Natural Resources
Conservation Service
Ecological site R034AY426CO
Loamy Cold Desert
Last updated: 9/07/2023
Accessed: 11/21/2024
General information
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
MLRA notes
Major Land Resource Area (MLRA): 034A–Cool Central Desertic Basins and Plateaus
Major Land Resource Area (MLRA): 034A–Cool Central Desertic Basins and Plateaus
Major Land Resource Area (MLRA): 34A-Cool Central Desertic
Basins and Plateaus
For further information regarding MLRAs, refer to:
http://soils.usda.gov/survey/geography/mlra/index.html
LRU notes
Land Resource Unit (LRU) 34A-10:
• Moisture Regime: aridic ustic
• Temperature Regime: frigid
• Dominant Cover: rangeland
• Representative Value (RV) Effective Precipitation: 7-10 inches
• RV Frost-Free Days: 75-105 days
Classification relationships
Ecoregions (EPA):
Level I: 10 North American Deserts
Level II: 10.1 Cold Deserts
Level III: 10.1.4 Wyoming Basin
Ecological site concept
• Site does not receive any additional water.
• Soils are:
o are not slightly saline or saline-sodic.
o are deep
o are not skeletal within 13” of soil surface, minimal rock fragments at the soil surface; may be skeletal below 13"
o are not strongly or violently effervescent in surface mineral 10”.
o surface textures usually range from loamy sand to sandy loam in surface mineral 2-3”.
• Slope is less than 12 percent.
• Clay content is less than 35% and great than 18% in mineral soil surface 1-2”.
Associated sites
R034AY420CO |
Cold Desert Breaks |
---|---|
R034AY421CO |
Cold Desert Overflow |
Similar sites
R034AY423CO |
Limy Cold Desert |
---|
Table 1. Dominant plant species
Tree |
Not specified |
---|---|
Shrub |
(1) Atriplex confertifolia |
Herbaceous |
(1) Achnatherum hymenoides |
Physiographic features
This site occurs on nearly flat to gently sloping areas. Slopes range from 3 to 12 percent. This site occurs on all aspects. Elevation for the site ranges from 5400 to 6000 feet above sea level.
Table 2. Representative physiographic features
Landforms |
(1)
Plateau
(2) Fan |
---|---|
Runoff class | Low |
Flooding frequency | None |
Ponding frequency | None |
Elevation | 5,400 – 6,000 ft |
Slope | 3 – 12% |
Aspect | Aspect is not a significant factor |
Climatic features
The climate of this site is arid to semi-arid, with precipitation averaging between 7 and 10 inches annually.
The growing season for the native plants averages 160 to 180 days. This usually starts in early April and goes until late September. Cool season grasses start spring growth using moisture stored in the soil from snow melt and spring rains. Optimum growth occurs from Mid-April through mid-June, and continues until the soil profile is depleted of usable soil moisture. A second growth period may occur in the fall months as a result of a fall moisture peak.
The average annual air temperature is about 45 to 48 degrees Fahrenheit. Summer temperatures can reach 100F, and winter temperatures can dip to -30 degrees Fahrenheit. Temperatures fall below the freezing mark much of the time in October through May. The average frost-free period occurs from approximately June 2 through September 15, lasting about 105 days.
Spring and fall are peak periods of precipitation. July is usually the driest month of the year. The seasonal distribution of precipitation and relatively low spring temperatures favor production of cool season plants making the site more productive than the annual precipitation might indicate.
Table 3. Representative climatic features
Frost-free period (characteristic range) | 75-105 days |
---|---|
Freeze-free period (characteristic range) | |
Precipitation total (characteristic range) | 7-10 in |
Frost-free period (average) | 105 days |
Freeze-free period (average) | |
Precipitation total (average) | 10 in |
Figure 1. Monthly precipitation range
Influencing water features
None
Wetland description
None
Soil features
Soils of this site are deep and well drained with surface textures of loamy sands, 2 to 3 inches thick. The upper part of the underlying materials are sandy loams from 2 to 14 inches. Below this are sandy loams to greater than 60 inches in the Chroder soils. The Clifsand soils are very cobbly sandy loams from 13 to 43 inches, and extremely stony loamy sands to 60 inches. Depth to the calcic horizon in the Chroder soils is 10 to 20 inches, and 10 to 25 inches in the Clifsand soils. Permeability is moderately rapid, available water holding capacity is low, runoff is low, hazard of water erosion is slight, and hazard of soil blowing is high for Clifsand soils.
Soils associated with this site are:
Chroder sandy loam, 3 to 12 percent slopes
Clifsand-Chroder complex, 3 to 12 percent slopes
Table 4. Representative soil features
Parent material |
(1)
Eolian deposits
(2) Alluvium – sedimentary rock |
---|---|
Surface texture |
(1) Loamy sand (2) Sandy loam |
Family particle size |
(1) Loamy |
Drainage class | Well drained |
Permeability class | Moderate to moderately rapid |
Soil depth | 60 in |
Surface fragment cover <=3" | 10% |
Surface fragment cover >3" | 5% |
Available water capacity (0-40in) |
3.9 – 7.1 in |
Calcium carbonate equivalent (0-40in) |
30 – 35% |
Sodium adsorption ratio (0-40in) |
5 |
Soil reaction (1:1 water) (0-40in) |
7.4 – 8.4 |
Subsurface fragment volume <=3" (0-40in) |
15% |
Subsurface fragment volume >3" (0-40in) |
30% |
Ecological dynamics
The aspect of this site is a grassland-shrub mix.
Historical records and photographs document the fact that the Browns Park Area was under sever grazing pressure by cattle, sheep, and horses during the last half of the 1800's and early 1900's. This pressure significantly altered the native vegetation, particularly in the lowlands immediately adjacent to the Green River and the area north of the river. This has made it difficult to determine the potential natural vegetation.
The dominant grasses are needle and thread, Indian ricegrass, and thickspike wheatgrass. Less abundant grasses are bottlebrush squirreltail, Sandberg bluegrass and muttongrass. Forbs that make up the plant community are sparse, but include stemless spring parsley, foothill deathcamas, and scarlet globemallow. Wyoming big sagebrush is the dominant shrub on this site, with shadscale occurring to a lesser extent.
If ecological retrogression is cattle induced, the percentage and production of desirable plants such needle and thread, Indian ricegrass, Sandberg bluegrass, Pacific aster, shadscale, and winterfat will decrease. If retrogression is sheep induced, the percentage and production of desirable plants such as Indian ricegrass, Pacific aster, Wyoming big sagebrush, shadscale black sagebrush, and winterfat will decrease. Along with the decrease in desirable plants, there will be an increase in plants such as foothill deathcamas, Hoods phlox, tufted evening primrose, plains pricklypear, small low rabbitbrush, broom snakeweed, black greasewood, and annuals such as cheatgrass.
Further evidence of retrogression may be "hedging" of shrubs, sheet erosion, a large increase in annuals, an absence of plant litter and new seedlings, and highly unstable forage production from year to year.
During winters of sever temperatures and snows, there will be heavy use in local areas of Wyoming big sagebrush, shadscale, and winterfat by deer, antelope, livestock, and any elk which may occupy the site. Wildlife and livestock will make use of low palatable species to avoid starvation.
Generally, there is inadequate fuel on this site to carry fire. Should a fire burn across the site, the bunchgrasses will be only slightly benefited, while thickspike wheatgrass will be greatly benefited and small low rabbitbrush, stickyleaf low rabbitbrush, and Nuttall horsebrush will flourish. Shrubs, particularly winterfat, Wyoming big sagebrush, and shadscale will be severely affected, and will be several years recovering. The production will decline the first year and thereafter grasses and forbs will increase, with shrubs having long-term increase.
Due to low precipitation of the area, this site will recover slowly from a prolonged and/or severe drought. Grass and forbs will show signs of stress and recovery earlier than shrubs because of their shallow root systems.
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
State 1 submodel, plant communities
State 1
Reference State
Community 1.1
Indian Ricegrass-Thickspike Wheatgrass/Shadscale
The plant community is about 50 to 75 percent grasses, 5 to 15 percent forbs, and 20 to 35 percent shrubs (air-dry weight of current seasons growth). Basal area (the area of ground surface covered by the perennial vegetation measured one inch above the soil) is approximately 15 percent when near the potential plant community. Annual Production: If the range is in excellent condition, the approximate total annual production (air-dry) is: Favorable years 600 lbs/ac Normal years 500 lbs/ac Unfavorable years 250 lbs/ac Of the production, 40 percent will likely be unpalatable or out of reach to grazing animals.
Figure 2. 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 | 135 | 310 | 340 |
Shrub/Vine | 95 | 140 | 180 |
Forb | 20 | 50 | 80 |
Total | 250 | 500 | 600 |
State 2
Degraded State
This State is result of soil-disturbing activities such as hoof-action, anthropogenic activity, and rodent activity. It can also occur after brush management followed by improper grazing techniques that usually include high-intensity grazing without appropriate recovery periods.
Transition T1A
State 1 to 2
The driver for transition T1A from State 1 (Reference State) to State 2 (Degraded) is low to high intensity, long duration, and high frequency herbivory events.
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 | 250–375 | |||||
Indian ricegrass | ACHY | Achnatherum hymenoides | 75–100 | – | ||
thickspike wheatgrass | ELLAL | Elymus lanceolatus ssp. lanceolatus | 75–100 | – | ||
needle and thread | HECOC8 | Hesperostipa comata ssp. comata | 50–100 | – | ||
squirreltail | ELEL5 | Elymus elymoides | 25–50 | – | ||
Sandberg bluegrass | POSE | Poa secunda | 40–50 | – | ||
muttongrass | POFE | Poa fendleriana | 10–25 | – | ||
Forb
|
||||||
2 | 25–75 | |||||
Fremont's beardtongue | PEFR | Penstemon fremontii | 5–10 | – | ||
spiny phlox | PHHO | Phlox hoodii | 5–10 | – | ||
littleleaf pussytoes | ANMI3 | Antennaria microphylla | 5–10 | – | ||
plains springparsley | CYAC | Cymopterus acaulis | 5–10 | – | ||
Pacific aster | SYCH4 | Symphyotrichum chilense | 5–10 | – | ||
hoary Townsend daisy | TOIN | Townsendia incana | 5–10 | – | ||
foothill deathcamas | ZIPA2 | Zigadenus paniculatus | 0–5 | – | ||
tufted evening primrose | OECA10 | Oenothera caespitosa | 0–5 | – | ||
scarlet globemallow | SPCO | Sphaeralcea coccinea | 0–5 | – | ||
small-leaf globemallow | SPPA2 | Sphaeralcea parvifolia | 0–5 | – | ||
Shrub/Vine
|
||||||
3 | 100–175 | |||||
shadscale saltbush | ATCO | Atriplex confertifolia | 40–50 | – | ||
yellow rabbitbrush | CHVI8 | Chrysothamnus viscidiflorus | 10–25 | – | ||
broom snakeweed | GUSA2 | Gutierrezia sarothrae | 10–25 | – | ||
winterfat | KRLA2 | Krascheninnikovia lanata | 10–25 | – | ||
plains pricklypear | OPPO | Opuntia polyacantha | 10–25 | – | ||
black sagebrush | ARNO4 | Artemisia nova | 10–25 | – | ||
Wyoming big sagebrush | ARTRW8 | Artemisia tridentata ssp. wyomingensis | 10–25 | – |
Interpretations
Animal community
WILDLIFE INTERPRETATIONS:
This site provides habitats which support a resident animal community that is characterized by antelope, mule deer, desert and Nuttall cottontail, white-tailed jackrabbit, prairie dog, sage thrasher, western bluebird, mourning dove, red-tailed hawk, Golden eagle, western meadowlark, and midget faded prairie rattlesnake. There is heavy seasonal use by mule deer in winter and, if the site is adjacent to pinyon-juniper, by elk during the winter months.
This site supports a wide variety of animals. Management should be geared to providing cover and food for the wildlife present. If the site is in poor or fair condition, the food supply will become limited and may force some animals to abandon the site. If range seeding is done, the seeding mixture should meet the needs of wildlife and livestock present. Brush control is not recommended near sage grouse leks.
GRAZING INTERPRETATIONS:
This site is best suited for winter grazing by cattle. Stock water developments are difficult to establish and therefore are few and far between; which is the reason the site is used mostly in winter. Cattle are usually sent to the high country in June for grazing on Federal land. A system of deferred grazing which varies the season of grazing in pastures during successive years is needed to maintain a healthy, well balanced plant community. Rest during different seasons of the year benefits different plants. Fall and winter rest (October through March) benefits shrubs such as winterfat, shadscale, and Wyoming big sagebrush. Spring rest (March through May) benefits cool-season plant such as needle and thread, Indian ricegrass, thickspike wheatgrass, and Sandberg bluegrass. Deferment during late winter and spring reduces competition between grazing animals for palatable shrubs and forbs.
Plants of particularly high grazing value on this site include Indian ricegrass, muttongrass, Sandberg bluegrass, and winterfat.
Brush management can be accomplished by using herbicides which will minimize soil disturbance caused by mechanical control. Burning in late fall or spring when soil moisture is high may also be an alternative method of brush control. Reseeding is best accomplished in the fall. Seedling establishment is difficult due to low precipitation. Fall is the best time to seed if reseeding is needed. Mechanical disturbance of the soil should be minimized to prevent wind erosion.
Stocking rate given below are based on continuous use for the entire growing season, and are intended only as an initial guide. Forage needs are calculated on the basis of 900 pounds of air-dry forage per animal unit month (AUM). To maintain proper use and allow for forage that disappears through trampling, small herbivore use, weathering, etc. Of the palatable forage produced, 35 percent is considered available for grazing by large herbivores.
Condition Class - Percent Climax - (Ac/AUM) (AUM/Ac)
Excellent - 76-100% - (4.6) (.22)
Good - 51-75% - (7.0) (.14)
Fair - 26-50% - (9.0) (.11)
Poor - 0-25% - (14.0+) (.07)
Adjustment to the initial stocking rates should be made as needed to obtain proper use. With specialized grazing systems, inaccessibility, dormant season use, presence of introduced species, etc., stocking rate adjustments will be required.
Major Poisonous Plants:
Nuttall larkspur can be poisonous to cattle, sheep, and horses. Poisoning results from an alkaloid. Season of most problem is Spring and early summer when forage is in short supply.
Orange Sneezeweed can be poisonous to sheep, cattle, and horses. Poisoning results from toxic glucoside. Season of most problem is when forage is in short supply.
Silvery lupine can be poisonous to sheep and cattle. Poisoning results from an alkaloid and is most serious when forage is in short supply.
Hydrological functions
This site has good vegetative cover when in good or excellent condition. As cover and residue increasses, runoff and water erosion will decrease and there will be greater infiltration of moisture into the soil profile. Efforts to maintain or improve plant cover are recommended, and if the soil is severely disturbed, seeding is neessary to prevent water erosion.
Soils in this site are grouped into "A" hydrologic group, as outlined in the Soils of Colorado Loss Factors and Erodibility Hydrologic Groupings handbook. Field investgations are needed to determine hydrologic cover conditions and hydrologic curve numbers. Refer to Peak Flows in Colorado handbook, and SCS National Engineering Handbook, Section 4, for hydrologic curve numbers in determining runoff quantitis.
Recreational uses
This site has low value for natural beauty. It is a great distance from any population centers and really does not draw people to it for scenic drives, camping or picknicking. It has high receational value in the form of hunting.
Wood products
There is no real potential for commercial wood products on this site. However, this site lends itself to tree and shrub plantings for windbreaks, wildlife, and controlling soil erosion. Species which should be considered include Russian olive, Rocky Mountain juniper, and pinyon pine. Sites should be engineered to provide supplemental moisture to promote seedling establishment.
Other products
ENDANGERED PLANTS AND ANIMALS:
This site can be important hunting grounds for Peregrine falcons, especially when rock outcrop are present. The site is within the historic range of the black-footed ferret, and any active prairie dog town on this site is potential habitat for the ferret.
Supporting information
Inventory data references
Information presented here has been derived from NRCS clipping data and other inventory data. Field observations from range trained personnel were also used. Other sources used as references include: USDA NRCS Water and Climate Center, USDA NRCS National Range and Pasture Handbook, and USDA NRCS Soil Surveys from various counties.
Type locality
Location 1: Moffat County, CO | |
---|---|
Township/Range/Section | T21N R102W SN |
General legal description | SW 1/4, Sec 21, T10N, R102W, in Browns Park, Moffat County, Colorado |
Other references
Belnap, J. and S. L. Phillips. 2001. Soil biota in an ungrazed grassland: Response to annual grass (Bromus tectorum) invasion. Ecological Applications: 11: 1261-1275.
Caudle, D., H. Sanchez, J. DiBenedetto, C. Talbot, and M. Karl. 2013. Draft Interagency Ecological Site Handbook for Rangelands. US Dept. of Agriculture. Washington D.C
Cleland, D.T.; Freeouf, J.A.; Keys, J.E., Jr.; Nowacki, G.J.; Carpenter, C; McNab, W.H. 2007. Ecological Subregions: Sections and Subsections of the Conterminous United States.[1:3,500,000], Sloan, A.M., cartog. Gen. Tech. Report WO-76. Washington, DC: U.S. Department of Agriculture, Forest Service.
Musgrave, G.W. 1955. How much of the rain enters the soil? In Water: U.S. Department of Agriculture Yearbook. Washington, D.C. P. 151-159.
National Engineering Handbook. US Department of Agriculture, Natural Resources Conservation Service. Available: http://www.info.usda.gov/CED/Default.cfm#National%20Engineering%20Handbook. Accessed February 25, 2008.
Passey, H. B., W. K. Hugie, E. W. Williams, and D. E. Ball. 1982. Relationships between soil, plant community, and climate on rangelands of the Intermountain west. USDA, Soil Conservation Service, Tech. Bull. No. 1669.
Soil Survey Staff, Natural Resources Conservation Service, United States Department of Agriculture. Web Soil Survey. Available online at http://websoilsurvey.nrcs.usda.gov/. Accessed [8/10/2015].
United States Department of Agriculture, Natural Resources Conservation Service. 2006. Land Resource Regions and Major Land Resource Areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296.
Western Regional Climate Center. Retrieved from http://www.wrcc.dri.edu/summary/Climsmco.html on May 17, 2018.
Contributors
Suzanne Mayne Kinney
Approval
Kirt Walstad, 9/07/2023
Acknowledgments
Field offices in Colorado where the site occurs: Craig
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) | |
---|---|
Contact for lead author | |
Date | 09/12/2023 |
Approved by | Kirt Walstad |
Approval date | |
Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
-
Number and extent of rills:
-
Presence of water flow patterns:
-
Number and height of erosional pedestals or terracettes:
-
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
-
Number of gullies and erosion associated with gullies:
-
Extent of wind scoured, blowouts and/or depositional areas:
-
Amount of litter movement (describe size and distance expected to travel):
-
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
-
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
-
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
-
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction 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:
Sub-dominant:
Other:
Additional:
-
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
-
Average percent litter cover (%) and depth ( in):
-
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
-
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:
-
Perennial plant reproductive capability:
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