The Canadian Rockies are a segment of the North American Rocky Mountains found in the Canadian provinces of Alberta and British Columbia.
The Canadian Rockies are a segment of the North American Rocky Mountains found in the Canadian provinces of Alberta and British Columbia.
There is no universally accepted hierarchical division of the Canadian Rockies into subranges. [1] [2] For ease of navigation only, this article follows [1] and divides the Canadian Rockies into Far Northern Rockies, Northern Continental Ranges, Central Main Ranges, Central Front Ranges and Southern Continental Ranges, each of these subdivided in distinct areas and ranges.
From north to south and west to east, these mountain ranges are:
The Far Northern Rockies lie in British Columbia, and run from Prince George almost to the Yukon border. [3]
The Northern Continental Ranges run along the British Columbia-Alberta border north from Jasper to Mount Sir Alexander. [4]
The Central Main (or Park) Ranges lie northeast of the Rocky Mountain Trench, from Golden to Valemount. [5]
The Central Front Ranges lie northeast of the Rocky Mountain Trench, from Banff to Jasper. [6]
The Southern Continental Ranges run along the British Columbia-Alberta border from Banff down to Fernie [7]
Yoho National Park is a national park of Canada. It is located within the Rocky Mountains along the western slope of the Continental Divide of the Americas in southeastern British Columbia, bordered by Kootenay National Park to the south and Banff National Park to the east in Alberta. The word Yoho is a Cree expression of amazement or awe, and it is an apt description for the park's spectacular landscape of massive ice fields and mountain peaks, which rank among the highest in the Canadian Rockies.
Banff National Park is Canada's oldest national park, established in 1885 as Rocky Mountains Park. Located in Alberta's Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with many glaciers and ice fields, dense coniferous forest, and alpine landscapes. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, in the Bow River valley.
The Canadian Rocky Mountain Parks World Heritage Site consists of seven contiguous parks including four national parks and three British Columbia provincial parks.
The Canadian Rockies or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico.
Crowsnest Pass is a low mountain pass across the Continental Divide of the Canadian Rockies on the Alberta–British Columbia border.
Kootenay National Park is a national park of Canada in southeastern British Columbia. The park consists of 1,406 km2 (543 sq mi) of the Canadian Rockies, including parts of the Kootenay and Park mountain ranges, the Kootenay River and the entirety of the Vermilion River. While the Vermilion River is completely contained within the park, the Kootenay River has its headwaters just outside the park boundary, flowing through the park into the Rocky Mountain Trench and eventually joining the Columbia River. The park ranges in elevation from 918 m (3,012 ft) at the southwestern park entrance to 3,424 m (11,234 ft) at Deltaform Mountain.
Height of the Rockies Provincial Park is a provincial park in the Canadian Rockies of south eastern British Columbia, Canada. It is located west of the Continental Divide, adjacent to Elk Lakes Provincial Park.
The Continental Ranges is a major grouping of mountain ranges in the Rocky Mountains located in eastern British Columbia and western Alberta. It is a physiographic designation for use by geologists and is not used by the general public; it is not recognized in Alberta, and does not appear on topographic maps, although the names of its subranges are in common use. It is the largest and best-known of the three main such subdivisions of the Canadian Rockies, the others being the Hart Ranges and the Muskwa Ranges.
The Elk Valley is a valley in the southeastern Kootenay region of British Columbia, Canada. Located in the heart of the Canadian Rockies, the Elk Valley is approximately 60 kilometres from the Alberta and Montana borders.
The Great Divide Trail (GDT) is a wilderness hiking trail in the Canadian Rockies. The trail closely follows the Great Divide between Alberta and British Columbia, crossing the divide more than 30 times. Its southern terminus is in Waterton Lakes National Park at the Canada–US border and its northern terminus is at Kakwa Lake in Kakwa Provincial Park, north of Jasper National Park. The trail is 1,130 km (700 mi) long and ranges in elevation from 1,055 m (3,461 ft) at Old Fort Point trailhead near Jasper to 2,590 m (8,500 ft) at an unnamed pass above Michele Lakes just south of the White Goat Wilderness Area.
Storm Mountain is a mountain in Alberta's Rockies, Canada.
Alberta's Rockies comprise the Canadian Rocky Mountains in Alberta, Canada. On the southwestern part of the province along the British Columbia border, the region covers all but the south of Census Division 15.
The Nikanassin Formation is a stratigraphic unit of Late Jurassic (Portlandian) to Early Cretaceous (Barremian) age. It is present along the western edge of the Western Canada Sedimentary Basin in western Alberta and northeastern British Columbia. Its name was first proposed by D.B. Dowling in 1909 (Coal Fields South of Grand Trunk Pacific Railway, in the foothills of the Rocky Mountain, Alberta Page 140 paragraph 4 " to this it is proposed to give the name Nikanassin, from the Cree word meaning outer range" Also it is noted on the map by D.B. Dowling.(Geological Survey of Canada. Incorrect info follows: It was named by B.R. MacKay in 1929 for the Nikanassin Range of the front-central ranges of the Canadian Rockies. Mackay did not designate a type locality for the formation, although he described outcrops near the hamlet of Brûlé, north of the Yellowhead Highway outside of Jasper National Park.
Neptuak Mountain was named by Samuel E.S. Allen in 1894. "Neptuak" is the Stoney Indian word for "nine" as Neptuak Mountain is peak #9 in the Valley of the Ten Peaks. It is located on the Continental Divide, which is also the British Columbia-Alberta border in this region, and is in the Bow Range of the Park Ranges of the Canadian Rockies. The summit is a tripoint for Banff National Park, Kootenay National Park, and Yoho National Park, where the three parks share a common border.
The Park Ranges, also known as the Main Ranges, are a group of mountain ranges in the Canadian Rockies of southeastern British Columbia and southwestern Alberta, Canada. It is one of the three main subranges and the most central of the Continental Ranges, extending from southeast of Mount McGregor to the Fernie Basin.
The Lizard Range is a mountain range southwest of Fernie, British Columbia in the Canadian Rockies. The range is home to the Fernie Alpine Resort and parts of the Mount Fernie Provincial Park.
The Alberta Mountain forests are a temperate coniferous forests ecoregion of Western Canada, as defined by the World Wildlife Fund (WWF) categorization system.
The Kootenay Group, originally called the Kootenay Formation, is a geologic unit of latest Jurassic to earliest Cretaceous age in the Western Canada Sedimentary Basin that is present in the southern and central Canadian Rockies and foothills. It includes economically important deposits of high-rank bituminous and semi-anthracite coal, as well as plant fossils and dinosaur trackways.
The geology of Alberta encompasses parts of the Canadian Rockies and thick sedimentary sequences, bearing coal, oil and natural gas, atop complex Precambrian crystalline basement rock.
