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Ecological site R009XY035OR

Cold South 17-24 PZ

Accessed: 12/22/2024

Home / Esd catalog / MLRA 009X / Ecological site R009XY035OR

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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.

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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

R009XY018OR	Cold Loamy 17-24 PZ Mountain Loamy 17-24" PZ
R009XY022OR	Cold Shallow 13+ PZ Mountian Shallow 13"+ PZ
R009XY027OR	Cold Very Shallow 13+ PZ Mountain Very Shallow 13" + PZ

R009XY018OR

Cold Loamy 17-24 PZ

Mountain Loamy 17-24" PZ

R009XY022OR

Cold Shallow 13+ PZ

Mountian Shallow 13"+ PZ

R009XY027OR

Cold Very Shallow 13+ PZ

Mountain Very Shallow 13" + PZ

Similar sites

R009XY036OR	Cold Shallow South 13+ PZ Mountain Shallow South 13"+ PZ
R009XY034OR	Cold South 13-17 PZ Mountian South 13-17" PZ (lower Production)

R009XY036OR

Cold Shallow South 13+ PZ

Mountain Shallow South 13"+ PZ

R009XY034OR

Cold South 13-17 PZ

Mountian South 13-17" PZ (lower Production)

Table 1. Dominant plant species

Tree	Not specified
Shrub	Not specified
Herbaceous	Not specified

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Physiographic features

This site occurs near and within forestland on the backslopes of canyons, tablelands, and mountain plateaus north of the Wallowa Mountains. It is typicaly on slopes with south and southwest aspects as one of the last grassland sites before and within the forest. Slopes range from 12 to 60%. Elevation varies from 4000 to 5000 feet.

Table 2. Representative physiographic features

Landforms	(1) Mountain (2) Plateau (3) Canyon
Elevation	1,219 – 1,524 m
Slope	12 – 60%
Aspect	S, SW

Climatic features

The annual precipitaton ranges from 17 to 24 inches most of which occurs in the form of snow during the months of November through March followed by ample spring rainfall. Localized, occasionally severe, convectional storms occur during the summer. The soil temperature regime is frigid with a mean annual air temperature of 44 degrees F. Teh frost-free period ranges from 70 to 95 days. The optimum period for plant growth is from late March to late June.

Table 3. Representative climatic features

Frost-free period (average)	95 days
Freeze-free period (average)	0 days
Precipitation total (average)	610 mm

Bar

Line

Figure 2. Monthly average minimum and maximum temperature

Soil features

The soils of this site are moderately deep over basalt bedrock and are well drained. Areas of rock outcrop and talus are common. Typically the surface layer is a very cobbly silt loam to a very stony clay loam. The subsoil varies from a very cobbly clay loam to an extremely cobbly clay. Depth to bedrock is typically less than 30 inches. Permeabilty is moderately slow and the available water holding capacity (AWC) is aboyut 3 to 5 inches for the profile. The potential for erosion, particularly on steep slopes, is severe.

Table 4. Representative soil features

Surface texture	(1) Very cobbly silt loam (2) Very stony clay loam
Family particle size	(1) Clayey
Drainage class	Well drained
Permeability class	Moderately slow

Ecological dynamics

Range in Characteristics:
Changes in precipitation and elevation have little effect on composition and yeild. Steep due south slopes will ahve the most bluebunch wheatgrass. Idaho fescue will be highest in compostition on moderate southeasterly and westerly slopes. Production is lowest as the soil approaches 20 inches of depth and as coarse fragments increase. Soils close to 40 inches of depth and with few coarse fragments will have the highest propduction.
Response to Disturbance:
If the condition of the site deteriorates as a result of overgrazing, Idaho fescue decreases first followed by bluebunch wheatgrass. Unpalatable forbs increase. Canada and Kentucky bluegrass invade along with soft chess, cheatgrass, salsify and a variety of other unpalatable forbs. Under deteriorated conditions, annuals dominate, bare ground increases and excessive erosion in the bare interspaces reduces the potential of teh site and contributes to downstream sedimentation.

State and transition model

Custom diagram

Standard diagram

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More interactive model formats are also available. View Interactive Models
Click on state and transition labels to scroll to the respective text

Ecosystem states

1. Historic Climax Plant Community

State 1 submodel, plant communities

1.1. Historic Climax Plant Community

State 1
Historic Climax Plant Community

Community 1.1
Historic Climax Plant Community

The potential native plant community is dominated by bluebunch wheatgrass, Idaho fescue and cinquefoil. Sandberg bluegrass, lupine, arrowleaf balsamroot, yarrow, penstemon and a variety of other forbs are prominent in the stand. Rose and other shrubs are occasionally present. The vegetative composition of the community is approximately 85 percent grasses, 13 percent forbs and 2 percent shrubs.

Figure 3. Annual production by plant type (representative values) or group (midpoint values)

Table 5. Annual production by plant type

Plant type	Low (kg/hectare)	Representative value (kg/hectare)	High (kg/hectare)
Grass/Grasslike	1130	1538	1946
Forb	63	149	235
Shrub/Vine	31	47	63
Total	1224	1734	2244

Additional community tables

Table 6. Community 1.1 plant community composition

Group	Common name	Symbol	Scientific name	Annual production (kg/hectare)	Foliar cover (%)
Grass/Grasslike
1	Perennial Deep-rooted Dominant			1098–1883
	bluebunch wheatgrass	PSSP6	Pseudoroegneria spicata	785–1255	–
	Idaho fescue	FEID	Festuca idahoensis	314–628	–
4	Perennial Shallow-rooted Sub-dominant			31–63
	prairie Junegrass	KOMA	Koeleria macrantha	16–31	–
	Sandberg bluegrass	POSE	Poa secunda	16–31	–
Forb
7	Perennial All Dominant			31–94
	lupine	LUPIN	Lupinus	16–47	–
	cinquefoil	POTEN	Potentilla	16–47	–
8	Perennial All Sub-dominant			16–31
	common yarrow	ACMI2	Achillea millefolium	16–31	–
9	PPFF			16–110
	milkvetch	ASTRA	Astragalus	2–12	–
	arrowleaf balsamroot	BASA3	Balsamorhiza sagittata	2–12	–
	Indian paintbrush	CASTI2	Castilleja	2–12	–
	buckwheat	ERIOG	Eriogonum	2–12	–
	old man's whiskers	GETR	Geum triflorum	2–12	–
	Scouler's woollyweed	HISC2	Hieracium scouleri	2–12	–
	western stoneseed	LIRU4	Lithospermum ruderale	2–12	–
	beardtongue	PENST	Penstemon	2–12	–
	mule-ears	WYAM	Wyethia amplexicaulis	2–12	–
Shrub/Vine
13	Perennial Deciduous Dominant			31–63
	rose	ROSA5	Rosa	16–31	–
	common snowberry	SYAL	Symphoricarpos albus	16–31	–

Interpretations

Animal community

Livestock Grazing:
This site is suited to use by cattle and sheep in the late spring and fall. As this site often occurs on both steep and rocky slopes, these limitations need to be carefully considered in developing alternatives. Care should be taken to avoid trampling damage and soil compaction when soils are wet.
Wildlife:
This site is important as a late winter, early spring feeding site for deer and elk. It is often free of snow during the late winter and is one of the first soil areas to warm up. Early green forage is available. Adjacent forested areas provide valueable escape, hiding and thermal cover. As a critical site for deer and elk adverse impacts can easily result without careful management.
Native Wildlife Associated With The Potential Climax Community:
Rodents, Songbirds, Red-tailed hawk, Coyote, Rocky Mountian elk, and Mule deer.

Hydrological functions

The hydrologic cover condition is good at higher condidtion classes. The soils are in hydrologic group C.

Recreational uses

North of the Wallowa Mountains this site occurs in complex with other sites near and within forestland. It adds to the view with the distant mountains and high canyon slopes.

Other information

This site has a low potentail for range seeding because of coarse fragments being in complex with shallower sites and/or steepness of slope.

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
Contact for lead author	Oregon State Rangeland Management Specialist
Date	07/30/2012
Approved by	Bob Gillaspy
Approval date
Composition (Indicators 10 and 12) based on	Annual Production

Indicators

Number and extent of rills:
None to some, severe sheet & rill erosion hazard
Presence of water flow patterns:
None to some
Number and height of erosional pedestals or terracettes:
None to some
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
5-10%
Number of gullies and erosion associated with gullies:
None
Extent of wind scoured, blowouts and/or depositional areas:
None, slight wind erosion hazard
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 to significantly resistant to erosion; aggregate stability = 3-6
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Moderately deep, well drained, with areas of rock outcrop and talus and with a very cobbly silt loam to a very stony clay loam surface; low to moderate OM (1-3%)
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Significant ground cover (80-90%) and steep slopes (12-60%) moderately to 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:
Bluebunch wheatgrass > Idaho fescue > dominant forbs > other forbs > other grasses = shrubs

Sub-dominant:

Other:

Additional:
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: 1800, Normal: 1400, Unfavorable: 1000 lbs/acre/year at high RSI (HCPC)
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:
With deterioration of plant community, bluegrasses, annual bromes, and medusahead invade sites that have lost deep rooted perennial grass functional groups. Excessive erosion may occur, deteriorating site potential.
Perennial plant reproductive capability:
All species should be capable of reproducing annually

Download reference sheet