
Natural Resources
Conservation Service
Ecological site R024XY012NV
SALINE TERRACE 6-8 P.Z.
Last updated: 3/07/2025
Accessed: 03/14/2025
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): 024X–Humboldt Basin and Range Area
Major land resource area (MLRA) 24, the Humboldt Area, covers an area of approximately 8,115,200 acres (12,680 sq. mi.). It is found in the Great Basin Section of the Basin and Range Province of the Intermontane Plateaus. Elevations range from 3,950 to 5,900 feet (1,205 to 1,800 meters) in most of the area, some mountain peaks are more than 8,850 feet (2,700 meters).
A series of widely spaced north-south trending mountain ranges are separated by broad valleys filled with alluvium washed in from adjacent mountain ranges. Most valleys are drained by tributaries to the Humboldt River. However, playas occur in lower elevation valleys with closed drainage systems. Isolated ranges are dissected, uplifted fault-block mountains. Geology is comprised of Mesozoic and Paleozoic volcanic rock and marine and continental sediments. Occasional young andesite and basalt flows (6 to 17 million years old) occur at the margins of the mountains. Dominant soil orders include Aridisols, Entisols, Inceptisols and Mollisols. Soils of the area are generally characterized by a mesic soil temperature regime, an aridic soil moisture regime and mixed geology. They are generally well drained, loamy and very deep.
Approximately 75 percent of MLRA 24 is federally owned, the remainder is primarily used for farming, ranching and mining. Irrigated land makes up about 3 percent of the area; the majority of irrigation water is from surface water sources, such as the Humboldt River and Rye Patch Reservoir. Annual precipitation ranges from 6 to 12 inches (15 to 30 cm) for most of the area, but can be as much as 40 inches (101 cm) in the mountain ranges. The majority of annual precipitation occurs as snow in the winter. Rainfall occurs as high-intensity, convective thunderstorms in the spring and fall.
Ecological site concept
This ecological site is on fan piedmonts. Soils associated with this site are very deep, well drained and formed in alluvium derived from mixed rocks, loess and volcanic ash. The soil profile is characterized by an ochric epipedon, a sodium free surface, and moderately to strongly sodium effected subsoil. Soil textures are dominated by silt loam, ashy very fine silt loam, and/or ashy fine sandy loam. The soil temperature regime is mesic and the soil moisture regime is typic aridic.
This ecological site does not exhibit different abiotic factors or soil characteristics than winterfat dominated ESCs and full consideration should be given to correlating this ES to Silty 4-8" PZ (024XY004NV) as a CP or state.
Future field work in compare the soil characteristics and abiotic factors for all winterfat dominated ESCs in MRLA 24 and determine if they are actually one ESC. All soil correlated to these ESCs, regardless of depth, are dominated by silt loam textures (SiL, VFSL, FSL) or textures that are probably ashy.
Associated sites
R024XY004NV |
SILTY 4-8 P.Z. This ecological site is on fan piedmonts. Soils associated with this site are very deep, and well drained. The soil profile is characterized by an ochric epipedon, a sodium free surface, and moderately to strongly sodium effected subsoil. Soil textures are dominated by silt loam, ashy very fine silt loam, and/or ashy fine sandy loam. |
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R024XY007NV |
SALINE BOTTOM Saline Bottom ecological site is on alluvial flats, stream terraces and flood plains. Soils are very deep, somewhat poorly drained and formed in alluvium derived from mixed alluvium, loess and volcanic ash. The soil profile is characterized by an ochric epipedon, strong to moderate salinity throughout and a high water table between 70-100cm at some time during the year. |
R024XY011NV |
SODIC FLAT 6-8 P.Z. Important abiotic factors include crusting & baking of the surface layer upon drying, inhibiting water infiltration and seedling emergence. Greasewood (SAVE4) dominant shrub; Shadscale saltbrush (ATCO) minor shrub. |
R024XY020NV |
DROUGHTY LOAM 8-10 P.Z. Important abiotic factors contributing to the presence of this site include limited available soil moisture due to texture and precipitation zone. Vegetative cover is less than 25% and is dominated by deep-rooted, cool season perennial bunchgrasses and drought tolerant shrubs. Dominant species include Thurber’s needlegrass (ACTH7), Indian ricegrass (ACHY), Wyoming big sagebrush (ARTRW8), and spiny hopsage (GRSP). |
Similar sites
R024XY067NV |
SHALLOW SILTY 5-8 P.Z. Shadscale saltbush (ATCO) dominant shrub and squirreltail (ELEL5) dominant herbaceous. |
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R024XY060NV |
SHALLOW SILTY 8-10 P.Z. Shadscale saltbush (ATCO) dominant shrub; squirreltail (ELEL5) and indian ricegrass (ACHY) dominant herbaceous. |
R024XY004NV |
SILTY 4-8 P.Z. Winterfat (KRLA2) dominant shrub and Indian ricegrass (ACHY) dominant herbaceous; Sickle saltbush (ATFA) rare to absent. |
R024XY014NV |
COARSE SILTY 4-8 P.Z. Winterfat (KRLA2) dominant shrub and Indian ricegrass (ACHY) dominant herbaceous; Sickle saltbush (ATFA) rare to absent. |
Table 1. Dominant plant species
Tree |
Not specified |
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Shrub |
(1) Atriplex falcata |
Herbaceous |
(1) Achnatherum hymenoides |
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