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.

Classification relationships

ASSOCIATED HABITAT TYPES:
Major association with:
Douglas-fir/bluebunch wheatgrass
Douglas-fir/pinegrass-kinnikinnick phase

Minor association with:
Douglas-fir/ninebark-ninebark phase
Douglas-fir/pinegrass-ponderosa pine phase
Douglas-fir/rough fescue

Ecological site concept

• Site does not receive any additional water
This is a site with shallower soils than the closely related Upland Cool Woodland and therefore has less productivity, and resistance and resilience to disturbance.
• Dominant Cover: Coniferous Forest
The reference vegetation community is a forest dominated by Douglas fir with a grassy understory, either pinegrass with the low shrub kinnikinnick or a bunchgrass dominated understory with bluebunch wheatgrass. Understory species species from most common to least include: common snowberry (Symphoricarpos albus), pinegrass (Calamagrostis rubescens), Geyer's sedge (Carex geyeri), arrowleaf balsamroot (Balsamorhiza sagittata), creeping barberry (Mahonia repens), bluebunch wheatgrass (Pseudoroegneria spicata) and ninebark (Physocarpus malvaceus). Understory production ranges from 200 to 300 and averages 274 dry pounds per acre.
• Soils are
o Generally not limy (limited extent)
o Shallow (less than 50cm deep to bedrock, lithic, or paralithic root restrictive layer)
o Not ashy or medial textural family
o Typically less than 5% stone and boulder surface cover (<15% max)
• Soil surface texture very gravelly ashy silt loam or gravelly loam in surface mineral 4”
• Parent material is colluvium over residuum, loamy till
• Drainage class is well drained; no flooding frequency
• Site Landform: south aspect mountain slopes, glacially scoured ridges, south aspect ridges
• Moisture Regime: ustic/udic
• Temperature Regime: frigid
• Elevation Range: 3100-5300 ft
• Slope: 15-50%

Associated sites

Similar sites

Table 1. Dominant plant species