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Natural Resources
Conservation Service
Ecological site R048AY305CO
Alpine Meadow
Last updated: 3/05/2024
Accessed: 08/17/2024
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): 048A–Southern Rocky Mountains
MLRA 48A makes up about 45,920 square miles (119,000 square kilometers) and is the southern part of the Rocky Mountains. The Southern Rocky Mountains lies east of the Colorado Plateau, south of the Wyoming Basin, west of the Great Plains, and north of the Rio Grande Rift. It is in western and central Colorado, southeastern Wyoming, eastern Utah, and northern New Mexico. The headwaters of major rivers such as the Colorado, Yampa, Arkansas, Rio Grande, North Platte and South Plate rivers are located here. This MLRA has numerous national forests, including the Medicine Bow National Forest in Wyoming; the Routt, Arapaho, Roosevelt, Pike, San Isabel, White River, Gunnison, Grand Mesa, Uncompahgre, Rio Grande, and San Juan National Forests in Colorado; the Carson National Forest and part of the Santa Fe National Forest in New Mexico. Rocky Mountain National Park also is in this MLRA.
MLRA 48A is the southern Rocky Mountains physiographic region. The Southern Rocky Mountains consist primarily of two belts of strongly sloping to precipitous mountain ranges trending north to south. Several basins, or parks, are between the belts. Some high mesas and plateaus are included. It is characterized by mountain ranges that were uplifted during the Laramide Orogeny and then had periods of glaciation. The ranges include the Sangre de Cristo Mountains, the Laramie Mountains, and the Front Range in the east and the San Juan Mountains and the Sawatch and Park Ranges in the west. The ranges are dissected by many narrow stream valleys having steep gradients. In some areas the upper mountain slopes and broad crests are covered by snowfields and glaciers. Elevation typically ranges from 6,500 to 14,400 feet (1,980 to 4,390 meters) in this area. The part of this MLRA in central Colorado includes the highest point in the Rockies, Mount Elbert, which reaches an elevation of 14,433 feet (4,400 meters). More than 50 peaks in the part of the MLRA in Colorado are at an elevation of more than 14,000 feet (4,270 meters). Many small glacial lakes are in the high mountains.
The mountains in this area were formed mainly by crustal uplifts during the late Cretaceous and early Tertiary periods. This large MLRA can be subdivided into at least 4 large general divisions. First is the Rockies on the east side of this area are called the “Front Range,” which is a fault block that has been tilted up on edge and uplifted and is largely igneous and metamorphic geology. It was tilted up on the east edge, so there is a steep front on the east and the west side is more gently sloping and in the south east there are rocks exposed in the mountains are mostly Precambrian igneous and metamorphic rocks. Second is the tertiary rocks, primarily basalt and andesitic lava flows, tuffs, breccias, and conglomerates, are throughout this area (San Juan Mountains Area). The third division is Northwest part of the MLRA is dominantly sedimentary rock from the cretaceous/tertiary and Permian/ Pennsylvanian periods. The fourth subset is the long and narrow Sangre de Cristos mountains uplifted in the Cenozoic are between the Rio Grande rift and the great plains. Many of the highest mountain ranges were reshaped by glaciation during the Pleistocene. Alluvial fans at the base of the mountains are recharge zones for local basin and valley fill aquifers. They also are important sources of sand and gravel.
The average annual precipitation ranges predominantly from 12 to 63 inches. Summer rainfall commonly occurs as high-intensity, convective thunderstorms. About half of the annual precipitation occurs as snow in winter; this proportion increases with elevation. In the mountains, deep snowpacks accumulate throughout the winter and generally persist into spring or early summer, depending on elevation. Some permanent snowfields and small glaciers are on the highest mountain peaks. In the valleys at the lower elevations, snowfall is lighter and snowpacks can be intermittent. The average annual temperature is 26 to 54 degrees F (-3 to 12 degrees C). The freeze-free period averages 135 days and ranges from 45 to 230 days, decreasing in length with elevation. The climate of this area is strongly dependent upon elevation; precipitation is greater, and temperatures are cooler at the higher elevations. The plant communities vary with elevation, aspect and change in latitudes due to changing in precipitation kind and timing and temperature.
The dominant soil orders in this MLRA are Mollisols, Alfisols, Inceptisols, and Entisols. The soils in the area dominantly have a frigid or cryic soil temperature regime and an ustic or udic soil moisture regime. Mineralogy is typically mixed, smectitic, or paramicaceous. In areas with granite, gneiss, and schist bedrock, Glossocryalfs (Seitz, Granile, and Leadville series) and Haplocryolls (Rogert series) formed in colluvium on mountain slopes. Dystrocryepts (Leighcan and Mummy series) formed on mountain slopes and summits at the higher elevations. In areas of andesite and rhyolite bedrock, Dystrocryepts (Endlich and Whitecross series) formed in colluvium on mountain slopes. In areas of sedimentary bedrock, Haplustolls (Towave series) formed on mountain slopes at low elevations and with low precipitation. Haplocryolls (Lamphier and Razorba series), Argicryolls (Cochetopa series), and Haplocryalfs (Needleton series) formed in colluvium on mountain slopes at high elevations.
Classification relationships
NRCS:
Major Land Resource Area 48A, Southern Rocky Mountains (United States Department of Agriculture, Natural Resources Conservation Service, 2006).
USFS:
M331F- Southern Parks and Rocky Mountain Range Section Southern Rocky Mountain Steppe - Open Woodland - Coniferous Forest - Alpine Meadow
M331G – South Central Highlands Section Southern Rocky Mountain Steppe - Open Woodland - Coniferous Forest - Alpine Meadow
M331H – North Central Highlands and Rocky Mountains Section Southern Rocky Mountain Steppe - Open Woodland - Coniferous Forest - Alpine Meadow
M331I – North Parks and Ranges Section Southern Rocky Mountain Steppe - Open Woodland - Coniferous Forest - Alpine Meadow
M341B – Tavaputs Plateau Section M341 Nevada-Utah Mountains Semi-Desert - Coniferous Forest - Alpine Meadow (Cleland, et al., 2007).
EPA:
21a – Alpine Zone, 21b – Crystalline Subalpine Forests, 21c – Crystalline Mid-Elevations Forests, 21d -Foothill Shrublands, 21e – Sedimentary Subalpine Forests, 21f – Sedimentary Mid-Elevation Forests, 21g – Volcanic Subalpine Forests, and 21h – Volcanic Mid-Elevation Forests < 21 Southern Rockies < 6.2 Western Cordillera < 6 Northwestern Forested Mountains North American Deserts (Griffith, 2006).
20c – Semiarid Benchlands and Canyonlands and 20e - Escarpements < 20 Colorado Plateau < 10.1 Cold Deserts < 10 North American Deserts (Griffith, 2006).
USGS: Southern Rocky Mountain Province and the southern part of Unita Basin Section Colorado Plateaus Province
Ecological site concept
R048AY305CO Alpine Meadow occurs on depressions, drainageways, cirques, flood plains and steams. Slopes is between 0 to 15 percent. Soils are greater than 60 inches in depth. Soils are derived mostly from colluvium from Monzonite, volcanic rock; alluvium from volcanic rocks; or slope alluvium from Andesite or latite. Soil surface texture is loam, cobbly loam or silt loam. The underlying material to a depth of 60 inches or more is variable material ranging from sandy loam to clay loam with variable amounts and sizes of rock fragments. It is Kobresia – Tufted Hairgrass community. This site has a water table at 0 to 36 inches in depth. It has a Typic udic moisture regime and cryic temperature regime. The effective precipitation ranges from 30 to 50 inches.
Associated sites
R048AY250CO |
Subalpine Loam R048AY250CO Subalpine Loam occurs on hills, mountain-slopes, and mountains. Slopes is between 1 to 30%. Soils are deep to very deep (20 to 60+ inches). Soils are derived from colluvium and alluvium from volcanic rock; complex landslide deposits from igneous, metamorphic, and sedimentary rock; and slope alluvium, colluvium, residuum, alluvium or complex landslide deposits from sandstone and shale or shale. Soil surface texture is loam with loamy textured subsurface. It is a mountain big sagebrush – Thurber’s Fescue community. It has an ustic udic/typic udic moisture regime and cryic temperature regime. The effective precipitation ranges from 20 to 30 inches. |
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R048AY304CO |
Alpine Slopes R048AY304CO Alpine Slopes occurs on mountain-slopes, ridges, mountains and valleys. Slopes is between 30 to 60%. Soils are moderately deep to very deep (20 to 60+ inches). Soils are derived mostly from colluvium and alluvium from volcanic, metamorphic and igneous rocks. Soil surface texture is gravelly, very gravelly, extremely gravelly, very cobbly, extremely cobbly, or very stony loam or extremely stony sandy loam with loamy--skeletal subsurface. It is Kobresia – Tufted Hairgrass community. It has a Typic udic moisture regime and cryic temperature regime. The effective precipitation ranges from 30 to 50 inches. |
R048AY308CO |
Shallow Alpine R048AY308CO Shallow Alpine occurs mountain-slopes, ridges, mountains, basin floor, cirque floors, and valleys floors. Slopes is between 5 to 60%. Soils are shallow (7 to 20 inches). Soils are derived mostly from slope alluvium from tuff, rhyolite, andesite, basalt volcanic breccia, and other volcanic rocks; residuum from sandstone, tuff, rhyolite, volcanic breccia, basalt, andesite, and limestone; till from andesite, conglomerate or sedimentary rock; or colluvium from rhyolite, tuff, andesite, basalt, and other volcanic rocks. Soil surface texture is very gravelly, very stony, or very cobby loam; loam; very stony or very cobbly sandy loam, or very cobbly silt loam with loamy—skeletal or loamy subsurface. It is Kobresia – Tufted Hairgrass community. It has a Typic udic moisture regime and cryic temperature regime. The effective precipitation ranges from 30 to 50 inches. |
Similar sites
R048AY253CO |
Wet Subalpine R048AY253CO Wet Subalpine occurs on mesa tops and swales, drainageways, glacial moraines, and alluvial fans formed by glacial action. Slopes is between 0 to 30%. Soils are moderately deep to very deep (20 to 60+ inches). Soils are derived from till from basalt, andesite, or tuff; slope alluvium from andesite or tuff, alluvium from andesite or tuff; eolian deposits from basalt; or residuum from basalt. Soil surface texture is loam, or gravelly loam with fine-loamy, loamy-skeletal or clayey-skeletal textured subsurface. It is slender wheatgrass – tufted hairgrass. It has a Typic udic moisture regime and cryic temperature regime. The effective precipitation ranges from 37 to 45 inches. |
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R048AY241CO |
Mountain Meadow R048AY241CO Mountain Meadow occurs flood plains, stream terraces, drainageways, ephemeral streams, flood-plain step and depressions. This site has natural sub-irrigation. Slopes is between 0 to 12%. Soils are moderately deep to very deep (20 to 60+ inches). Soils are derived from alluvium from sandstone and shale, sedimentary rock, igneous, metamorphic and sedimentary rock, or shale. Soil surface texture is loam, silty clay loam, clay loam, clay, sandy clay loam or sandy loam with fine-loamy or fine textured subsurface. It has a typic aquic or oxyaquic ustic moisture regime. The effective precipitation ranges from 16 to 20 inches. |
R048AY304CO |
Alpine Slopes R048AY304CO Alpine Slopes occurs on mountain-slopes, ridges, mountains and valleys. Slopes is between 30 to 60%. Soils are moderately deep to very deep (20 to 60+ inches). Soils are derived mostly from colluvium and alluvium from volcanic, metamorphic and igneous rocks. Soil surface texture is gravelly, very gravelly, extremely gravelly, very cobbly, extremely cobbly, or very stony loam or extremely stony sandy loam with loamy--skeletal subsurface. It is Kobresia – Tufted Hairgrass community. It has a Typic udic moisture regime and cryic temperature regime. The effective precipitation ranges from 30 to 50 inches. |
R048AY306CO |
Shrubby Alpine R048AY306CO Shrubby Alpine occurs on cirque floors, mountains, mountain slopes and basin floor. Slopes is between 0 to 30%. Soils are greater than 60 inches in depth. Soils are derived mostly from till from conglomerate, sandstone or slope alluvium from basalt, rhyolite, andesite, tuff or volcanic breccia; or colluvium from andesite. Soil surface texture is very gravelly, cobbly, , or stony loam; or gravelly silt loam with loamy--skeletal subsurface. It is Kobresia – Tufted Hairgrass community. It has a Typic udic moisture regime and cryic temperature regime. The effective precipitation ranges from 30 to 50 inches. |
R048AY308CO |
Shallow Alpine R048AY308CO Shallow Alpine occurs mountain-slopes, ridges, mountains, basin floor, cirque floors, and valleys floors. Slopes is between 5 to 60%. Soils are shallow (7 to 20 inches). Soils are derived mostly from slope alluvium from tuff, rhyolite, andesite, basalt volcanic breccia, and other volcanic rocks; residuum from sandstone, tuff, rhyolite, volcanic breccia, basalt, andesite, and limestone; till from andesite, conglomerate or sedimentary rock; or colluvium from rhyolite, tuff, andesite, basalt, and other volcanic rocks. Soil surface texture is very gravelly, very stony, or very cobby loam; loam; very stony or very cobbly sandy loam, or very cobbly silt loam with loamy—skeletal or loamy subsurface. It is Kobresia – Tufted Hairgrass community. It has a Typic udic moisture regime and cryic temperature regime. The effective precipitation ranges from 30 to 50 inches. |
R048AY309CO |
Warm Alpine R048AY309CO Warm Alpine occurs mountain-slopes, alluvial fan and valleys. Slopes is between 10 to 60%. Soils are moderately deep to very deep (20 to 60+ inches). Soils are derived mostly from alluvium from rhyolite, slope alluvium from rhyolite, tuff, sandstone and volcanic rocks or colluvium from rhyolite, tuff, and volcanic rocks. Soil surface texture very gravelly loam, loam or very stony sandy loam with loamy--skeletal subsurface. It is Thurber’s Fescue community. It has a Typic udic moisture regime and cryic temperature regime. The effective precipitation ranges from 30 to 50 inches. |
Table 1. Dominant plant species
Tree |
Not specified |
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Shrub |
Not specified |
Herbaceous |
(1) Kobresia myosuroides |
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