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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.
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Figure 1. Mapped extent
Areas shown in blue indicate the maximum mapped extent of this ecological site. Other ecological sites likely occur within the highlighted areas. It is also possible for this ecological site to occur outside of highlighted areas if detailed soil survey has not been completed or recently updated.
Associated sites
R025XY412UT Mountain Gravelly Loam (Mountain Big Sagebrush)
R025XY418UT Mountain Windswept Ridge (Low Sagebrush)
Similar sites
R025XY412UT Mountain Gravelly Loam (Mountain Big Sagebrush)
Table 1. Dominant plant species
Tree (1) Populus tremuloides
Shrub Not specified
Herbaceous (1) Bromus carinatus
Physiographic features
This site is found on hillslopes on slopes between 15 and 40%. The elevation of the site ranges between 6,000 to 7,000 feet. There is no flooding or ponding potential for this site.
Table 2. Representative physiographic features
Landforms (1) Hill
Flooding frequency None Ponding frequency None Elevation 6000 – 7000 ft Slope 15 – 40 % Aspect N Climatic features
The soil series is in hydrologic groups c and d. The runoff curve numbers are 74 through 89 depending on the condition of the watershed.Climate is cold and snowy in the winter and fairly mild and warm in the summer. Approximately 70 percent of the precipitation comes as snow from December through February on the average July, August, and September are the driest months and January, February, and March are the wettest months. During periods of high precipitation this site acts as a catch basin for extensive amounts of snow accumulations that often persist long after adjacent areas of snow accumulation have melted. Moisture is not limiting to plant growth on this site.
Table 3 Representative climatic features
Frost-free period (average) 0 days Freeze-free period (average) 80 days Precipitation total (average) 20 in BarLineFigure 2. Monthly precipitation range
BarLineFigure 3. Monthly average minimum and maximum temperature
">Influencing water features
Soil features
The soils on this site were formed in colluvium derived from quartzite and mica schist. The soil is well drained with moderate permeability in the upper 10 inches of soil. The soil does not have bedrock within 20 inches of the soil surface. The soil texture at the surface is gravelly loam. Surface rock fragments over 3 inches is are not present at this site, subsurface rock fragments over 3 inches is 5% by volume. Surface rock fragments between 2 millimeters and 3 inches is 28% by cover and subsurface rock fragments of the same size is 42% by volume. Available water capacity is between 3.2 and 4.1 in the upper 40 inches of soil. The soil pH is between 6.1 and 6.5. The soil temperature regime is frigid.
Soils associated with this site:
UT601 – Parkay (57)Table 4. Representative soil features
Surface texture (1) Gravelly loam
Drainage class Well drained Permeability class Moderate Surface fragment cover <=3" 28 % Surface fragment cover >3" Not specified Available water capacity
(0-40in)3.2 – 4.1 in Calcium carbonate equivalent
(0-40in)Not specified Electrical conductivity
(0-40in)Not specified Sodium adsorption ratio
(0-40in)Not specified Soil reaction (1:1 water)
(0-40in)6.1 – 6.5 Subsurface fragment volume <=3"
(Depth not specified)42 % Subsurface fragment volume >3"
(Depth not specified)5 % Ecological dynamics
As this site deteriorates due to grazing pressure mountain brome, slender wheatgrass, meadowrue, and horsemint decrease while milkvetch, mountain big sagebrush, and snowberry increase. When the potential natural plant community is burned, mountain brome, slender wheatgrass, and mountain big sagebrush decrease while rabbitbrush, and snowberry increase.
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 textEcosystem states
State 1 submodel, plant communities
State 1
Reference StateCommunity 1.1
Reference StateThe general view of this site is low-growing quaking aspen. The composition by air-dry weight is approximately 45 percent perennial grasses, 20 percent forbs, and 20 percent shrubs and 15 percent trees.
Figure 4. 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 653 990 1328 Shrub/Vine 290 440 590 Forb 290 440 590 Tree 218 330 443 Total 1451 2200 2951 Table 6. Ground cover
Tree foliar cover 70-70% Shrub/vine/liana foliar cover 10-20% Grass/grasslike foliar cover 30-30% Forb foliar cover 20-20% Non-vascular plants 0% Biological crusts 0% Litter 0% Surface fragments >0.25" and <=3" 0% Surface fragments >3" 0% Bedrock 0% Water 0% Bare ground 0% Table 7. Canopy structure (% cover)
Height Above Ground (ft) Tree Shrub/Vine Grass/
GrasslikeForb <0.5 – – – – >0.5 <= 1 – – – – >1 <= 2 – – 29-31% 19-21% >2 <= 4.5 – 14-16% – – >4.5 <= 13 – – – – >13 <= 40 69-71% – – – >40 <= 80 – – – – >80 <= 120 – – – – >120 – – – – Additional community tables
Table 8. Community 1.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Tree0 Dominant Trees 225–338 quaking aspen POTR5 Populus tremuloides 225–338 – Shrub/Vine0 Dominant Shrubs 181–338 mountain snowberry SYOR2 Symphoricarpos oreophilus 113–225 – chokecherry PRVI Prunus virginiana 68–113 – 3 Sub-Dominant Shrubs 432–950 Shrub (>.5m) 2SHRUB Shrub (>.5m) 225–338 – Saskatoon serviceberry AMAL2 Amelanchier alnifolia 23–68 – mountain big sagebrush ARTRV Artemisia tridentata ssp. vaseyana 23–68 – snowbrush ceanothus CEVE Ceanothus velutinus 23–68 – yellow rabbitbrush CHVIL4 Chrysothamnus viscidiflorus ssp. lanceolatus 23–68 – creeping barberry MARE11 Mahonia repens 23–68 – bitter cherry PREM Prunus emarginata 23–68 – sticky currant RIVI3 Ribes viscosissimum 23–68 – Woods' rose ROWO Rosa woodsii 23–68 – Scouler's willow SASC Salix scouleriana 23–68 – Grass/Grasslike0 Dominant Grasses 430–789 California brome BRCA5 Bromus carinatus 113–225 – slender wheatgrass ELTR7 Elymus trachycaulus 113–225 – Ross' sedge CARO5 Carex rossii 68–113 – Columbia needlegrass ACNE9 Achnatherum nelsonii 68–113 – 1 Sub-Dominant Grasses 387–926 Grass, annual 2GA Grass, annual 113–225 – Grass, perennial 2GP Grass, perennial 113–225 – Letterman's needlegrass ACLE9 Achnatherum lettermanii 23–68 – western needlegrass ACOC3 Achnatherum occidentale 23–68 – squirreltail ELEL5 Elymus elymoides 23–68 – blue wildrye ELGL Elymus glaucus 23–68 – Idaho fescue FEID Festuca idahoensis 23–68 – oniongrass MEBU Melica bulbosa 23–68 – bluebunch wheatgrass PSSP6 Pseudoroegneria spicata 23–68 – Forb0 Dominant Forbs 272–452 Gray's biscuitroot LOGR Lomatium grayi 68–113 – stemless dwarf lupine LUCA3 Lupinus caespitosus 68–113 – Fendler's meadow-rue THFE Thalictrum fendleri 68–113 – 2 Sub-Dominant Forbs 495–1260 Forb, annual 2FA Forb, annual 113–225 – Forb, perennial 2FP Forb, perennial 113–225 – common yarrow ACMI2 Achillea millefolium 23–68 – nettleleaf giant hyssop AGUR Agastache urticifolia 23–68 – heartleaf arnica ARCO9 Arnica cordifolia 23–68 – northwestern Indian paintbrush CAAN7 Castilleja angustifolia 23–68 – twolobe larkspur DENU2 Delphinium nuttallianum 23–68 – shaggy fleabane ERPU2 Erigeron pumilus 23–68 – Richardson's geranium GERI Geranium richardsonii 23–68 – oblongleaf bluebells MEOB Mertensia oblongifolia 23–68 – slender cinquefoil POGR9 Potentilla gracilis 23–68 – yellow salsify TRDU Tragopogon dubius 23–68 – hookedspur violet VIAD Viola adunca 23–68 – Interpretations
Animal community
This site provides proper grazing for cattle and sheep during spring, summer, and fall.
This site provides food and cover for wildlife.
Wildlife using this site include blacktail jackrabbit, coyote, sage grouse, mule deer, and elk.
Recreational uses
Hunting and Hiking
Wood products
Poles and Fire Wood
Supporting information
Contributors
GBB
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) Shane A. Green (NRCS), Mike Gates (BLM), Tyler Staggs (BLM), Alan Bass (BLM), Brock Benson (NRCS), Robert D. Stager (BLM). Contact for lead author shane.green@ut.usda.gov Date 03/30/2007 Approved by Approval date Composition (Indicators 10 and 12) based on Annual Production Indicators
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Number and extent of rills:
None to very rare. Any rills present should be somewhat short in length (less than 3 feet long) and only occur on areas with increased runoff on the lower parts of steeper slopes and areas below exposed bedrock. An increase in rill formation may be seen after disturbance events such as recent fire or episodic thunderstorms. -
Presence of water flow patterns:
None to few. Flow patterns wind around perennial plant bases and should show very slight evidence of erosion. They are expected to be short, stable, sinuous and not connected. There is usually very minor evidence of deposition. Evidence of flow will increase a little with slope. -
Number and height of erosional pedestals or terracettes:
Plants should show little or no pedestalling. Terracettes should be absent. These areas are small pockets of trees not large enough to have terracettes form when vegetation is stable. -
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
3 – 10%. The soil surface may have large rocks throughout with 30 to 60 percent rock fragments. Ground cover is measured as first raindrop impact, bare ground is the inverse of cover. Ground cover + bare ground = 100%. -
Number of gullies and erosion associated with gullies:
None to few. If present, gullies may be wide and shallow and armored with rock fragments and dense vegetation. -
Extent of wind scoured, blowouts and/or depositional areas:
None. No evidence of wind generated soil movement is anticipated. -
Amount of litter movement (describe size and distance expected to travel):
Most litter resides in place with little redistribution caused by water movement. Minor litter removal may occur in flow channels with deposition occurring at points of obstruction. The majority of litter accumulates at the base of plants. Some grass leaves and small twigs (grass stems) may accumulate in soil depressions adjacent to plants. Woody stems are not likely to move. However, some litter movement is expected with increases in slope and/or increased runoff resulting from heavy thunderstorms. -
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
This site should have a soil stability rating of 5 or 6 under the plant canopies, and a rating of 4 to 5 in the interspaces. The average should be a 5. Surface texture is a cobbly loam. Vegetation cover, litter and/or surface rock reduce erosion. -
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Soil surface horizon is 8 inches thick. Structure is weak fine granular. Color is very dark grayish brown (10YR3/2). Mollic epipedon is 30 inches thick. Use the specific information for the soil you are assessing found in the published soil survey to supplement this description. -
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Plants occur in sufficient cover and spatial arrangement to intercept raindrops and reduce raindrop splash erosion. Litter on soil surface and condition of soil surface also protect soil from splash erosion and encourage a high rate of infiltration. Plant spatial distribution should slow runoff allowing additional time for infiltration. Bare spaces are expected to be small and irregular in shape and are usually not connected. The vegetative structure is usually adequate to capture snow and ensure snowmelt occurs in a subdued manner allowing maximum time for infiltration and reduce runoff and erosion in all but the most extreme thunder storm events. When perennial grasses, shrubs and/or trees (aspen) decrease, reducing ground cover and increasing bare ground, runoff is expected to increase and any associated infiltration reduced. -
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
None. -
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:
Dominants: Aspen, Mountain snowberry, Mountain brome, Slender wheatgrass,Sub-dominant:
Sub-dominants: Chokecherry, Mountain big sagebrush and other shrubs, perennial grasses and forbs.Other:
Perennial and annual forbs can be expected to vary widely in their expression in the plant community based upon departures from average growing conditions.Additional:
Disturbance regime includes fire, drought, and disease. Assumed fire cycle of 30-50 years. Dominance is based on average annual production, air dry weight: Perennial bunchgrasses > trees (aspen) > sprouting shrubs > native perennial and annual forbs > non-sprouting shrubs. Functional/structural groups may appropriately contain non-native species if their ecological function is the same as the native species in the reference state (e.g. Smooth brome, intermediate wheatgrass, alfalfa, etc.) Following a recent disturbance such as fire, drought or disease that remove the woody vegetation, forbs and perennial grasses (herbaceous species) may dominate the community. If a disturbance has not occurred for an extremely extended period of time, woody species may continue to increase crowding out the perennial herbaceous understory species. In either case, these conditions would reflect a functional community phase within the reference state. -
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
All age classes of perennial grasses should be present under average to above average growing conditions with age class expression likely subdued in below average growing conditions, or on sites with high (usually greater than 65%) similarity index (late seral to historic climax). Slight decadence in the principle trees and shrubs could occur near the end of the fire cycle or during periods of extended drought, or insect infestations. In general, a mix of age classes may be expected with some dead and decadent plants present. Trees will normally be a more even aged stand. -
Average percent litter cover (%) and depth ( in):
Variability may occur due to growing conditions. -
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
2150-2250 #/acre on an average year. -
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:
Rabbitbrush, annual grasses and forbs. -
Perennial plant reproductive capability:
All perennial plants should have the ability to reproduce in all years, except in extreme drought years and snow drift accumulation areas.
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