
Natural Resources
Conservation Service
Ecological site R028AY260UT
Semidesert Very Steep Shallow Loam (Black Sagebrush)
Last updated: 5/02/2025
Accessed: 10/19/2025
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.

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): 028A–Ancient Lake Bonneville
MLRA 28A occurs in Utah (82 percent), Nevada (16 percent), and Idaho (2 percent). It encompasses approximately 36,775 square miles (95,246 square kilometers). 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. Most of the valleys are closed basins containing sinks or playa lakes. Elevation ranges from 3,950 to 6,560 feet (1,204 to 2000 meters) in the basins and from 6,560 to 11,150 feet (1996 to 3398 meters) in the mountains. Much of the MLRA has alluvial valley fill and playa lakebed deposits at the surface from pluvial Lake Bonneville, which dominated this MLRA 13,000 years ago. A level line of remnant lake terraces on some mountain slopes indicates the former extent of this glacial lake. The Great Salt Lake is what remains of the pluvial lake.
Mountains in the interior of this MLRA consist of tilted blocks of marine sediments from Cambrian to Mississippian age with scattered outcrops of Tertiary continental sediments and volcanic rocks. The average annual precipitation is 5 to 12 inches (13 to 30 cm) in the valleys and ranges up to 49 inches (124 cm) in the mountains. Most of the rainfall in the southern LRU occurs as high-intensity, convective thunderstorms during the growing season (April through September). The driest period is from midsummer to early autumn in the northern LRU. Precipitation in winter typically occurs as snow. The average annual temperature is 39 to 53 °F (4 to 12 °C). The freeze-free period averages 165 days and ranges from 110 to 215 days, decreasing in length with increasing elevation. The dominant soil orders in this MLRA are Aridisols, Entisols, and Mollisols. Soils are dominantly in the mesic or frigid soil temperature regime, aridic or xeric soil moisture regime, and mixed mineralogy. The soils are generally well drained, loamy or loamy-skeletal, and very deep.
LRU notes
The Basin and Range North LRU exhibits dry summer with stronger xeric patterns than the Basin and Range South LRU. Ranges in the north LRU are about 50 percent Paleozoic sedimentary/metasedimentary (limestone/quartzite dominant) and about 10 percent Tertiary volcanics. The basin floors are between 4,200 and 5,100 feet (1,280 to 1,554 meters) in elevation. Pinyon and juniper sites have a greater percentage of Utah juniper (Juniperus osteosperma) in the plant community than pinyon pine (Pinus edulis or monophylla). The Basin and Range North have few semidesert ecological sites with Utah juniper. Cool season grasses, such as bluebunch wheatgrass (Pseudorogneria spicata), are dominant in the plant community, while warm season grasses are largely absent or a small component of the plant community.
Ecological site concept
The Semidesert Very Steep Shallow Loam (Black Sagebrush) site is found on very steep (greater than 50 percent slopes) hills and very steep scarp slopes between 5,260 to 8,740 feet. The soil is shallow to bedrock with over 40 percent rock fragments on the soil surface and subsurface. The surface texture is very cobbly loam. The dominant shrub in this site is black sagebrush (Artemisia nova) and the dominant grasses are bluebunch wheatgrass and Indian ricegrass (Achnatherum hymenoides). This site is similar to Semidesert Shallow Loam (black sagebrush), R028AA236UT. Semidesert Shallow Loam is found on slopes less than 50 percent and Semidesert Very Shallow Loam is found on slopes greater than 50 percent. Additional field works needs to be done to separate out the soils correlated to 260UT and 236UT to determine correct site correlation. Field work also needs to be done to better describe the range of characteristics within the reference state and any additional states that have not been identified.
Associated sites
R028AY262UT |
Semidesert Very Steep Shallow Loam (Utah Juniper) This site is found adjacent to the site and is on very shallow soils. |
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Similar sites
R028AY236UT |
Semidesert Shallow Loam (Black Sagebrush) North This site is located on hills and mountainsides on rocky, shallow soil. It is dominated by black sagebrush. It is on slopes less than 50 percent. |
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Table 1. Dominant plant species
Tree |
Not specified |
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Shrub |
(1) Artemisia nova |
Herbaceous |
Not specified |
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