Natural Resources
Conservation Service
Ecological site R025XY022ID
LOAMY 16-22
Last updated: 4/25/2024
Accessed: 11/13/2024
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.
MLRA notes
Major Land Resource Area (MLRA): 025X–Owyhee High Plateau
MLRA Notes 25—Owyhee High Plateau
This area is in Nevada (56 percent), Idaho (30 percent), Oregon (12 percent), and Utah (2 percent). It makes up about 27,443 square miles. MLRA 25 is characteristically cooler and wetter than the neighboring MLRAs of the Great Basin. The western boundary is marked by a gradual transition to the lower and warmer basins of MLRA 24. The boundary to the south-southeast, with MLRA 28B, is marked by gradual changes in geology marked by an increased dominance of singleleaf pinyon and Utah juniper and a reduced presence of Idaho fescue. The boundary to the north, with MLRA 11, is a rapid transition from the lava plateau topography to the lower elevation Snake River Plain.
Physiography:
All of this area lies within the Intermontane Plateaus. The southern half is in the Great Basin section of the Basin and Range province. This part of the MLRA is characterized by isolated, uplifted fault-block mountain ranges separated by narrow, aggraded desert plains. This geologically older terrain has been dissected by numerous streams draining to the Humboldt River.
The northern half of the area lies within the Columbia Plateaus province. This part of the MLRA forms the southern boundary of the extensive Columbia Plateau basalt flows. Most of the northern half is in the Payette section, but the northeast corner is in the Snake River Plain section. Deep, narrow canyons draining into the Snake River have been incised into this broad basalt plain. Elevation ranges from 3,000 to 7,550 feet on rolling plateaus and in gently sloping basins. It is more than 9,840 feet on some steep mountains. The Humboldt River crosses the southern half of this area
Geology:
The dominant rock types in this MLRA are volcanic. They include andesite, basalt, tuff, and rhyolite. In the north and west parts of the area, Cretaceous granitic rocks are exposed among Miocene volcanic rocks in mountains. A Mesozoic igneous and metamorphic rock complex dominates the south and east parts of the area. Upper and Lower Paleozoic calcareous sediments, including oceanic deposits, are exposed with limited extent in the mountains. Alluvial fan and basin fill sediments occur in the valleys.
Climate:
The average annual precipitation in most of this area is typically 11 to 22 inches. It increases to as much as 49 inches at the higher elevations. Rainfall occurs in spring and sporadically in summer. Precipitation occurs mainly as snow in winter. The precipitation is distributed fairly evenly throughout fall, winter, and spring. The amount of precipitation is lowest from midsummer to early autumn. The average annual temperature is 33 to 51 degrees F. The freeze-free period averages 130 days and ranges from 65 to 190 days, decreasing in length with elevation. It is typically less than 70 days in the mountains.
Water:
The supply of water from precipitation and streamflow is small and unreliable, except along the Owyhee, Bruneau, and Humboldt Rivers. Streamflow depends largely on accumulated snow in the mountains. Surface water from mountain runoff is generally of excellent quality and suitable for all uses. The basin fill sediments in the narrow alluvial valleys between the mountain ranges provide some ground water for irrigation. The alluvial deposits along the large streams have the most ground water. Based on measurements of water quality in similar deposits in adjacent areas, the basin fill deposits probably contain moderately hard water. The water is suitable for almost all uses. The carbonate rocks in this area are considered aquifers, but they are little used. Springs are common along the edges of the limestone outcrops.
Soils:
The dominant soil orders in this MLRA are Aridisols and Mollisols. The soils in the area dominantly have a mesic or frigid temperature regime and an aridic, aridic bordering on xeric, or xeric moisture regime. Soils with aquic moisture regimes are limited to drainage or spring areas, where moisture originates or runs on and through. These soils are of a very limited extent throughout the MLRA. They generally are well drained, clayey or loamy, and shallow or moderately deep. Most of the soils formed in mixed parent material. Volcanic ash and loess mantle the landscape. Surface soil textures are loam and silt loam with ashy texture modifiers in some areas. Argillic horizons occur on the more stable landforms. They are exposed nearer the soil surface on convex landforms, where ash and loess deposits are more likely to erode. Soils that formed in carbonatic parent material in areas that receive less than 12 inches of precipitation are characterized by calcic horizons throughout the profile, while soils in areas that receive more than 12 inches of precipitation do not have calcic horizons in the upper part of the profile. Soils that formed on stable landforms at the lower elevations are dominated by ochric horizons. Soils that formed at the middle and upper elevations are characterized by mollic epipedons. Soils in drainage areas at all elevations that receive moisture running on or through them are characterized by thicker mollic epipedons.
Biological Resources:
This MLRA supports shrub-grass vegetation. Lower elevations are characterized by Wyoming big sagebrush associated with bluebunch wheatgrass, western wheatgrass, and Thurber’s needlegrass. Other important plants include bluegrass, squirreltail, penstemon, phlox, milkvetch, lupine, Indian paintbrush, aster, and rabbitbrush. Black sagebrush occurs but is less extensive. Singleleaf pinyon and Utah juniper occur in limited areas. With increasing elevation and precipitation, vast areas characterized by mountain big sagebrush or low sagebrush/early sagebrush in association with Idaho fescue, bluebunch wheatgrass, needlegrasses, and bluegrass become common. Snowberry, curl-leaf mountain mahogany, ceanothus, and juniper also occur. Mountains at the highest elevations support whitebark pine, Douglas-fir, limber pine, Engelmann spruce, subalpine fir, aspen, and curl-leaf mountain mahogany.
Major wildlife species include mule deer, bighorn sheep, pronghorn, mountain lion, coyote, bobcat, badger, river otter, mink, weasel, golden eagle, red-tailed hawk, ferruginous hawk, Swainson’s hawk, northern harrier, prairie falcon, kestrel, great horned owl, short-eared owl, long-eared owl, burrowing owl, pheasant, sage grouse, chukar, gray partridge, and California quail. Reptiles and amphibians include western racer, gopher snake, western rattlesnake, side-blotched lizard, western toad, and spotted frog. Fish species include bull, red band, and rainbow trout.
Classification relationships
Artemisia vaseyana/ Festuca idahoensis HT in “Hironaka, M., M.A. Fosberg, A. H. Winward. 1983. Sagebrush- Grass Habitat Types of Southern Idaho. University of Idaho. Moscow, Idaho. Bulletin Number 35”.
Ecological site concept
This site occurs on gently sloping to steep mountains. Slopes are nearly level to steep and range from 2 to 35 percent. It occurs on all aspects and elevations range from approximately 5500 to 7500 feet (1676-2286 meters). Except at upper elevations, this site occurs in areas of moisture accumulation such as bottoms or on east and north facing slopes.
The soils supporting this site are predominately deep to very deep, (Ola and Watchabob soils are moderately deep to bedrock), well drained, with moderately slow to moderately rapid permeability. Runoff is very low to very high, and increases with slope. The erosion hazard is slight to high by water, and moderate to high by wind. The available water holding capacity (AWC) is very low to moderate.
This site is dominated by a Wyoming big sagebrush and Idaho fescue community.
Associated sites
R025XY001ID |
ASPEN THICKET |
---|---|
R025XY010ID |
CLAYPAN 12-16 |
R025XY011ID |
LOAMY 13-16 |
R025XY018ID |
MAHOGANY SAVANNA 16-22 |
Similar sites
R025XY024ID |
LOAMY 12-16 |
---|---|
R025XY011ID |
LOAMY 13-16 |
Table 1. Dominant plant species
Tree |
Not specified |
---|---|
Shrub |
(1) Artemisia tridentata var. vaseyana |
Herbaceous |
(1) Festuca idahoensis |
Click on box and path labels to scroll to the respective text.
States 2 and 5 (additional transitions)
T1A | - | This transition develops through lack of fire and improper grazing management. The site has crossed the threshold. It is not economically feasible to move this state back towards state 1. |
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T1B | - | From community phase 1.3 or 1.5 this transition develops with no fire and improper grazing management. The site has crossed the threshold. It is not economically feasible to move this state back towards state 1. |
T2A | - | This transition is a result of brush management, pest management or prescribed fire prior to range seeding. |
T2B | - | This transition is a result of excessive soil loss and changes in the hydrologic cycle caused by improper grazing management or frequent fire. This state retrogresses to a new site with reduced potential. The site has crossed the threshold and is not economically feasible to move the state back towards state 1. |
T3A | - | This transition develops with fire. |
T3B | - | This transition develops from brush management, fire, or pest management in preparation for a range seeding. |
T3C | - | This transition is a result of improper grazing management and lack of fire. This state retrogresses to a new site with reduced potential due to significant soil loss and changes in hydrology. It has crossed the threshold, and it will not go back to state 1. |
State 1 submodel, plant communities
Communities 1, 5 and 6 (additional pathways)
1.1a | - | This pathway develops in the absence of fire. No juniper seed source is present. |
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1.1b | - | This pathway typically results from improper grazing management and absence of fire. Juniper seed source is present. |
1.1c | - | This pathway is a result of fire, either wildfire or prescribed burns. |
1.1d | - | This pathway develops in the absence of fire. Juniper seed source present. |
1.1e | - | This pathway is a result of improper grazing management and absence of fire. No juniper seed source is present. |
1.2a | - | This pathway is a result of fire. |
1.3a | - | This pathway is a result of prescribed burning or fire and prescribed grazing. |
1.3b | - | This pathway is a result of prescribed burning or fire. |
1.4a | - | This pathway develops with prescribed grazing and lack of fire. |
1.5a | - | This pathway is a result of prescribed burning or fire and prescribed grazing. |
1.5b | - | This pathway is a result of fire. |
1.6a | - | This pathway is a result of prescribed grazing, brush management and lack of fire. |
P1.6b | - | This pathway is a result from prescribed burning or fire. |