
Natural Resources
Conservation Service
Ecological site R047XY378CO
Mountain Stony Loam
Last updated: 2/11/2025
Accessed: 04/29/2025
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): 047X–Wasatch and Uinta Mountains
MLRA 47 occurs in Utah (86 percent), Wyoming (8 percent), Colorado (4 percent), and Idaho (2 percent). It encompasses approximately 23,825 square miles (61,740 square kilometers). The northern half of this area is in the Middle Rocky Mountains Province of the Rocky Mountain System. The southern half is in the High Plateaus of the Utah Section of the Colorado Plateaus Province of the Intermontane Plateaus. Parts of the western edge of this MLRA are in the Great Basin Section of the Basin and Range Province of the Intermontane Plateaus. The MLRA includes the Wasatch Mountains, which trend north and south, and the Uinta Mountains, which trend east and west. The steeply sloping, precipitous Wasatch Mountains have narrow crests and deep valleys. Active faulting and erosion are a dominant force in controlling the geomorphology of the area. The Uinta Mountains have a broad, gently arching, elongated shape. Structurally, they consist of a broadly folded anticline that has an erosion-resistant quartzite core. The Wasatch and Uinta Mountains have an elevation of 4,900 to about 13,500 feet (1,495 to 4,115 meters).
The mountains in this area are primarily fault blocks that have been tilted up. Alluvial fans at the base of the mountains are recharge zones for the basin fill aquifers. An ancient shoreline of historic Bonneville Lake is evident on the footslopes along the western edge of the area. Rocks exposed in the mountains are mostly Mesozoic and Paleozoic sediments, but Precambrian rocks are exposed in the Uinta Mountains. The Uinta Mountains are one of the few ranges in the United States that are oriented west to east. The southern Wasatch Mountains consist of Tertiary volcanic rocks occurring as extrusive lava and intrusive crystalline rocks.
The average precipitation is from 8 to 16 inches (203 to 406 mm) in the valleys and can range up to 73 inches (1854 mm) in the mountains. In the northern and western portions of the MLRA, peak precipitation occurs in the winter months. The southern and eastern portions have a greater incidence of high-intensity summer thunderstorms; hence, a significant amount of precipitation occurs during the summer months. The average annual temperature is 30 to 50 degrees Fahrenheit (-1 to 15 C). The freeze-free period averages 140 days and ranges from 60 to 220 days, generally decreasing in length with elevation.
The dominant soil orders in this MLRA are Aridisols, Entisols, Inceptisols, and Mollisols. The lower elevations are dominated by a frigid temperature regime, while the higher elevations experience cryic temperature regimes. Mesic temperature regimes come in on the lower elevations and south facing slopes in the southern portion of this MLRA. The soil moisture regime is typically xeric in the northern part of the MLRA, but grades to ustic in the extreme eastern and southern parts. The minerology is generally mixed and the soils are very shallow to very deep, generally well-drained, and loamy or loamy–skeletal.
LRU notes
E47C is the Uinta Mountains portion of MLRA 47 that run east and west which includes the Uinta Wilderness and The Flaming Gorge National Recreation Area and towns such as Evanston, Wyoming, Hanna and Tabiona, Utah. Structurally these mountains consist of a broadly folded anticline that has an erosion resistance quartzite core. The Duchesne River and many other tributaries to the Green River run through this range, as well as the headwaters of the Bear River.
Ecological site concept
The soils of this site formed mostly in colluvium from sandstone. Surface soils are very bouldery loam in texture. Rock fragments may be present on the soil surface and throughout the profile and make up more than 35 percent of the soil volume. These soils are deep to very deep, well-drained, and have moderate to moderately rapid permeability. pH is neutral. Available water-holding capacity ranges from 2.4 to 3.4 inches of water in the upper 60 inches of soil. The soil moisture regime is mostly ustic and the soil temperature regime is frigid. Precipitation ranges from 16 to 22 inches annually.
Associated sites
F048AY924CO |
Douglas Fir/Gambel Oak This site is a forested site with Douglas Fir and Gambel's oak as dominant plants. This site is found mostly commonly on mountain slopes, hillslopes, scarp slopes on cuestas, and mesas. Soils are moderately deep to very deep (20 to 60+ inches). Soil surface texture is loam, very stony loam, clay loam, stony sandy clay loam or very stony sandy loam. Subsurface textures can be loamy-skeletal or fine-loamy. It is usually ustic udic or typic ustic and frigid. It is a Douglas Fir – Gambel’s Oak – Arizona Fescue plant community. The effective precipitation ranges from 20 to 25 inches. |
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Similar sites
F047XC458UT |
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R047XC456UT |
Mountain Stony Loam (antelope bitterbrush) Dominant vegetation is bitterbrush. Surface soils are cobbly loam in texture and loamy-skeletal family particle size. The soils of this site formed in alluvium derived from sandstone and quartzite with some locations derived from dolomitic limestone. |
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Mountain Stony Loam (shrub) Dominant vegetation is Alderleaf Mountainmahogany and Utah serviceberry. Surface soils are extremely stony loam in texture and loamy-skeletal family particle size. The soils on this site were formed in slope alluvium and colluvium from sandstone and quartzite. The subsoils are extremely stony sandy clay loams. |
R047XC461UT |
Mountain Stony Loam (curl-leaf mountain mahogany) Dominant vegetation is Curlleaf Mountainmahogany. Surface soils are extremely bouldery loam in texture and loamy-skeletal family particle size. The soils on this site were formed in slope alluvium and colluvium derived from sandstone and quartzite. |
R047XC462UT |
Mountain Stony Loam (mountain big sagebrush) Dominant vegetation is mountain big sagebrush. Surface soils are very cobbly loam, extremely cobbly loam or stony loam in texture and loamy-skeletal family particle size. It formed in colluvium derived mainly from Duchesne River interbedded sandstone and shale, and uinta mountain sandstone and quartzite. |
Table 1. Dominant plant species
Tree |
Not specified |
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Shrub |
(1) Cercocarpus ledifolius |
Herbaceous |
Not specified |
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