Natural Resources
Conservation Service
Ecological site F043AX954MT
Upper Subalpine Cold Coniferous subalpine fir (Engelmann spruce) /thinleaf huckleberry-rusty menziesia/ Hitchcock’s smooth woodrush-beargrass/yellow avalanche lily.
Last updated: 9/09/2023
Accessed: 12/22/2024
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): 043A–Northern Rocky Mountains
This MLRA is located in Montana (43 percent), Idaho (34 percent), and Washington (23 percent). It makes up about 31,435 square miles (81,460 square kilometers). It has no large cities or towns. It has many national forests, including the Okanogan, Colville, Kootenai, Lolo, Flathead, Coeur d’Alene, St. Joe, Clearwater, and Kaniksu National Forests.
This MLRA is in the Northern Rocky Mountains Province of the Rocky Mountain System. It is characterized by rugged, glaciated mountains; thrust- and block-faulted mountains; and hills and valleys. Steep-gradient rivers have cut deep canyons. Natural and manmade lakes are common.
The major Hydrologic Unit Areas (identified by four-digit numbers) that make up this MLRA are: Kootenai-Pend Oreille-Spokane (1701), 67 percent; Upper Columbia (1702), 18 percent; and Lower Snake (1706), 15 percent. Numerous rivers originate in or flow through this area, including, the Sanpoil, Columbia, Pend Oreille, Kootenai, St. Joe, Thompson, and Flathead Rivers.
This area is underlain primarily by stacked slabs of layered sedimentary or metasedimentary bedrock. The bedrock formations range from Precambrian to Cretaceous in age. The rocks consist of shale, sandstone, siltstone, limestone, argillite, quartzite, gneiss, schist, dolomite, basalt, and granite. The formations have been faulted and stacked into a series of imbricate slabs by regional tectonic activity. Pleistocene glaciers carved a rugged landscape that includes sculpted hills and narrow valleys filled with till and outwash. Continental glaciation over road the landscape in the northern half of the MLRA while glaciation in the southern half was confined to montane settings.
The average annual precipitation is 25 to 60 inches (635 to 1,525 millimeters) in most of this area, but it is as much as 113 inches (2,870 millimeters) in the mountains and is 10 to 15 inches (255 to 380 millimeters) in the western part of the area. Summers are dry. Most of the precipitation during fall, winter, and spring is snow. The average annual temperature is 32 to 51 degrees F (0 to 11 degrees C) in most of the area, decreasing with elevation. In most of the area, the freeze-free period averages 140 days and ranges from 65 to 215 days. It is longest in the low valleys of Washington, and it decreases in length with elevation. Freezing temperatures occur every month of the year on high mountains, and some peaks have a continuous cover of snow and ice.
The dominant soil orders in this MLRA are Andisols, Inceptisols, and Alfisols. Many of the soils are influenced by Mount Mazama ash deposits. The soils in the area have a frigid or cryic soil temperature regime; have an ustic, xeric, or udic soil moisture regime; and dominantly have mixed mineralogy. They are shallow to very deep, are very poorly drained to well drained, and have most of the soil texture classes. The soils at the lower elevations include Udivitrands, Vitrixerands and Haplustalfs. The soils at the higher elevations include Dystrocryepts, Eutrocryepts, Vitricryands , and Haplocryalfs. Cryorthents, Cryepts, and areas of rock outcrop are on ridges and peaks above timberline
This area is in the northern part of the Northern Rocky Mountains. Grand fir, Douglas-fir, western red cedar, western hemlock, western larch, lodgepole pine, subalpine fir, ponderosa pine, whitebark pine, and western white pine are the dominant overstory species, depending on precipitation, temperature, elevation, and landform aspect. The understory vegetation varies, also depending on climatic and landform factors. Some of the major wildlife species in this area are whitetailed deer, mule deer, elk, moose, black bear, grizzly bear, coyote, fox, and grouse. Fish, mostly in the trout and salmon families, are abundant in streams, rivers, and lakes.
More than one-half of this area is federally owned and administered by the U.S. Department of Agriculture, Forest Service. Much of the privately-owned land is controlled by large commercial timber companies. The forested areas are used for wildlife habitat, recreation, watershed, livestock grazing, and timber production. Meadows provide summer grazing for livestock and big game animals. Less than 3 percent of the area is cropland.
LRU notes
This ecological site resides in MLRA 43A in the Livingston-Lewis-Apgar Mountains which includes the bulk of Glacier National Park (GNP) and the lower western valley portions along the Flathead River. The landscape is mountains and landforms include glaciated mountains with associated features such as U-shaped valleys, mountain slopes, alpine ridges, cirques, valley floors and moraines. Glaciation of this area was in the form of alpine, icecaps and valley outlet glaciers. It also includes associated alluvium and outwash features. This area includes low valleys to tall mountains with elevation ranging 989-2,762 m (3,250-9,050 ft.). The climate is cold and wet with mean annual air temperature of 3 degrees Celsius (37 degrees F.), mean frost free days of 65 days and mean annual precipitation of 1295 mm (51 in.) and relative effective annual precipitation is 169 cm (66 in.). The soil temperature regime is cryic and the soil moisture regime is udic. The geology of this area is dominated by metasedimentary rocks of the Belt Supergroup (Grinnell argillite and Siyeh limestone) with minor Tertiary sediments. Soils are generally weakly developed on mountain slopes within U-shaped valleys. Parent materials are commonly of colluvium, till, and residuum from metasedimentary rocks. Limestone bedrock within this part of the Belt Supergroup is not highly calcareous and due to high precipitation received in this area most carbonates at mid and upper elevations have been leached from the soil profiles. Bedrock depth varies greatly with location, landform and slope position. Volcanic ash is often found in the soil surface with various degrees of mixing. Thicker volcanic ash can be found on more stable positions on mid and upper elevation slopes that are protected from wind erosion. Volcanic ash is not typically found in low elevation areas on stream and outwash terraces associated with streams and rivers. There are numerous large lakes including St. Mary, Bowman, Kintla, Lake Sherburne, Logging, Upper Waterton and numerous creeks (
Classification relationships
This ecological site relates to the USFS Habitat Type ABLA/LUGLH. This site relates to the USFS Habitat Type Group 10 and Fire Group 10. Both of these classification guides are specifically for the western Montana and northern Idaho region. It also relates to the National Park Service, NatureServe classification Abies lasiocarpa-Picea engelmannii/Luzula glabrata var. hitchcockii Woodland CEGL000317.
Ecological site concept
The 43A Upper Subalpine Cold Coniferous ecological site is found along the Continental Divide in cold, moist to moderately dry, high elevation sites that span the upper subalpine zone. These sites are above the cold limits of Douglas-fir (Pseudotsuga menziesii), western white pine (Pinus monticola), western larch (Larix occidentalis), with common species including whitebark pine (Pinus albicaulis), lodgepole pine (Pinus contorta), mountain hemlock (Tsuga mertensiana), subalpine fir (Abies lasiocarpa), Engelmann spruce (Picea engelmannii), and subalpine larch (Larix lyallii). Subalpine fir dominates the Reference State with the long-lived seral species whitebark pine and Engelmann spruce. Subalpine fir is tall, usually growing more than 50 feet tall at maturity and is not stunted in the krummholtz form. The understory is not diverse, rather it is composed of only a few important species. Shrubs include rusty menziesia (Menziesia ferruginea), grouse whortleberry (Vaccinium scoparium), pink mountainheath (Phyllodoce empetriformis), and yellow mountainheath (Phyllodoce glanduliflora). There may be high cover of grouse whortleberry and/or Hitchcocks smooth woodrush, which are indicative of cold conditions. Common forbs are broadleaf arnica, beargrass, Rosss sedge, Idaho fescue, Parrys rush, and Hitchcocks smooth woodrush. The soils associated with this ecological site are moderately deep, well drained and derived from glacial till or colluvium over residuum weathered from metasedimentary rock. Moderately deep depth class indicates that these soils are greater than 50 cm (20 inches) deep, but less than 100 cm (40 inches). These soils classify in the Inceptisols soil order and in the Typic Haplocryepts taxonomic subgroup. Less common soil taxa found in association with this ecological site are the Andic subgroups, indicating the presence of volcanic ash, and in minor extent soils of the Andisols soil order.
Associated sites
R043AX963MT |
Alpine Shallow Meadow yellow avalanche-lily-Scouler’s St. Johnswort-alpine leafybract aster-Sitka valerian- heartleaf arnica/Hitchcock’s smooth woodrush The 43A Alpine Shallow Meadow ecological site is found on a wide range of high elevation sites that share in common cold winter temperatures, heavy snow loading, and a short growing season. These are large patch size meadows. These sites are on backslopes, with generally slopes below 35 percent, but can be found on steep backslope positions, and on all aspects. It is found at the base of talus slopes and on large, broad areas on colluvial aprons. It also is found in linear areas between ribbons of high elevation forests found on cirque platforms and headwalls, roche moutonées, or scoured bedrock knobs and hills, and saddles. The 43A Alpine Shallow Meadow ecological site is found on soils that are shallow to moderately deep, well drained, have a high amount of rock fragments, and form from till or colluvium over residuum soil parent materials. These soils very rarely have a surface organic layer, and it is typically less than 5 cm deep if it occurs. The 43A Alpine Shallow Meadow ecological site has a reference vegetation community of Yellow avalanche-lily (Erythronium grandiflorum), Scouler’s St. Johnswort (Hypericum scouleri), alpine leafybract aster (Symphyotrichum foliaceum), Sitka valerian (Valeriana sitchensis), heartleaf arnica (Arnica cordifolia), Hitchcock’s smooth woodrush (Luzula glabrata var. hitchcockii) and shortstalk sedge (Carex podocarpa). |
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F043AX956MT |
Subalpine Coniferous Cool Moderately Dry subalpine fir (Abies lasiocarpa) / Engelmann spruce (Picea engelmannii) The 43A Subalpine Cool Dry Coniferous, (ABLA/XETE) ecological site is found in cool, moderately dry mid-elevation areas that span the lower subalpine to subalpine. It is found primarily on foot and backslope positions on lateral moraine and cirque floor landforms at elevations ranging from 1,300 to 2,600 meters (4,250-8,500 feet) on various slope inclinations ranging from 15 to 80 percent.The 43A Subalpine Cool Dry Coniferous, (ABLA/XETE): Soil associated with this ecological site are very deep, well drained and formed in volcanic ash over glacial till or colluvium parent material. The origin of the volcanic ash is from the eruption of Mount Mazama (Crater Lake, Oregon) and occurs as a surface mantle on these soils. Due to the parent materials that these soils form in they generally have many rock fragments in the subsurface below the volcanic ash surface layers. These soils are classified in the Inceptisols soil order and more specifically in the Andic Haplocryepts subgroup.The 43A Subalpine Cool Dry Coniferous, (ABLA/XETE) has a reference vegetation community of an overstory of Subalpine fir (with minor Engelmann spruce) and an understory of Utah honeysuckle, thinleaf huckleberry, beargrass and Western meadowrue. |
F043AX952MT |
Lower Subalpine Cool Moist Coniferous subalpine fir-Engelmann spruce/Rocky Mountain maple-thinleaf huckleberry/thimbleberry |
F043AX955MT |
Subalpine Coniferous Cool Moist subalpine fir (Abies lasiocarpa)-Engelmann spruce (Picea engelmannii) |
R043AX962MT |
Alpine Unstable Talus rocky ledge penstemon (Penstemon ellipticus) |
R043AX971MT |
Alpine Solifluction Terrace Dryas octopetala (Arctostaphylos uva-ursi/Salix arctica) |
Similar sites
F043AX956MT |
Subalpine Coniferous Cool Moderately Dry subalpine fir (Abies lasiocarpa) / Engelmann spruce (Picea engelmannii) |
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Table 1. Dominant plant species
Tree |
(1) Abies lasiocarpa |
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Shrub |
(1) Vaccinium membranaceum |
Herbaceous |
(1) Luzula glabrata var. hitchcockii |
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