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Ecological site F030XC247NV
Pinus monophylla-Juniperus osteosperma/Cercocarpus ledifolius-Artemisia nova/Bouteloua gracilis
Last updated: 4/26/2024
Accessed: 07/14/2026
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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.
Ecological site concept
This forest site occurs on the back slopes of rock pediments. Slopes range from 15 to 50 percent. Elevations are 6000 to 8300 feet. The soils associated with this site are typically shallow to moderately deep and somewhat excessively drained. These soils have formed in alluvium from limestone.
Please refer to group concept F30XC252NV to view the provisional STM.Associated sites
F030XC243NV Pinus monophylla-Juniperus osteosperma/Purshia stansburiana-Artemisia nova/Bouteloua gracilis
Same soil series, lower elevation, lower site index. Stansbury's cliffrose major shrub component.
F030XC246NV Pinus monophylla-Juniperus osteosperma/Purshia stansburiana-Artemisia tridentata ssp. vaseyana/Poa fendleriana
Occurs on mountains, shallow soils.
F030XC249NV Pinus monophylla/Quercus gambelii/Poa fendleriana
Occurs on mountains on shallow soils at slightly higher elevations. Pinyon woodland.
Similar sites
F030XC243NV Pinus monophylla-Juniperus osteosperma/Purshia stansburiana-Artemisia nova/Bouteloua gracilis
Same soil series, lower elevation, lower site index. Stansbury's cliffrose major shrub component.
Table 1. Dominant plant species
Tree (1) Pinus monophylla
(2) Juniperus osteospermaShrub (1) Cercocarpus ledifolius
(2) Artemisia novaHerbaceous (1) Bouteloua gracilis
Physiographic features
This forest site occurs on the back slopes of rock pediments. Slopes range from 15 to 50 percent. Elevations are 6000 to 8300 feet.
Table 2. Representative physiographic features
Landforms (1) Pediment
Elevation 6000 – 8300 ft Slope 15 – 50 % Aspect Aspect is not a significant factor Climatic features
The primary air masses affecting the Spring Mountains are cold maritime polar air from the Gulf of Alaska and warmer, moist maritime subtropical air from lower latitudes. Occasionally there are invasions of cold continental polar air from northern Canada or the Rocky Mountains. Precipitation in the area results primarily from the passage of cyclones with associated fronts during fall, winter and spring; from closed cyclones in late winter and spring; and from the flow of moist tropical air from the southeast to the southwest quadrant in the summer.
The mean annual precipitation is about 12 to 16 inches. Mean annual air temperature is 41 to 45 degrees F. The average growing season is about 90 to 130 days.
Table 3 Representative climatic features
Frost-free period (average) 130 days Freeze-free period (average) Precipitation total (average) 20 in BarLineFigure 1. Monthly precipitation range
BarLineFigure 2. 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 are typically shallow to moderately deep and somewhat excessively drained. These soils have formed in alluvium from limestone. The soil surface is typically covered by approximately 70 percent gravel and 5 percent cobbles with a 20 percent discontinuous duff layer. The soil moisture is usually moist in late winter and spring, and periodically moist in the upper part following summer thunderstorms. The soil temperature regime is mesic, and the soil moisture regime is aridic bordering on ustic. Soil series associated with this site includes Doesprings.
Table 4. Representative soil features
Surface texture (1) Very gravelly loam
Family particle size (1) Loamy
Drainage class Somewhat excessively drained Permeability class Moderate Soil depth 10 – 39 in Surface fragment cover <=3" 60 – 80 % Surface fragment cover >3" 1 – 10 % Available water capacity
(0-40in)1.3 – 1.4 in Calcium carbonate equivalent
(0-40in)30 – 60 % Electrical conductivity
(0-40in)0 – 2 mmhos/cm Sodium adsorption ratio
(0-40in)0 – 5 Soil reaction (1:1 water)
(0-40in)7.9 – 8.4 Subsurface fragment volume <=3"
(Depth not specified)35 – 50 % Subsurface fragment volume >3"
(Depth not specified)2 – 4 % Ecological dynamics
Please refer to group concept F30XC252NV to view the provisional STM.
The pinyon-juniper forest is generally a climax vegetation type throughout its range, reaching climax about 300 years after disturbance, with an ongoing trend toward increased tree density and canopy cover and a decline in understory species over time. Singleleaf pinyon seedling establishment is episodic. Population age structure is affected by drought, which differentially reduces seedling and sapling recruitment more than other age classes. The ecotones between singleleaf pinyon forests and adjacent shrublands and grasslands provide favorable microhabitats for singleleaf pinyon seedling establishment since they are active zones for seed dispersal, nurse plants are available, and singleleaf pinyon seedlings are only affected by competition from grass and other herbaceous vegetation for a couple of years.
Several natural and anthropogenic processes can lead to changes in the spatial distribution of pinyon-juniper forests over time. These include 1) tree seedling establishment during favorable climatic periods, 2) tree mortality (especially seedlings and saplings) during periods of drought, 3) expansion of trees into adjacent grassland in response to overgrazing and/or fire suppression, and 4) removal of trees by humans, fire, or other disturbance episodes. Specific successional pathways after disturbance in singleleaf pinyon stands are dependent on a number of variables such as plant species present at the time of disturbance and their individual responses to disturbance, past management, type and size of disturbance, available seed sources in the soil or adjacent areas, and site and climatic conditions throughout the successional process.
Fire Ecology:
Wildfire is recognized as a natural disturbance that strongly influenced the structure and composition of the climax vegetation of this forest site. On high-productivity sites where sufficient fine fuels existed, singleleaf pinyon communities burn every 15 to 20 years, and on less productive sites with patchy fuels, fire return intervals may be in the range of 50 to 100 years or longer. Thin bark and lack of self pruning make singleleaf pinyon very susceptible to intense fire. Mature singleleaf pinyon can survive low-severity surface fires but is killed by more severe fires. Most tree seedlings are killed by fire, but cached seeds may survive.
Utah juniper is usually killed by fire, especially when trees are small. However, Utah juniper habitat types rarely have sufficient fine fuels to produce severe or continuous fires.
Black sagebrush is highly susceptible to fire-caused mortality; plants are readily killed by all fire intensities. Following burning, reestablishment occurs through off-site sources.
Major Successional Stages of Forest Development:
Herbaceous: Vegetation is dominated by grasses and forbs under full sunlight. This stage is experienced after a major disturbance such as crown fire. Skeleton forest (dead trees), remaining after fire or residual trees left following harvest, have little or no affect on the composition and production of the herbaceous vegetation.
Shrub Herbaceous: Herbaceous vegetation and woody shrubs dominate the site. Various amounts of tree seedlings (less than 20 inches in height) may be present up to the point where they are obviously a major component of the vegetal structure.
Sapling: In the absence of disturbance, tree seedling develops into saplings (20 inches to 4.5 feet in height) with a range in canopy cover of about 5 to 10 percent. Vegetation consists of grasses, forbs, and shrubs in association with tree samplings.
Immature Forest: The visual aspect and vegetal structure are dominated by Utah juniper trees and singleleaf pinyon trees greater than 4.5 feet in height. The upper crown of dominant and co-dominant trees are cone or pyramidal shaped. Seedling and saplings of pinyon and Utah juniper are present in the understory. Dominants are the tallest trees on the site; co-dominants are 65 to 85 percent of the highest of dominant trees. Understory vegetation is moderately influenced by a tree overstory canopy of about 10 to 25 percent.
Mature Forest: The visual aspect and vegetal structure are dominated by singleleaf pinyon and Utah juniper that have reached or are near maximal heights for the site. Dominant trees average greater than five inches in diameter at one-foot stump. Upper crowns of singleleaf pinyon adn Utah juniper are typically either irregularly or smoothly flat-topped or rounded. Tree canopy cover ranges from 30 to about 45 percent. Understory vegetation is strongly influenced by tree competition, overstory shading, duff accumulation, etc. Infrequent, yet periodic wildfire is presumed to be a natural disturbance influencing the understory of mature pinyon-juniper forests. This stage of community development is assumed to be representative of this forest site in the pristine environment.
Over-Mature Forest: In the absence of wildfire or other naturally occurring disturbances, the tree canopy on this site can become very dense. This stage is dominated by singleleaf pinyon and Utah juniper that have reached maximal heights for the site. Dominant and co-dominant trees average greater than five inches in diameter at one-foot stump height. Upper crowns are typically irregularly flat-topped or rounded. Understory vegetation is sparse or absent due to tree competition, overstory shading, duff accumulation, etc. Tree canopy cover is commonly greater than 50 percent.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 Plant CommunityCommunity 1.1
Reference Plant CommunityThe reference plant community is dominated by singleleaf pinyon and Utah juniper. An overstory canopy cover of about 35 percent is assumed to be representative of tree dominance on this site in the pristine environment. Overstory tree canopy composition is about 75 to 85 percent singleleaf pinyon, 15 to 10 percent Utah juniper and up to 10 percent curlleaf mountain mahogany. Muttongrass and blue grama are the most prevalent understory grasses. Black sagebrush and curlleaf mountainmahogany are the principal understory shrubs.
Forest overstory.Mature Forest: The visual aspect and vegetal structure are dominated by singleleaf pinyon and Utah juniper that have reached or are near maximal heights for the site. Dominant trees average greater than five inches in diameter at one-foot stump. Upper crowns of singleleaf pinyon adn Utah juniper are typically either irregularly or smoothly flat-topped or rounded. Tree canopy cover ranges from 30 to about 45 percent. Understory vegetation is strongly influenced by tree competition, overstory shading, duff accumulation, etc. Infrequent, yet periodic wildfire is presumed to be a natural disturbance influencing the understory of mature pinyon-juniper forests. This stage of community development is assumed to be representative of this forest site in the pristine environment. <br /> <br />
Forest understory. Muttongrass and blue grama are the most prevalent understory grasses. Black sagebrush and curlleaf mountainmahogany are the principal understory shrubs. Understory vegetative composition is about 15 percent grasses, 5 percent forbs and 80 percent shrubs and young trees when the average overstory canopy is representative (35 percent). Average understory production ranges from 500 to 700 pounds per acre with a representative canopy cover. Understory production includes the total annual production of all species within 4.5 feet from the ground surface.<br /> <br />
Table 5. Ground cover
Tree foliar cover 0% Shrub/vine/liana foliar cover 0% Grass/grasslike foliar cover 0% Forb foliar cover 0% Non-vascular plants 0% Biological crusts 0-0% Litter 0-20% Surface fragments >0.25" and <=3" 60-80% Surface fragments >3" 0-10% Bedrock 0% Water 0% Bare ground 20-40% Table 6. Canopy structure (% cover)
Height Above Ground (ft) Tree Shrub/Vine Grass/
GrasslikeForb <0.5 1-5% 1-5% 1-5% 1-5% >0.5 <= 1 1-5% 1-5% 1-5% 1-5% >1 <= 2 1-5% 1-5% – – >2 <= 4.5 1-5% 5-15% – – >4.5 <= 13 10-25% – – – >13 <= 40 25-35% – – – >40 <= 80 – – – – >80 <= 120 – – – – >120 – – – – Additional community tables
Table 7. Community 1.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Interpretations
Animal community
Livestock Interpretations:
This site is suited to cattle and sheep grazing during the summer and fall. Wild horses may use this site year round if water is available. Grazing management should be keyed to blue grama and muttongrass production. Livestock will often concentrate on this site taking advantage of the shade and shelter offered by the tree overstory. Many areas are not used because of steep slopes or lack of adequate water. Harvesting trees under a sound management program can open up the tree canopy to allow increased production of understory species desirable for grazing.
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:
This site has high value for mule deer during the summer, fall and winter. Singleleaf pinyon trees provide shelter from winter storms and juniper foliage is also browsed during the winter. Sites where water is available offer good quail habitat and are visited seasonally by mourning dove. Various songbirds, rodents, reptiles and associated predators native to the area also use it.
Hydrological functions
Runoff is very high. Permeability is moderate.
Recreational uses
This site has potential for hiking, cross-country skiing, camping, and deer and upland game hunting.
Wood products
Singleleaf pinyon wood is rather soft, brittle, heavy with pitch, and yellowish brown in color. Singleleaf pinyon has played an important role as a source of fuelwood and mine props. It has been a source of wood for charcoal used in ore smelting. It still has a promising potential for charcoal production. Other important uses for this tree are for Christmas trees and as a source of nuts for wildlife and human food.
Christmas trees: About 5 trees per acre per year in stands of medium canopy.
Utah juniper wood is very durable. Its primary uses have been for posts and fuelwood. It probably has considerable potential in the charcoal industry and in wood fiber products.
This forest community is of moderately high site quality for tree production. Site index ranges from 75 to 95. (Howell, 1940).
Productivity Class: 0
Fuelwood Production: 9 to 13 cord per acre for stands averaging 5 inches in diameter at 1 foot height with a medium canopy cover. There are about 289,000 gross British Thermal Units (BTUs) heat content per cubic foot of pinyon pine wood and about 274,000 gross BUTs heat content per cubic foot of Utah juniper. Solid wood volume in a cord varies but usually ranges from 65 to 90 cubic feet. Assuming an average of 75 cubic feet of solid wood per cord, there are about 21 million BTUs of heat value in a cord of mixed pinyon pine and Utah juniper.
Posts (7 foot): About 20 to 35 post per acres in stands of medium canopy.
Management Guides and Interpretations
1. Limitations and Considerations
a. Potential for sheet and rill erosion is moderate to severe depending on slope.
b. Moderate to severe equipment limitations on steeper slopes and moderate to severe equipment limitations on sties having extreme surface stoniness.
c. Proper spacing is the key to a well managed, multiple use and multi-product pinyon forest.
2. Essential Requirements
a. Harvest cut selectively or in small patches size dependent upon site conditions to enhance forage production.
1. Thinning and improvement cutting – Removal of poorly formed, diseased and low vigor trees for fuelwood.
2. Harvest cutting – Selectively harvest surplus trees to achieve desired spacing. Save large, healthy, full-crowned singleleaf pinyon trees for nut producers. Do no select only “high grade” trees during harvest.
3. Slash Disposal – Broadcasting slash improves reestablishment of native understory herbaceous species and establishment of seeded grasses and forbs after tree harvest.
4. Spacing Guide – D+9 (A higher spacing is required if managing for Christmas trees).
b. Prescription burning program to maintain desired canopy cover and manage site reproduction.
c. Mechanical tree removal (i.e. chaining) is not recommended on this site.
d. Pest control – Porcupines can cause extensive damage and populations should be controlled.
e. Fire hazard – Fire usually not a problem in well-managed, mature stands.
Other products
Pinyon-juniper ecosystems have had subsistence, cultural, spiritual, economic, aesthetic and medicinal value to Native American peoples for centuries, and singleleaf pinyon has provided food, fuel, medicine and shelter to Native Americans for thousands of years. The pitch of singleleaf pinyon was used as adhesive, caulking material, and a paint binder. It may also be used medicinally and chewed like gum. Pinyon seeds are a valuable food source for humans, and a valuable commercial crop. Thousands of pounds of nuts are gathered each year and sold on commercial markets throughout the United States.
Pinyon nuts: Production varies year to year, but mature stands can yield about 100 pounds per acre in favorable years.
Other information
Black sagebrush is an excellent species to establish on sites where management objectives include restoration or improvement of domestic sheep, pronghorn, or mule deer winter range.
There are 4 plant species of concern associated with this ecological site within the Spring Mountain National Recreational Area (SMNRA). There are also 3 animal species of concern.Table 8. Representative site productivity
Common name Symbol Site index low Site index high CMAI low CMAI high Age of CMAI Site index curve code Site index curve basis Citation singleleaf pinyon PIMO 75 95 10 12 – – – Supporting information
Type locality
Location 1: Clark County, NV Township/Range/Section T19 S R56 E S24 UTM zone N UTM northing 4025954n UTM easting 0621094e General legal description Approximately .5 miles north of Macks Canyon road, Spring Mountains, Clark County, Nevada. Other references
Clokey, I. 1951. Flora of the Charleston Mountains Clark County, Nevada. University of California Press, Berkeley and Los Angeles.
Fire Effects Information System [Online]http://www.fs.fed.us/feis
Glenne, G. and D. Johnson. 2002. Guide to Species of Concern in the Spring Mountains National Recreation Area, Clark and Nye Counties, Nevada. USFS, Las Vegas, NV.
Howell, J. 1940. Pinyon and juniper: a preliminary study of volume, growth, and yield. Regional Bulletin 71. Albuquerque, NM: USDA, SCS; 90 p.
Jordan, M., 1974. An Inventory of Two Selected Woodland Sites in the Pine Nut Hills of Western Nevada. MS Thesis, Univ. NV Reno.
Lanner, R.M. 1981. The Pinyon pine. A Natural and cultural history. University of Nevada Press. Reno, Nevada.
Nachlinger, J. and G. Reese. 1996. Plant Community Classification of the Spring Mountains National Recreation Area, Clark and Nye Counties, Nevada. The Nature Conservancy. Reno, Nevada.
USDA-NRCS. 2000. National Forestry Manual - Part 537. Washington, D.C.
West, N.E., R.J. Tausch, and P.T. Tueller. 1998. A management-oriented classification of pinyon-juniper woodlands of the Great Basin. USFS, Forest Service, Rocky Mountain Research Sta., Gen. Tech. Rep. RMRS-GTR-12. Section 322A:Pinyon-juniper woodlands of the Northern Mohave Desert. Page 22.
Contributors
TJW
Approval
Kendra Moseley, 4/26/2024
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 07/14/2026 Approved by Approval date Composition (Indicators 10 and 12) based on Annual Production Indicators
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Number and extent of rills:
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Presence of water flow patterns:
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Number and height of erosional pedestals or terracettes:
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Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
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Number of gullies and erosion associated with gullies:
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Extent of wind scoured, blowouts and/or depositional areas:
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Amount of litter movement (describe size and distance expected to travel):
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Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
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Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
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Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
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Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
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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:
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Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
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Average percent litter cover (%) and depth ( in):
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Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
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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:
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Perennial plant reproductive capability:
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