
Natural Resources
Conservation Service
Ecological site R030XA056NV
LOAMY HILL 3-5 P.Z.
Last updated: 2/18/2025
Accessed: 03/15/2025
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.
Ecological site concept
This site occurs on mountain summits and sideslopes on all exposures. Slopes range from 30 to 75 percent. Elevations are 1000 to about 4000 feet. The soils associated with this site well drained and are very shallow to shallow to bedrock. They formed in residuum and colluvium from limestone and dolomite.
Please refer to group concept R030XA029CA to view the provisional STM.
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---|---|
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R030XA068NV |
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Table 1. Dominant plant species
Tree |
Not specified |
---|---|
Shrub |
(1) Atriplex confertifolia |
Herbaceous |
(1) Achnatherum hymenoides |
Physiographic features
This site occurs on mountain summits and sideslopes on all exposures. Slopes range from 30 to 75 percent. Elevations are 1000 to about 4000 feet.
Table 2. Representative physiographic features
Landforms |
(1)
Mountain
|
---|---|
Elevation | 1,000 – 4,000 ft |
Slope | 30 – 75% |
Aspect | Aspect is not a significant factor |
Climatic features
The climate of the Mojave Desert has extreme fluctuations of daily temperatures, strong seasonal winds, and clear skies. The climate is arid and is characterized with cool, moist winters and hot, dry summers. Most of the rainfall falls between November and April. Summer convection storms from July to September may contribute up to 25 percent of the annual precipitation. Average annual precipitation is 3 to 5 inches. Mean annual air temperature is 65 to 76 degrees F. The average growing season is about 270 to 360 days.
Table 3. Representative climatic features
Frost-free period (average) | 360 days |
---|---|
Freeze-free period (average) | |
Precipitation total (average) | 5 in |
Figure 1. Monthly average minimum and maximum temperature
Influencing water features
There are no influencing water features associated with this site.
Soil features
The soils associated with this site well drained and are very shallow to shallow to bedrock. They formed in residuum and colluvium from limestone and dolomite. Available water capacity is very low. Runoff is high and permeability is moderately rapid.
Soils correlated to this site are classified as Loamy-skeletal, carbonatic, thermic Lithic Torriorthents.
Table 4. Representative soil features
Parent material |
(1)
Colluvium
–
limestone
|
---|---|
Surface texture |
(1) Very cobbly sandy loam |
Family particle size |
(1) Loamy |
Drainage class | Well drained |
Permeability class | Moderately rapid |
Soil depth | 4 – 14 in |
Surface fragment cover <=3" | 50 – 60% |
Surface fragment cover >3" | 5 – 10% |
Available water capacity (0-40in) |
0.7 – 0.8 in |
Calcium carbonate equivalent (0-40in) |
25 – 60% |
Electrical conductivity (0-40in) |
2 mmhos/cm |
Sodium adsorption ratio (0-40in) |
5 |
Soil reaction (1:1 water) (0-40in) |
8.4 – 9 |
Subsurface fragment volume <=3" (Depth not specified) |
50 – 60% |
Subsurface fragment volume >3" (Depth not specified) |
5 – 10% |
Ecological dynamics
Please refer to group concept R030XA029CA to view the provisional STM.
As ecological condition deteriorates, creosotebush increases as perennial grasses decrease. Species likely to invade this site are annual forbs and grasses such filaree and red brome.
Fire Ecology:
The mean fire return interval for shadscale communities range from 35 to 100 years. Shadscale communities are usually unaffected by fire because of low fuel loads, although a year of exceptionally heavy winter rains can generate fuels by producing a heavy stand of annual forbs and grasses. Increased presence of non-native annual grasses, such as cheatgrass, can alter fire regimes by increasing fire frequency under wet to near-normal summer moisture conditions. Fire kills many creosotebush. Creosotebush is poorly adapted to fire because of its limited sprouting ability. Creosotebush survives some fires that burn patchily or are of low severity. Fire generally kills white bursage. However, most white bursage plants burned because their canopies contained numerous small branches in proximity to herbaceous fuels. Shadscale is fire intolerant and it does not readily recover from fire, except for establishment through seed.
State and transition model
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Ecosystem states
State 1 submodel, plant communities
State 1
Reference State
Community 1.1
Reference Plant Community
The reference plant community is dominated by shadscale, creosotebush and white bursage. Potential vegetative composition is about 5% grasses, 10% perennial and annual forbs and 85% shrubs. Approximate ground cover (basal and crown) is less than 5 percent.
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) |
---|---|---|---|
Shrub/Vine | 21 | 85 | 128 |
Forb | 3 | 10 | 15 |
Grass/Grasslike | 1 | 5 | 7 |
Total | 25 | 100 | 150 |
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 | Perennial grasses | 2–8 | ||||
Indian ricegrass | ACHY | Achnatherum hymenoides | 1–3 | – | ||
desert needlegrass | ACSP12 | Achnatherum speciosum | 1–3 | – | ||
low woollygrass | DAPU7 | Dasyochloa pulchella | 1–3 | – | ||
squirreltail | ELEL5 | Elymus elymoides | 1–3 | – | ||
2 | Annual Grasses | 1–8 | ||||
Forb
|
||||||
3 | Perennial forbs | 1–5 | ||||
globemallow | SPHAE | Sphaeralcea | 1–3 | – | ||
4 | Annual forbs | 1–15 | ||||
plantain | PLANT | Plantago | 1–3 | – | ||
Shrub/Vine
|
||||||
5 | Primary shrubs | 47–85 | ||||
shadscale saltbush | ATCO | Atriplex confertifolia | 40–60 | – | ||
creosote bush | LATR2 | Larrea tridentata | 5–15 | – | ||
burrobush | AMDU2 | Ambrosia dumosa | 2–10 | – | ||
6 | Secondary shrubs | 5–15 | ||||
Nevada jointfir | EPNE | Ephedra nevadensis | 1–5 | – | ||
desert-thorn | LYCIU | Lycium | 1–5 | – | ||
pricklypear | OPUNT | Opuntia | 1–5 | – | ||
Nevada dalea | PSPO | Psorothamnus polydenius | 1–5 | – |
Interpretations
Animal community
Livestock Interpretations:
This site has limited value for livestock grazing, due to the low forage production, steep slopes and stony surfaces. Shadscale provides good browse for domestic sheep and goats. Shadscale leaves and seeds are an important component of domestic sheep and cattle winter diets. Shadscale tends to be browse tolerant. Heavy grazing during the winter and/or spring reduces shadscale. Die-off can also occur during extended periods of high precipitation. Shadscale is tolerant of early spring light-intensity browsing. Creosotebush is unpalatable to livestock. Consumption of creosotebush may be fatal to sheep. White bursage is of intermediate forage value. It is fair to good forage for horses and fair to poor for cattle and sheep. However, because there is often little other forage where white bursage grows, it is often highly valuable to browsing animals and is sensitive to browsing.
Stocking rates vary over time depending upon season of use, climate variations, site, and previous and current management goals. A safe starting stocking rate is an estimated stocking rate that is fine tuned by the client by adaptive management through the year and from year to year.
Wildlife Interpretations:
Shadscale is a valuable browse species providing a source of palatable, nutritious forage for a wide variety of wildlife. The fruits and leaves are a food source for deer, desert bighorn sheep and pronghorn antelope. Creosotebush is unpalatable to most browsing wildlife. White bursage is an important browse species for wildlife.
Hydrological functions
Runoff is very high. Permeability is moderate.
Other products
Seeds of shadscale were used by Native Americans for bread and mush. Creosotebush has been highly valued for its medicinal properties by Native Americans. It has been used to treat at least 14 illnesses. Twigs and leaves may be boiled as tea, steamed, pounded into a powder, pressed into a poultice, or heated into an infusion. White bursage is a host for sandfood, a parasitic plant. Sandfood was a valuable food supply for Native Americans.
Other information
Once established, creosotebush may improve sites for annuals that grow under its canopy by trapping fine soil, organic matter, and symbiont propagules. It may also increase water infiltration and storage. White bursage may be used to revegetate disturbed sites in southwestern deserts.
Supporting information
Type locality
Location 1: Nye County, NV | |
---|---|
Township/Range/Section | T19S R51E S1 |
General legal description | Resting Spring Range south of Ash Meadows, Nye County, Nevada. This site also occurs in Southwestern Nye County, Nevada. |
Other references
Fire Effects Information System (Online; http://www.fs.fed.us/database/feis/plants/).
USDA-NRCS Plants Database (Online; http://www.plants.usda.gov).
Contributors
HA
Approval
Kendra Moseley, 2/18/2025
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) | PATTI NOVAK-ECHENIQUE |
---|---|
Contact for lead author | State Rangeland Management Specialist. |
Date | 04/02/2014 |
Approved by | Kendra Moseley |
Approval date | |
Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
-
Number and extent of rills:
Rills are none. Rock fragments armor the soil surface against erosion. -
Presence of water flow patterns:
Water flow patterns are none to rare. A few may occur on steeper slopes (short <1 m) after summer convection storms. -
Number and height of erosional pedestals or terracettes:
Pedestals are none. -
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Bare ground is 5-15%; surface rock fragments up to 70%. -
Number of gullies and erosion associated with gullies:
None Natural drainages may occur on steeper slopes and are well vegetated. -
Extent of wind scoured, blowouts and/or depositional areas:
None -
Amount of litter movement (describe size and distance expected to travel):
Fine litter (foliage from grasses and annual & perennial forbs) expected to move distance of slope length (<10 ft) during intense summer convection storms or rapid snowmelt events. Persistent litter (large woody material) will remain in place except during large rainfall events. -
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Soil stability values should be 3 to 6 on most soil textures found on this site. -
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Surface structure is typically weak, medium platy. Soil surface colors are pale browns and soils are typified by an ochric epipedon. Organic matter of the surface 2 to 3 inches is typically less than 1%. Organic matter content can be more or less depending on micro-topography. -
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Perennial herbaceous plants slow runoff and increase infiltration. Shrub canopy and associated litter provide some protection from raindrop impact. -
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
Compacted layers are none. Platy or massive sub-surface horizons are not to be interpreted as compacted layers. -
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:
salt desert shrubs (shadscale)Sub-dominant:
associated shrubs >> cool-season perennial bunchgrasses >> associated shrubs > perennial forbs > annual forbs > annual grasses.Other:
succulentsAdditional:
-
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Dead branches within individual shrubs common and standing dead shrub canopy material may be as much as 25% of total woody canopy; some of the mature bunchgrasses (<20%) have dead centers. -
Average percent litter cover (%) and depth ( in):
Between interspaces 5-10% cover and depth of litter is <1/4 inch. -
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
For normal or average growing season ± 100 lbs/ac. Favorable years 150 lbs/ac and unfavorable years 25 lbs/ac. -
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:
Potential invaders on this site include red brome, redstem filaree, Mediterranean grass, and annual mustards. -
Perennial plant reproductive capability:
All functional groups should reproduce in average (or normal) and above average growing season years. Little growth or reproduction occurs during drought years.
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