
Natural Resources
Conservation Service
Ecological site R029XY009NV
UPLAND WASH
Last updated: 2/20/2025
Accessed: 04/10/2025
General information
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
MLRA notes
Major Land Resource Area (MLRA): 029X–Southern Nevada Basin and Range
The Southern Nevada Basin and Range MLRA (29) represents the transition from the Mojave Desert to the Great Basin. It is cooler and wetter than the Mojave. It is warmer and typically receives more summer precipitation than the Great Basin. This area is in Nevada (73 percent), California (25 percent), and Utah (2 percent). It makes up about 26,295 square miles (68,140 square kilometers). Numerous national forests occur in the area, including the San Bernardino, Angeles, Sequoia, Inyo, Humboldt-Toiyabe, and Dixie National Forests. Portions of Death Valley National Monument, the Nuclear Regulatory Commission’s Nevada Test Site, the Hawthorne Ammunition Depot, and the Nellis Air Force Range in Nevada and the China Lake Naval Weapons Center in California also are in this MLRA. The northeast part of the Paiute Indian Reservation and the southern third of the Walker River Indian Reservation are in the part of this MLRA in Nevada, and the Lone Pine, Fort Independence, and Big Pine Indian Reservations are in the part in California.
Physiography:
The entire area is in the Great Basin Section of the Basin and Range Province of the Intermontane Plateaus. The area of broad, nearly level, aggraded desert basins and valleys between a series of mountain ranges trending north to south. The basins are bordered by sloping fans and pluvial lake terraces. The mountains are uplifted fault blocks with steep side slopes and not well dissected due to limited annual precipitation. Most of the valleys in this MLRA are closed basins or bolsons containing sinks or playa lakes.
Geology:
The mountains are dominated by Pliocene and Miocene andesite and basalt rocks, Paleozoic and Precambrian carbonate rocks prominent in some areas. Scattered outcrops of older Tertiary intrusives and very young tuffaceous sediments (Pliocene and Miocene) are in the western and eastern thirds of this MLRA. The valleys consist mostly of alluvial fill and playa deposits at the lowest elevations in the closed basins.
Climate:
The average annual precipitation is 3 to 12 inches (75 to 305 millimeters) in most of this area. It may be as high as 29 inches (735 millimeters), on the higher mountain slopes. Most of the rainfall occurs as high-intensity, convective thunderstorms during the growing season. Summers are dry, but sporadic storms are common in July and August.
Water Resources:
Water resources are scarce. Ground water and surface water sources are limited. Streams are small and intermittent. Quality of surface water in naturally degraded as streams cross area of valley fill effected by dissolved salts. Irrigation water may raise the levels of dissolved salts and suspended sediments causing contamination.
Soils:
Dominant soil orders include Entisols and Aridisols.
Ecological site concept
The Upland Wash site occurs in drainageways on intermountain valley fans and active channels of hills and mountains and on inset fans of upper piedmont slopes. Slopes range from 2 to 15 percent, but slope gradients of 4 to 8 percent are most typical. Elevations are 3800 to 6200 feet. Flooding may occur occasionally and is very brief. The soils are deep alluvium from mixed sources. They are quite variable as they continue to be re-worked by water.
Associated sites
R029XY014NV |
SHALLOW CALCAREOUS SLOPE 8-12 P.Z. Black sagebrush dominated. This site occurs on summits and backslopes of hills and mountains, fan remnants, and rock pediments. Slopes range from 2 to over 75 percent, but slope gradients of 15 to 50 percent are typical. Elevations are 4300 to about 8800 feet. The soils on this site are calcareous or carbonatic and have a shallow effective rooting zone with depth to a hardpan or bedrock ranging from 5 to 20 inches. The soils have high amounts of gravels throughout the soil profile and are well drained to moderately well drained. The soil surface typically has a cover of 75 percent or more rock fragments. |
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R029XY077NV |
SHALLOW GRAVELLY LOAM 8-10 P.Z. This site occurs on fan remnants, lower mountain and hill sideslopes of all exposures. Slopes range from 2 to 50 percent. Elevations are 3600 to about 6500 feet. The soils are shallow to moderately deep and well drained. Surface soils are medium to coarse textured. Subsoils are generally heavy textured with a high percent of gravels. |
Similar sites
R029XY072NV |
VALLEY WASH ATCA2-AMER codominant |
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R029XY158NV |
COARSE LOAMY 8-10 P.Z. Stable plant community; ARTRW8-ATCA2 codominant |
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LOAMY FAN 8-12 P.Z. Stable plant community; ARTRW8 dominant shrub; LECI4-ACHY codominant grasses |
R029XY049NV |
SANDY LOAM 8-12 P.Z. Stable plant community; ARTRW8 dominant shrub |
R029XY041NV |
DRY WASH ARTR2 rare to absent; ERNAN5-ATCA2 codominant; lower elevations |
Table 1. Dominant plant species
Tree |
Not specified |
---|---|
Shrub |
(1) Artemisia tridentata |
Herbaceous |
(1) Poa secunda |
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