
Natural Resources
Conservation Service
Ecological site R028AY038NV
UPLAND WASH
Last updated: 6/12/2025
Accessed: 10/22/2025
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): 028A–Ancient Lake Bonneville
MLRA 28A occurs in Utah (82%), Nevada (16%), and Idaho (2%). It makes up about 36,775 square miles. A large area west and southwest of Great Salt Lake is a salty playa. This area is the farthest eastern extent of the Great Basin Section of the Basin and Range Province of the Intermontane Plateaus. It is an area of nearly level basins between widely separated mountain ranges trending north to south. The basins are bordered by long, gently sloping alluvial fans. The mountains are uplifted fault blocks with steep side slopes. They are not well dissected because of low rainfall in the MLRA. Most of the valleys are closed basins containing sinks or playa lakes. Elevation ranges from 3,950 to 6,560 ft. in the basins and from 6,560 to 11,150 ft. in the mountains. Most of this area has alluvial valley fill and playa lakebed deposits at the surface. Great Salt Lake is all that remains of glacial Lake Bonneville. A level line on some mountain slopes indicates the former extent of this glacial lake. Most of the mountains in the interior of this area consist of tilted blocks of marine sediments from Cambrian to Mississippian age. Scattered outcrops of Tertiary continental sediments and volcanic rocks are throughout the area. The average annual precipitation is 5 to 12 ins. in the valleys and is as much as 49 ins. in the mountains. Most of the rainfall occurs as high-intensity, convective thunderstorms during the growing season. The driest period is from midsummer to early autumn. Precipitation in winter typically occurs as snow. The average annual temperature is 39 to 53 °F. The freeze-free period averages 165 days and ranges from 110 to 215 days, decreasing in length with elevation. The dominant soil orders in this MLRA are Aridisols, Entisols, and Mollisols. The soils in the area dominantly have a mesic or frigid soil temperature regime, an aridic or xeric soil moisture regime, and mixed mineralogy. They generally are well drained, loamy or loamy-skeletal, and very deep.
Ecological site concept
This site occurs on the inset fans of mid- to upper fan piedmonts, alluvial fans, and mountain valley fans, and along ephemeral stream channels. Slope gradients of 4 to 8 percent are most typical. Elevations are 5000 to 6500 feet.
Average annual precipitation is 8 to 12 inches. Mean annual air temperature is 50 to 55 degrees F. The average growing season is about 90 to 120 days.
The soils of this site are deep alluvium from mixed sources. Generally, these soils are gravelly or cobbly throughout. Water intake rates are rapid, available water capacity is low, runoff is medium and soils are well drained. These soils are subject to periodic flood flows associated with intense summer convection storms.
The reference state is variable, however, big sagebrush, Indian ricegrass, Nevada ephedra and rubber rabbitbrush are the major species associated with this site. Potential vegetative composition is about 20% grasses, 5% forbs and 75% shrubs. Approximate ground cover (basal and crown) is 20 to 35 percent. Production ranges from 500 to 1000 pounds per acre.
Associated sites
R028AY013NV |
SHALLOW CALCAREOUS LOAM 8-10 P.Z. |
---|---|
R028AY015NV |
LOAMY 8-10 P.Z. |
Similar sites
R028AY037NV |
VALLEY WASH Valley Wash. ARTR2 minor shrub, if present; ATAC2 & GRSP major shrubs. |
---|---|
R028AY031NV |
LOAMY FAN 8-10 P.Z. Loamy Fan 8-10 |
R028AY028NV |
DROUGHTY LOAM 8-10 P.Z. Droughty Loam 8-10 |
R028AY032NV |
DROUGHTY SODIC LOAM Droughty Sodic Loam. SAVE4-GRSP codominant shrubs; stable plant community. |
Table 1. Dominant plant species
Tree |
Not specified |
---|---|
Shrub |
(1) Artemisia tridentata |
Herbaceous |
(1) Achnatherum hymenoides |
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