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Conservation Service
Ecological site R010XA009OR
Juniper Shrubby Pumice Flat
10-12 PZ
Last updated: 3/26/2025
Accessed: 07/12/2026
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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.
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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.
MLRA notes
Major Land Resource Area (MLRA): 010X–Central Rocky and Blue Mountain Foothills
This MLRA is characterized by gently rolling to steep hills, plateaus, and low mountains at the foothills of the Blue Mountains in Oregon and the Central Rocky Mountains in Idaho. The geology of this area is highly varied and ranges from Holocene volcanics to Cretaceous sedimentary rocks. Mollisols are the dominant soil order and the soil climate is typified by mesic or frigid soil temperature regimes, and xeric or aridic soil moisture regimes. Elevation ranges from 1,300 to 6,600 feet (395 to 2,010 meters), increasing from west to east. The climate is characterized by dry summers and snow dominated winters with precipitation averaging 8 to 16 inches (205 to 405 millimeters) and increasing from west to east. These factors support plant communities with shrub-grass associations with considerable acreage of sagebrush grassland. Big sagebrush, bluebunch wheatgrass, and Idaho fescue are the dominant species. Stiff sagebrush, low sagebrush, and Sandberg bluegrass are often dominant on sites with shallow restrictive layers. Western juniper is one of the few common tree species and since European settlement has greatly expanded its extent in Oregon. Nearly half of the MLRA is federally owned and managed by the Bureau of Land Management. Most of the area is used for livestock grazing with areas accessible by irrigation often used for irrigated agriculture.
Ecological site concept
This ecological site occurs on nearly level basalt lava plains overlain by eolian pumice sands. Elevations range from 2,500 to 4,000 feet (750 to 1,200 meters) and slopes range from 0 to 10 percent but is typically less 3 percent. The soils associated with this site are moderately deep to deep to bedrock. The soil climate is mesic (soil temperature regime) and aridic (soil moisture regime). The reference plant community is characterized by an open stand of old growth western juniper, which are over 150 years old and express old growth morphological and structural characteristics. The interspaces between the trees (openings) are dominated by antelope bitterbrush and mountain big sagebrush over a diverse understory of grass species. Idaho fescue is the dominant grass on this site, with dense stands under the trees and within influence of the tree crowns. Interspaces between the trees express a more diverse mix of grasses including Idaho fescue, Thurber’s needlegrass, western needlegrass, and Indian ricegrass.
Associated sites
R010XA023OR Juniper Shrubby Lava Blisters 10-12 PZ
Occurs in complex with this site on pressure ridges of lava flows. Pumice sand mantle is shallow to bedrock and commonly mixed with rock outcrop.
Similar sites
R010XA027OR Juniper Pumice Flat 8-10 PZ
Lower precipitation and production. Understory dominated by mountain big sagebrush, and needle and thread grass.
R010XA021OR Juniper Shallow Pumice Hills 10-12 PZ
Frigid soil temperature regime. Understory dominated by mountain big sagebrush and Idaho fescue.
Table 1. Dominant plant species
Tree (1) Juniperus occidentalis
Shrub (1) Purshia tridentata
(2) Artemisia tridentata var. vaseyanaHerbaceous (1) Festuca idahoensis
Physiographic features
This site occurs on nearly level basalt lava plains. Slopes range from 0 to 10 percent, but are generally less than 3 percent. Elevations range from 2,500 to 4,000 feet.
Table 2. Representative physiographic features
Landforms (1) Lava plain > Lava plateau
Flooding frequency None Ponding frequency None Elevation 2500 – 4000 ft Slope 0 – 10 % Aspect Aspect is not a significant factor Climatic features
The annual precipitation ranges from 10 to 12 inches which occurs mainly between the months of October and June, mostly in the form of rain and snow. The average annual air temperature is 48 degrees F. with extreme temperatures ranging from -27 to 105 degrees F. The frost free period is 40 to 90 days. The optimum period for plant growth is from late March through June.
Table 3 Representative climatic features
Frost-free period (characteristic range) 50 days Freeze-free period (characteristic range) 100 days Precipitation total (characteristic range) 10-10 in Frost-free period (actual range) 50 days Freeze-free period (actual range) 100 days Precipitation total (actual range) 10-10 in Frost-free period (average) 50 days Freeze-free period (average) 100 days Precipitation total (average) 10 in Characteristic rangeActual rangeBarLineFigure 2. Monthly precipitation range
Characteristic rangeActual rangeBarLineFigure 3. Monthly minimum temperature range
Characteristic rangeActual rangeBarLineFigure 4. Monthly maximum temperature range
BarLineFigure 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) BEND 7 NE [USC00350699], Bend, OR
">Influencing water features
This site is not associated with riparian or wetland features.
Soil features
The soils of this site are moderately deep or deep to basalt bedrock. They are formed from eolian deposited pumice ash, primarily derived from Mt. Mazama. They are typically well drained and have an ashy sandy loam texture throughout the profile. Permeability is moderately rapid to rapid and the available water holding capacity is 3 to 7 inches for the profile. The potential for wind erosion is high. Soil temperature regime is mesic. Soil moisture regime is aridic.
Table 4. Representative soil features
Parent material (1) Basic volcanic ash
(2) Residuum – basalt
Surface texture (1) Ashy sandy loam
(2) Ashy loamy sand
Family particle size (1) Coarse-loamy
(2) Ashy
(3) Fine-loamy
Drainage class Well drained to somewhat excessively drained Permeability class Moderately rapid to rapid Soil depth 20 – 60 in Surface fragment cover <=3" 0 – 5 % Surface fragment cover >3" 0 – 5 % Available water capacity
(0-40in)3 – 7 in Calcium carbonate equivalent
(0-40in)Not specified Electrical conductivity
(0-40in)0 – 2 mmhos/cm Sodium adsorption ratio
(0-40in)Not specified Soil reaction (1:1 water)
(0-40in)6.6 – 7.8 Subsurface fragment volume <=3"
(0-60in)0 – 10 % Subsurface fragment volume >3"
(0-60in)0 – 5 % Ecological dynamics
This site occurs on nearly level lava plains overlain by eolian pumice sands and supports a juniper woodland plant community. These woodlands are characterized by an open stand of old growth western juniper, which are over 150 years old and express old growth morphological and structural characteristics. The interspaces between the trees (openings) are dominated by antelope bitterbrush and mountain big sagebrush over a diverse understory of grass species. Idaho fescue is the dominant grass on this site, with dense stands under the trees and within influence of the tree crowns. Interspaces between the trees express a more diverse mix of grasses including Idaho fescue, Thurber’s needlegrass, western needlegrass, and Indian ricegrass.
Woodland ecological sites existing on these eolian-volcanic sands collectively represent the most extensive old growth western juniper woodlands within the range of the species (Waichler et al. 2001). Trees in this region have been aged at over 1,600 years old and standing snags have been dated back to 100 BC. When compared to younger trees, old growth trees have a more rounded canopy shape with limited leader growth, deep vertical furrows in their bark, rot pockets, cavities, abundant arboreal lichen cover, and changing branch structure, including large basal branches. These woodlands have evolved over centuries and are relatively stable, resulting in the accumulation of dead wood in the form of snags, dead branches in live trees, logs, and weathered stumps (RMRS-GTR-403, pg 57). It also predominately stays aloft throughout the decay process, deteriorating more through abiotic weathering than biotic decomposition; greatly limiting contributions to soil organic matter and nitrogen pools (Waichler et al. 2001).
Western juniper is highly susceptible to fire, so old growth juniper woodlands are often isolated in fire resistant locations such as “rock outcrops, knolls, ridges, and/or soils that are shallow, coarse, rocky, and often high in clay or sand” (RMRS-GTR-403, pg 57). This site occurs on basalt lava plains overlain with moderately deep to deep pumice ash, primarily derived from Mt. Mazama. While soils on this site are deeper and have fewer course fragments than is typical of other old growth juniper sites, the soils on this site are geologically young; less than 7,000 years old, and primarily course pumice sands. Limited pedogenic development of these sandy soils in a low precipitation environment (10-12 inches annually) limits resources and results in a plant community that expresses large gaps between individual plants and limits overall understory production. Distance between trees and a discontinuous understory breaks up fine fuels and limits ladder fuels, typically containing fire events to one or several trees thereby creating the conditions for old growth woodlands to develop. Stand replacement fires and mixed-severity fires were historically rare (return intervals measured in centuries) (Tech Bulletin 152, 2005, pg 21 and RMRS-GTR-403, pg 112); meaning climatic conditions, such as severe drought, are the primary influence on tree mortality and establishment and understory dynamics.
In addition to influencing fire behavior, soil characteristics on this site drive species composition and production in the understory. While soil textures are coarse, the soil particles themselves are porous and can hold water in addition to the capillary water of the profile. Some of this water is plant available, greatly increasing the available water capacity (AWC) of the soil compared to non-pumice soils with similar textures. (Ecological Provinces, SR 990, pg 89). These pumice soils also have high albedo. The light color on the surface absorbs less sunlight and thus keeps the soil cooler than soils with darker A horizons. The porous nature of these soils also makes them very insulating, moderating subsurface temperatures, and keeping them cooler longer into the growing season. These unique characteristics result in a diverse species composition in the understory community that is typically more common on cooler, wetter, higher production sites. Spatial distribution of these understory species is further influenced by the size of the pumice sands. Redistribution of the pumice ash by wind resulted in varying surface textures across the site. The courser sands favor the needlegrasses, while the finer sands favor other species like Idaho fescue and bluebunch wheatgrass.
Paleobotany and Climate:
Western juniper first arrived in its current geographical range in Central Oregon between 4,800 to 6,600 years ago, during the mid Holocene era. Cool and moist conditions 4,000 to 3,000 years ago favored tree growth, cone production and seedling establishment, resulting in rapid expansion; Western juniper reached its prehistoric maximum across most of its present-day range during this period. A subsequent warm period 2,500 to 3,000 years ago caused severe droughts, major fires, and regional declines in western juniper stands. With the onset of the Little Ice Age conditions again became cooler and wetter and pollen records indicate juniper again began to gradually increase to its current range. (RMRS-GTR-403, pg 102-103). Under a natural disturbance regime, climate is the primary driver of juniper distribution and persistence, particularly in juniper woodlands. It directly influences seed production, seedling establishment, and plant mortality while also influencing other disturbances such as fire, competition, insects, and disease. (RMRS-GTR-403, pg 123)
Cool, moist conditions favor juniper expansion, while severe or extended drought and warmer conditions cause tree stress and mortality (RMRS-GTR-403, pg 102). Some mortality is the direct result of drought stress, while some trees succumb to secondary disturbances due to reduced vigor. Old trees are susceptible to heart-rots, which target the heartwood of the trunk and large limbs. Heart-rots rarely kill the tree but can structurally weaken them. Stressed trees are also more susceptible to mistletoe infestations and insects. In spite of vulnerabilities, western juniper is very resistant to many pressures. Overall, tree mortality in old growth juniper woodlands is typically low (RMRS-GTR-403, pg 42 to 48); estimated at less than one percent per century (RMRS-GTR-403, pg 111).
Western Juniper Woodland Infill:
While old growth juniper woodlands are relatively stable, they are not static. They have historically experienced cycles of infill and mortality in response to climatic conditions. With the end of the Little Ice Age in the 1850s, evidence suggests these woodlands were slowly expanding and infilling. Rate of infill throughout the Great Basin greatly accelerated in the late 1800s, peaking in the early 1900s. Infill rates slowed with the onset of widespread severe droughts starting in the 1920s. This acceleration coincides with a significant rise in settlement throughout the Intermountain West and is attributed to a combination of factors including climate, grazing, altered fire regimes, and increased CO2 levels (RMRS-GTR-403, pg 83, 104).
Woodland infill, precipitated by the end of the Little Ice Age, coincided with a time of rapid settlement and introduction of livestock grazing in the Great Basin, altering understory dynamics and fire behavior. Wetter periods, as were experienced during this timeframe, typically result in the accumulation of fine fuels (RMRS-GTR-403, pg 83). In addition to effects increased understory vegetation has on fire cycles, paleobotany literature suggests competition with herbaceous vegetation may limit tree seedling establishment and/or result in thinning. This indicates a robust understory can provide some competition to juniper establishment, limiting infill (RMRS-GTR-403, pg 112). Large numbers of domestic livestock grazing during this period prevented fine fuel accumulation and areas of heavy grazing would have resulted in understory plant stress. Without fire or competition, young juniper trees were able to rapidly establish.
Carbon dioxide (CO2) levels have also increased since the end of the Little Ice Age. Increased CO2 can increase water use efficiency in conifers relative to herbaceous species, resulting in faster tree growth and denser canopies (RMRS-GTR-403, pg 119). As climate conditions became warmer and drier in the early 1900s, expansion and infill slowed but still exceeded historic rates under similar conditions. This suggests CO2 concentrations and reduced competition from perennial grasses could be playing a significant role in current woodland expansion (RMRS-GTR-403, pg 121 and 123). These factors have resulted in altered stand structure in many persistent woodlands.
Infill trees compete with understory vegetation for water and other resources. Shrubs decline as trees increase in dominance, with sagebrush being highly sensitive to tree competition. Bitterbrush and Idaho fescue will persist longer as infill progresses, in part due to their superior shade tolerance relative to other species but will also eventually be removed from the site. (RMRS-GTR-403, pg 52; Miller et al., 2000) Herbaceous species are more resistant to tree competition, but also decline with increased tree dominance. Microclimate conditions under old growth trees shelter Idaho fescue, so interspace species are the first to decline. Understory decline is accelerated when plants are stressed by other disturbances such as drought, heavy grazing, or recreational use (RMRS-GTR-403, pg 48 to 55).
Non-Native Species:
With increased native plant understory stress and mortality, there is greater opportunity for establishment of non-native species and native increasers. This site is susceptible to cheatgrass, an invasive annual grass, and introduced annual forbs like pale madwort (Alyssum alyssoides). Medusahead and Ventenata dubia are not a concern on this site, as they typically do not establish in these coarse textured pumaceous soils. With repeated disturbance, sprouting shrubs (e.g. rabbitbrush species) and forbs (e.g. granite prickly phlox, Linanthus pungens and tansymustard Descurainia sp.) also increase and fill open spaces in the understory.
Over time, this can create fuel continuity that is atypical of old growth woodlands, making this site more prone to fire. Fires become more frequent and widespread. Higher tree densities from juniper infill also creates ladder fuels, making old trees more susceptible to fire, leading to more stand-replacing fires. (RMRS-GTR-403, pg 115). Recurring fires favor re-establishment of annual and sprouting species over native perennial grasses and shrubs, thereby perpetuating the fire cycle.
Resilience Management:
Within the natural range of variability under a normal distribution regime this site is resistant to disturbance, but has low resilience when disturbance occurs. Physiographic characteristics including proximity to rock outcrops and adjacent shallow soils as well as low fine fuel loads and minimal ladder fuels make this site very fire resistant. The site is also capable of withstanding extended drought with limited plant mortality. Disturbances outside of shifts in climate are not common resulting in a very stable site.
When disturbance occurs outside the normal range of variability the plant community shifts quickly and is very susceptible to invasion by non-native annual species. This low resilience is a result of the site’s limited resources (arid soil moisture regime and sandy soils) and warmer climate (mesic soil temperature regime).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 textT1A - Non-native species, fire, heavy grazing, and/or increased CO2 levels. R2A - Mechanical treatment of infill trees (non-old growth juniper); non-native species are not present. T2A - Time. R3A - Mechanical treatment of infill trees (non-old growth juniper). T3A - Time or stand replacement fire. State 1 submodel, plant communities
1.1A - Insects , drought stress, and/or small isolated fire. 1.2A - Time and favorable climatic conditions. State 2 submodel, plant communities
2.1A - Insects, drought, and/or small isolated fire. 2.2A - Time and favorable climatic conditions. State 3 submodel, plant communities
3.1A - Time. 3.2A - Disturbance removal and/or mechanical treatment of infill trees (non-old growth juniper). State 4 submodel, plant communities
4.1A - Stand replacement fire. 4.2A - Time and lack of fire. 4.3A - Fire. State 1
ReferenceThe Reference state is representative of the natural range of variability under pristine conditions. No introduced species occur in this state and disturbance has not fundamentally altered soil quality or plant community composition. This state represents a persistent old growth juniper woodland and has two general plant communities; a grass – shrub dominant community and a grass – forb dominated community. Both support an open stand of old growth juniper.
Negative feedbacks enhance ecosystem resilience and contribute to the stability of the state. These include the presence of all structural and functional groups and low fine fuel loads. Plant community phase changes are primarily driven by climate. Warm, dry cycles resulting in severe drought stresses plants and increases susceptibility to insects and disease. Cooler, wetter cycles that are conducive to tree establishment may result in woodland infill, and fine fuel accumulations may result in single tree or small area fires. Fire return interval is centuries.
Characteristics and indicators. • Lack of introduced plant species • Presence of all functional and structural groups • High plant vigor and reproductive capacity in most years
Resilience management. Management should focus on preservation of old growth juniper and prevention of non-native species establishment. Removal of infill trees to maintain pre-European infill rates can prevent transition to State 2.
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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antelope bitterbrush (Purshia tridentata), shrub
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mountain big sagebrush (Artemisia tridentata ssp. vaseyana), shrub
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Idaho fescue (Festuca idahoensis), grass
Community 1.1
Old Growth Juniper, Bitterbrush, Mountain Big Sagebrush, and Deep Rooted Perennial GrassesThis community is characterized by an open stand of old growth juniper. Occasional younger trees of varying ages are present in the understory or as a limited part of the overstory. The interspaces between the trees (openings) are dominated by antelope bitterbrush and mountain big sagebrush over a diverse understory of grass species. Idaho fescue is the dominant grass on this site, with dense stands under the trees and within influence of the tree crowns. Interspaces between the trees express a more diverse mix of grasses including Idaho fescue, Thurber’s needlegrass, western needlegrass, and Indian ricegrass. This community is very stable and the most common community in this state.
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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antelope bitterbrush (Purshia tridentata), shrub
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mountain big sagebrush (Artemisia tridentata ssp. vaseyana), shrub
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Idaho fescue (Festuca idahoensis), grass
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 465 590 700 Shrub/Vine 160 200 250 Tree 45 70 90 Forb 30 40 60 Total 700 900 1100 Figure 9. Plant community growth curve (percent production by month). OR4011 , B10A Mesic, Mid Elev., N/A, Good Condition. RPC Growth Curve (Pumice Flats).
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec J F M A M J J A S O N D 0 0 2 10 58 28 2 0 0 0 0 0 Community 1.2
Old Growth Juniper, Deep Rooted Perennial Grasses, and ForbsJuniper overstory has experienced isolated mortality as the result of small, single tree or small area fire; or drought and disease. This community is limited to the extent of the disturbance (usually a small, isolated area). Site is still characterized by an open stand of old growth juniper. Young trees (
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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Idaho fescue (Festuca idahoensis), grass
Pathway 1.1A
Community 1.1 to 1.2Insects (e.g. aroga moth), drought stress, and/or small isolated fire reduces shrubs and young juniper trees. Disturbance from drought and disease may be more widespread than fire.
Pathway 1.2A
Community 1.2 to 1.1Time and favorable climatic conditions (cooler/wetter climatic cycles) facilitate increase in shrub overstory.
State 2
Current Potential
This state is similar to the reference state yet some amount of introduced species occur and/or infill rates are exceeding pre-European settlement rates. Ecological function is largely intact, however the resiliency of the state has been reduced. This state represents a persistent old growth juniper woodland and has two general plant communities; a grass – shrub dominant community and a grass – forb dominated community. Both support an open stand of old growth juniper. Non-natives may increase in abundance but will not become dominant within this State.
Negative feedbacks enhance ecosystem resilience and contribute to the stability of the state. These include the presence of all structural and functional groups and low fine fuel loads. Positive feedbacks decrease ecosystem resilience and stability of the state. These include the non-natives’ high seed output, persistent seed bank, rapid growth rate, residual dry matter accumulation, and adaptations for seed dispersal.
Plant community phase changes are primarily driven by climate. Warm, dry cycles resulting in severe drought stresses plants and increases susceptibility to insects and disease. Cooler, wetter cycles that are conducive to tree establishment may result in woodland infill, and fine fuel accumulations may result in single tree or small area fires. Fire return interval is centuries.
Characteristics and indicators. • Presence of all functional and structural groups • High plant vigor and reproductive capacity in most years
Resilience management. Management should focus on preservation of old growth juniper and prevention of non-native species expansion. Removal of infill trees to maintain pre-European infill rates can prevent transition to State 3; or restore to Reference (State 1) if non-native species are not present.
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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antelope bitterbrush (Purshia tridentata), shrub
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mountain big sagebrush (Artemisia tridentata ssp. vaseyana), shrub
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Idaho fescue (Festuca idahoensis), grass
Community 2.1
Old Growth Juniper, Bitterbrush, Mountain Big Sagebrush, and Deep Rooted Perennial GrassesThis community is characterized by an open stand of old growth juniper. Occasional younger trees of varying ages are present in the understory or as a limited part of the overstory. The interspaces between the trees (openings) are dominated by antelope bitterbrush and mountain big sagebrush over a diverse understory of grass species. Idaho fescue is the dominant grass on this site, with dense stands under the trees and within influence of the tree crowns. Interspaces between the trees express a more diverse mix of grasses including Idaho fescue, Thurber’s needlegrass, western needlegrass, and Indian ricegrass. Annual non-native species may be present but not dominant. This community is very stable and the most common community in this state.
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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antelope bitterbrush (Purshia tridentata), shrub
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mountain big sagebrush (Artemisia tridentata ssp. vaseyana), shrub
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Idaho fescue (Festuca idahoensis), grass
Community 2.2
Old Growth Juniper, Deep Rooted Perennial Grasses, and ForbsJuniper overstory has experienced isolated mortality as the result of small, single tree or small area fire; or drought and disease. This community is limited to the extent of the disturbance (usually a small, isolated area). Site is still characterized by an open stand of old growth juniper. Young trees (
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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Idaho fescue (Festuca idahoensis), grass
Pathway 2.1A
Community 2.1 to 2.2Insects (e.g. aroga moth), drought stress, and/or small isolated fire reduces shrubs. Disturbance from drought and disease may be more widespread than fire.
Pathway 2.2A
Community 2.2 to 2.1Time and favorable climatic conditions (cooler/wetter climatic cycles) facilitate increase in shrub overstory.
State 3
Western Juniper InfillIn this state western juniper dominates the overstory and site resources. Young juniper (
Characteristics and indicators. • Western juniper infill trees are co-dominant with old growth trees or dominant in the overstory • Presence of all functional and structural groups, though diversity may be reduced • Bare ground patches are large and connected
Resilience management. Management should focus on preservation of old growth juniper and promoting native understory vigor and expansion. Removal of infill trees to release resources and reduce competition for native understory vegetation can help maintain State 3; or restore to Current Potential (State 2) if all functional groups and understory species are present.
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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antelope bitterbrush (Purshia tridentata), shrub
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mountain big sagebrush (Artemisia tridentata ssp. vaseyana), shrub
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Idaho fescue (Festuca idahoensis), grass
Community 3.1
Western Juniper, Bitterbrush, Mountain Big Sagebrush, and Deep Rooted Perennial Grasses
Western juniper dominates the overstory and site resources. Young trees are actively growing with noticeable leader growth. Shrubs and bunchgrasses are still present in the understory, but production has been reduced. Gaps between perennial plants have increased. Annual non-native species and perennial increasers are present, particularly in the interspaces.
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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antelope bitterbrush (Purshia tridentata), shrub
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mountain big sagebrush (Artemisia tridentata ssp. vaseyana), shrub
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Idaho fescue (Festuca idahoensis), grass
Community 3.2
Western Juniper (At Risk)Western juniper dominates the site. Trace amounts of bitterbrush and sagebrush may be present however dead skeletons will be more numerous than living brush. Deep-rooted bunchgrasses may or may not be present in the interspaces. Idaho fescue may still be present under the canopy of large trees. Bare ground interspaces are large and connected. Soil redistribution may be increasing, especially by wind . Annual non-native species and perennial increasers are present and increasing, particularly in the interspaces .
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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Idaho fescue (Festuca idahoensis), grass
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cheatgrass (Bromus tectorum), grass
Pathway 3.1A
Community 3.1 to 3.2Time allows for maturation of the tree community. Additional disturbances such as recreational vehicle use, repeated heavy grazing, and pressure from the urban interface that stress understory species accelerate this pathway.
Pathway 3.2A
Community 3.2 to 3.1Removal of disturbances such as recreational vehicle use, repeated heavy grazing, and pressure from the urban interface may allow understory species to increase vigor and expand in the understory if infill trees are not utilizing all site resources. Mechanical treatment of infill trees (non-old growth juniper) can also facilitate this pathway.
State 4
AnnualIn this state, perennial bunchgrasses and non-resprouting shrubs are greatly reduced or missing on the site. The understory has been replaced by non-native annual grasses and forbs, sprouting shrubs, and native increasers. Competition with the tree overstory and/or repeated disturbances such as fire, heavy grazing, and recreational use has allowed non-resprouting shrubs and perennial grasses to be replaced by cheatgrass, an invasive annual grass, and introduced annual forbs like pale madwort (Alyssum alyssoides). Forbs (e.g. granite prickly phlox , Linanthus pungens and tansymustard, Descurainia sp.) and sprouting shrubs (e.g. rabbitbrush species) also increase and fill open spaces in the understory.
This state may still support a western juniper overstory. If the site has not had a stand replacement fire, it will be a mix of old growth and young juniper. Following a stand replacement fire, the tree overstory will be temporarily lost. Time without disturbance will allow trees to reestablish. However, fuel continuity typical of annual dominated systems causes fires to become more frequent and widespread making replacement of old growth trees unlikely. Reestablishment of old growth trees would take centuries without disturbance (primarily fire), and feasibility of this pathway is currently unknown.
Characteristics and indicators. • Understory is dominated by cheatgrass and introduced annual forbs • Perennial grasses are greatly reduced or missing
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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yellow rabbitbrush (Chrysothamnus viscidiflorus), shrub
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rubber rabbitbrush (Ericameria nauseosa), shrub
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cheatgrass (Bromus tectorum), grass
Community 4.1
Old Growth Western Juniper and AnnualsAnnual non-native plants, native increaser forbs, and sprouting shrubs dominate this site. This community has a western juniper overstory that still supports old growth trees. Young trees (
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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yellow rabbitbrush (Chrysothamnus viscidiflorus), shrub
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rubber rabbitbrush (Ericameria nauseosa), shrub
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cheatgrass (Bromus tectorum), grass
Community 4.2
AnnualsThis community occurs after stand replacement fire. Annual non-native plants, native increaser forbs, and sprouting shrubs dominate this site. Scattered juniper or patches of juniper may persist, but the western juniper overstory has been removed.
Dominant plant species
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yellow rabbitbrush (Chrysothamnus viscidiflorus), shrub
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rubber rabbitbrush (Ericameria nauseosa), shrub
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cheatgrass (Bromus tectorum), grass
Community 4.3
Young Western Juniper and AnnualsAnnual non-native plants, native increaser forbs, and sprouting shrubs dominate this site. Western juniper has re-established in the overstory following a stand replacing fire.
Dominant plant species
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western juniper (Juniperus occidentalis), tree
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yellow rabbitbrush (Chrysothamnus viscidiflorus), shrub
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rubber rabbitbrush (Ericameria nauseosa), shrub
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cheatgrass (Bromus tectorum), grass
Pathway 4.1A
Community 4.1 to 4.2Stand replacement fire.
Pathway 4.2A
Community 4.2 to 4.3Time and lack of fire allows for sprouting shrubs such as rabbitbrush to increase, and potentially bitterbrush and sagebrush to establish. The probability of bitterbrush/sagebrush establishment is extremely low. Young juniper reestablishes.
Pathway 4.3A
Community 4.3 to 4.2Fire
Transition T1A
State 1 to 2Introduction of non-native species, altered fire regimes, repeated heavy grazing by domestic livestock, and/or increased CO2 levels.
Context dependence.The combination of multiple triggers increases likelihood of this transition.
Restoration pathway R2A
State 2 to 1Mechanical treatment of infill trees (non-old growth juniper); non-native species are not present.
Context dependence.Non-native species are not present.
Transition T2A
State 2 to 3Time and favorable conditions for tree expansion allow trees to become dominant.
Restoration pathway R3A
State 3 to 2Mechanical treatment of infill trees (non-old growth juniper).
Context dependence.Depleted understories may be slow to recover. Understory recovery may not be possible if anthropogenic disturbances are still stressing understory species. Restoration to State 2 is possible from Community 3.1 when all functional groups are still present, and site has maintained understory species diversity. Restoration from Community 3.2 is unlikely due to depleted understory.
Transition T3A
State 3 to 4Time allows for maturation of the tree community and loss of understory species; or stand replacement fire.
Constraints to recovery.Additional disturbances such as recreational vehicle use, repeated heavy grazing, and pressure from the urban interface that stress understory species accelerate this transition.
Additional community tables
Table 6. Community 1.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Grass/Grasslike1 Perennial Grasses/Grasslikes 455–690 Idaho fescue FEID Festuca idahoensis 180–450 – needle and thread HECO26 Hesperostipa comata 10–225 – Thurber's needlegrass ACTH7 Achnatherum thurberianum 45–50 – western needlegrass ACOC3 Achnatherum occidentale 20–45 – Indian ricegrass ACHY Achnatherum hymenoides 20–45 – thickspike wheatgrass ELLAL Elymus lanceolatus ssp. lanceolatus 20–40 – Ross' sedge CARO5 Carex rossii 10–20 – 2 Other Perennial Grasses 10–30 squirreltail ELEL5 Elymus elymoides 0–10 – bluebunch wheatgrass PSSPS Pseudoroegneria spicata ssp. spicata 0–10 – Sandberg bluegrass POSE Poa secunda 0–10 – Forb3 Perennial Forbs 30–60 common yarrow ACMI2 Achillea millefolium 0–20 – pussytoes ANTEN Antennaria 0–20 – buckwheat ERIOG Eriogonum 0–20 – slender buckwheat ERMI4 Eriogonum microthecum 0–20 – common starlily LEMO4 Leucocrinum montanum 0–20 – granite prickly phlox LIPU11 Linanthus pungens 0–20 – desertparsley LOMAT Lomatium 0–20 – lupine LUPIN Lupinus 0–20 – phacelia PHACE Phacelia 0–20 – spiny phlox PHHO Phlox hoodii 0–20 – Shrub/Vine4 Shrubs 90–250 antelope bitterbrush PUTR2 Purshia tridentata 45–180 – mountain big sagebrush ARTRV Artemisia tridentata ssp. vaseyana 45–90 – 5 Other Shrubs 0–50 yellow rabbitbrush CHVI8 Chrysothamnus viscidiflorus 0–20 – rubber rabbitbrush ERNA10 Ericameria nauseosa 0–20 – desert gooseberry RIVE Ribes velutinum 0–20 – Tree6 Tree 45–90 western juniper JUOC Juniperus occidentalis 45–90 – Table 7. Community 1.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 8. Community 2.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 9. Community 2.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 10. Community 3.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 11. Community 3.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 12. Community 4.1 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 13. Community 4.2 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Table 14. Community 4.3 plant community composition
Group Common name Symbol Scientific name Annual production () Foliar cover (%) Interpretations
Animal community
The unique morphological structure of old growth western juniper trees including hollows and cavities provide habitat for cavity nesting birds. A study in Central Oregon found cavity nesting birds were 2.7 times more abundant in old growth juniper woodlands than post settlement stands (Waichler et al. 2001).
Hydrological functions
The soils of this site have high infiltration rates and low runoff potential.
Wood products
Fence posts, firewood, and speciality products.
Supporting information
Inventory data references
Prineville District BLM Ecological Site Inventory NASIS component and pedon data Range Site Descriptions Field knowledge of range-trained personnel
Other references
Anderson, E. J., M. M. Borman, and W. C. Krueger. 1998. The Ecological Provinces of Oregon: a Treatise on the Basic Ecological Geography of the State., Oregon Agricultural Experiment Station. Special Report 990. (Oregon State University: Corvallis.)
Miller, R.F.; Bates, J.D.; Svejcar, T.J.; [et al.] E. Eddleman. 2005. Biology, ecology, and management of western juniper (Juniperus occidentalis). Tech. Bul. 152. Corvallis, OR: Oregon State University Agricultural Experiment Station. 82 p.
Miller, Richard F.; Chambers, Jeanne C.; Evers, Louisa; Williams, C. Jason; Snyder, Keirith A.; Roundy, Bruce A.; Pierson, Fred B. 2019. The ecology, history, ecohydrology, and management of pinyon and juniper woodlands in the Great Basin and Northern Colorado Plateau of the western United States. Gen. Tech. Rep. RMRS-GTR-403. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 284 p.
Waichler, W.S.; Miller, R.F.; Doescher, P.S. 2001. Community characteristics of old-growth western juniper woodlands. Journal of Range Management. 54(5): 518-527.Contributors
Bob Gillaspy
Cici Brooks
E Ersch
Gene Hickman
K.Kennedy
Jennifer Moffitt - 2025 Ecological dynamics and STM updatesApproval
Kirt Walstad, 3/26/2025
Acknowledgments
Dr. Richard Miller, Professor Emeritus Oregon State University - Thank you for reviewing this ecological site and providing valuable feedback.
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) Jeff Repp and Bruce Franssen. Contact for lead author State Rangeland Management Specialist for NRCS in Oregon. Date 04/24/2003 Approved by Approval date Composition (Indicators 10 and 12) based on Annual Production Indicators
-
Number and extent of rills:
None -
Presence of water flow patterns:
None -
Number and height of erosional pedestals or terracettes:
None -
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
15-30% -
Number of gullies and erosion associated with gullies:
None -
Extent of wind scoured, blowouts and/or depositional areas:
None to some -
Amount of litter movement (describe size and distance expected to travel):
Fine - limited movement -
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Moderately resistant to erosion: aggregate stability = 4-5 -
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Weak to moderate very fine granular structure, dry color value 4-5, 7-20 inches thick; low SOM (1-2%) -
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Significant ground cover (65-80%) and level to gently rolling slopes (0-20%) significantly limit rainfall impact and overland flow -
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:
Deep-rooted, perennial bunch-grassesSub-dominant:
Deciduous shrubs > evergreen shrubsOther:
perennial forbsAdditional:
-
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Normal decadence and mortality expected -
Average percent litter cover (%) and depth ( in):
-
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
Favorable: 1100, Normal: 900, Unfavorable: 700 lbs/acre/year at high RSI -
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:
Cheatgrass and Medusahead invade sites that have lost deep rooted perennial grass functional groups -
Perennial plant reproductive capability:
All species should be capable of reproducing annually
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