigoshe soils (coarse-loamy mixed, Alfic Argiudolls) which have been tentatively included in the Loamy Savannah site. They are of very limited extent. A few delineations are closely associated with Kelvin and Rolla soils on the higher elevations of Turtle Mountain. These delineations appear to have similar vegetation as the Upland Hardwood Forest site. MLRA map units to investigate are:
Metigoshe coarse sandy loam, 2 to 9 percent slopes (map unit 2q4vb)
Metigoshe coarse sandy loam, 9 to 25 percent slopes (map unit 2q4vc)
• Further evaluation and refinement of the State-and-Transition model may be needed to identify disturbance driven dynamics. Additional states and/or phases may be required to address grazing response.
• Site concepts will be refined as above noted investigations are completed.
• The long-term goal is to complete an approved, correlated Ecological Site Description as defined by the National Ecological Site Handbook.
This ESD is the best available knowledge. The site concept and species composition table have been used in the field and tested for more than five years. It is expected that as additional information becomes available revisions may be required.
Supporting information
Inventory data references
Information presented here has been derived from NRCS and other federal/state agency clipping and inventory data. Also, field knowledge of range-trained personnel was used. All descriptions were peer reviewed and/or field-tested by various private, state, and federal agency specialists.
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USDA, NRCS. National water & climate center, 1201 NE Lloyd Blvd, Suite 802, Portland, OR 97232- 1274. (https://www.wcc.nrcs.usda.gov/)
USDA, NRCS. 2001. The PLANTS database, version 3.1 (http://plants.usda.gov). National Plant Data Center, Baton Rouge, LA 70874-4490 USA.
USDA, NRCS, Various published soil surveys.
USDI BLM.1999. Utilization studies and residual measurements. Interagency Technical Reference 1734-3.
U.S. Fish and Wildlife Service. 2015. Endangered and threatened wildlife and plants; designation of critical habitat for the Dakota skipper and Poweshiek skipperling; Vol. 79 No. Final Rule October 1, 2015, 50 CFR Part 17.
Vinton, M.A. and E.M. Goergen. 2006. Plant-soil feedbacks contribute to the persistence of Bromus inermis in tallgrass prairie. Ecosystems 9: 967-976.
Waddington, J., D.H. McCartney, and L.P. Lefkovitch. 1999. Effects of management on species dynamics of Canadian aspen parkland pastures. Journal of Range Management 52:60-67.
Weatherill, R.G., and L.B. Keith. 1969. The effect of livestock grazing on an aspen forest community. Utah State University. Department of Lands and Forests Fish and Wildlife Division Technical Bulletin No. 1. 31 pages.
Whitman, W.H., H. Hanson, and R. Peterson. 1943. Relation of drought and grazing to North Dakota range lands. North Dakota Agricultural Experimentation Bulletin 340.
Contributors
ND NRCS: David Dewald, Jonathan Fettig, Alan Gulsvig, Mark Hayek, Chuck Lura, Jeff Printz, Steve Sieler, and Hal Weiser.
Approval
Suzanne Mayne-Kinney, 5/08/2025
Acknowledgments
We gratefully acknowledge Shawn Krance, Jason Sieler, Dustin Brodina, and Jody Forman for their help with data collection (ND NRCS), Henry “Chick” LaRocque NRCS tribal liaison for securing access to Turtle Mountain Band of Chippewa tribal lands, and Ernie Azure and Ron Davis (Turtle Mountain Band of Chippewa) for assistance with data collection and land-use history. We also gratefully acknowledge North Dakota State University: Joe Zeleznik, North Dakota Forest Service: Cody Clemenson, and Derek Lowstuter for their insight into forest management and tree and shrub species identification.
Rangeland health reference sheet
Interpreting Indicators of Rangeland Health is a qualitative assessment protocol used to determine ecosystem condition based on benchmark characteristics described in the Reference Sheet. A suite of 17 (or more) indicators are typically considered in an assessment. The ecological site(s) representative of an assessment location must be known prior to applying the protocol and must be verified based on soils and climate. Current plant community cannot be used to identify the ecological site.
Author(s)/participant(s) | USDA-NRCS North Dakota |
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Contact for lead author | NRCS State Rangeland Management Specialist |
Date | 12/01/2021 |
Approved by | Suzanne Mayne-Kinney |
Approval date | |
Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
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Number and extent of rills:
Rills are not expected on this site when slopes are less than 25%. On slopes greater than 25%, short (12 to 20 inches in length), discontinuous rills would be expected. -
Presence of water flow patterns:
Water flow patterns are not visible. -
Number and height of erosional pedestals or terracettes:
Neither pedestals nor terracettes are expected. -
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Bare ground is 10% or less consisting of randomly scattered small patches no greater than 2 inches in diameter. Animal activity (burrows and ant mounds) may occasionally result in isolated bare patches of up to 24 inches in diameter. -
Number of gullies and erosion associated with gullies:
Active gullies are not expected on this site. If present, gully channel(s) are fully vegetated with no active erosion visible. -
Extent of wind scoured, blowouts and/or depositional areas:
No wind-scoured or depositional areas expected on this site. -
Amount of litter movement (describe size and distance expected to travel):
Plant litter movement not expected on this site. -
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Stability class anticipated to average 5 or greater. -
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Use soil series description for depth, color, and structure of A-horizon. -
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Mid- and short-statured cool- season bunch grasses are dominant. Mid- and short statured cool-season rhizomatous grasses, and shrubs are subdominant. Dominant and subdominant functional/structural groups are well distributed across the site. -
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
No compaction layers occur naturally on this site. -
Functional/Structural Groups (list in order of descending dominance by above-ground annual-production or live foliar cover using symbols: >>, >, = to indicate much greater than, greater than, and equal to):
Dominant:
Phase 1.1:
Mid & short C3 bunch grasses (5)Sub-dominant:
Phase 1.1:
Mid & short C3 rhizomatous grasses (1); Tall C4 rhizomatous grasses (2); Shrubs (6)Other:
Phase 1.1:
Mid & short C4 bunch grasses; Forbs; Grass- likes; TreesAdditional:
Due to differences in phenology, root morphology, soil biology relationships, and nutrient cycling Kentucky bluegrass, smooth brome, and crested wheatgrass are included in a new Functional/structural group, mid- and short-statured early cool-season grasses (MSeC3), not expected for this site.
To see a full version 5 rangeland health worksheet with functional/structural group tables, please use the following hyperlink:
https://efotg.sc.egov.usda.gov/references/public/ND/55A_Loamy_Savannah_Narrative_FINAL_Ref_FSG.pdf -
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Dead or dying plants/plant parts occur rarely on this site. Some dead centers may be observed on warm-season bunchgrasses after one to several years of below normal precipitation. -
Average percent litter cover (%) and depth ( in):
Plant litter cover is 60 to 80% with a depth of 0.25 to 0.5 inches. Litter is in contact with soil surface. -
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
Annual air-dry production is 2875 lbs./ac (reference value) with normal precipitation and temperatures. Low and high production years should yield 2450 to 3300 lbs./ac, respectively. -
Potential invasive (including noxious) species (native and non-native). List species which BOTH characterize degraded states and have the potential to become a dominant or co-dominant species on the ecological site if their future establishment and growth is not actively controlled by management interventions. Species that become dominant for only one to several years (e.g., short-term response to drought or wildfire) are not invasive plants. Note that unlike other indicators, we are describing what is NOT expected in the reference state for the ecological site:
State and local noxious species, Kentucky bluegrass, smooth bromegrass, crested wheatgrass, quackgrass, buckthorn, and Eastern red cedar/juniper. -
Perennial plant reproductive capability:
Noninvasive species in all functional/structural groups are vigorous and capable of reproducing annually under normal weather conditions.
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The Ecosystem Dynamics Interpretive Tool is an information system framework developed by the USDA-ARS Jornada Experimental Range, USDA Natural Resources Conservation Service, and New Mexico State University.
Click on box and path labels to scroll to the respective text.
Ecosystem states
T1A | - | Introduction of exotic cool-season grasses, outside of historic disturbance regime |
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T2A | - | Clear cutting and brush management |
State 1 submodel, plant communities
1.1A | - | Long-term drought, fire return interval more frequent |
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1.1B | - | Long-term above average precipitation, fire return interval less frequent |
1.2A | - | Return to average growing conditions, fire return interval returns to normal |
1.3A | - | Return to average growing conditions, fire return interval returns to normal |
State 2 submodel, plant communities
2.1A | - | Introduction of livestock grazing. Long-term light to moderate use |
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2.2B | - | Removal of livestock |
2.2A | - | Increased livestock grazing. Long-term season long heavy use |
2.3A | - | Long-term light to moderate use |