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This ecoregion lies almost wholly within Alberta but hugs the Alberta-British Columbia border from Banff northward to Jasper and Kakwa. Mean annual temperature in the Eastern Continental Ranges is 2.5°C, mean summer temperature is 12°C and mean winter temperature is -7.5°C. Precipitation increases from east to west with elevation, from 600-800mm per year. Valley regions are marked by warm, dry summers and mild, snowy winters, and subalpine areas have cool, showery summers and cold, snowy winters (ESWG 1995). This region covers the Rocky Mountains of Alberta, incorporating the eastern flanks of the Continental Ranges. The major peaks cluster around the Columbia Icefield, the largest ice field in the Rocky Mountains. The ranges themselves are linear with great cliffs and precipitous faces of thick sections of gray carbonate strata, and peaked by rock outcrops (ESWG 1995).
Vegetation in this ecoregion is composed of alpine and subalpine ecosystems characterized by mixed forests of lodgepole pine (Pinus contorta), Engelmann spruce (Picea engelmannii), and alpine fir (Abies lasiocarpa). Alpine fir is found at higher elevations. Alpine vegetation is also characterized by heather (Ericaceae) with sedges (Carex spp.) and mountain avens (Dryas hookeriana) on warmer sites (ESWG 1995). Wildlife of this region includes bighorn sheep (Ovis canadensis), elk (Cervus elaphus), black-tailed deer (Odocoileus hemionus), wolf (Canis lupus), grizzly and black bear (Ursus arctos and U. americanus), caribou (Rangifer tarandus), and mountain goat (Oreamnos americanus). The ecoregion exhibits a high diversity of large mammals (ESWG 1995). Habitat Loss Approximately 80 percent of this region was considered to remain as intact habitat. Major road corridors in valley lands with major outdoor recreation facilities and town sites are primarily responsible for loss of habitat. Remaining Blocks of Intact Habitat
Degree of Fragmentation Road and travel corridors in the major valleys impedes large carnivore and other wildlife movement. Degree of Protection
Types and Severity of Threats Expansion of road systems and recreational activities pose a major threat. A recent review (1996) of Banff National Park has recommended major changes to recreational and town site development in the park which would re-dress some of the habitat loss in this ecoregion over the long term. These recommendations have generally been accepted by the federal government. Attempts are also underway to begin adding structural elements to the trans-Canada highway, which passes through Banff National Park, to lower wildlife-auto collisions, although the highway is also under going a major expansion. New coal mining adjacent to Jasper National Park is a threat to the integrity of this protected area.
This ecoregion covers the Rocky Mountains of Alberta, incorporating the eastern portion of the continental Ranges (TEC 207) (ESWG 1995). The forests of this region cover the Subalpine East Slope Rockies (1), Montane Douglas-fir and Lodgepole Pine (5) and Tundra (Rowe 1972). Prepared by: D. Demarchi, R. Usher, K. Kavanagh, M. Sims, G. Mann. This text was originally published in the book Terrestrial ecoregions of North America: a conservation assessment from Island Press. This assessment offers an in-depth analysis of the biodiversity and conservation status of North America's ecoregions. All text by World Wildlife Fund © 2001 For more general information on this ecoregion, go to the WildWorld version of this description.
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