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Klapperhorn Mountain
Klapperhorn Mountain is a summit in British Columbia, Canada. Description Klapperhorn Mountain, elevation 2,301-meters (7,549-feet), is located in Mount Robson Provincial Park, just south and within view of the park's visitor centre. It is the northernmost peak of the Selwyn Range, which is a subrange of the Canadian Rockies. Precipitation runoff from the peak drains north into the Fraser River. Topographic relief is significant as the summit rises 1,400 meters (4,600 ft) above the Robson Valley in . The Yellowhead Highway (Highway 16) and Canadian National Railway traverse the northern base of the mountain. The nearest neighbor is line parent Overlander Mountain, to the southeast. Etymology The mountain was named by BC Parks on March 13, 1972, and the toponym was officially adopted December 19, 1978, by the Geographical Names Board of Canada. The mountain is a classic horn-shaped summit, which is notable for the frequency of its rockslides which are audible to cam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Selwyn Range (British Columbia)
The Selwyn Range is a mountain range in the Canadian Rockies in British Columbia. A subrange of the Park Ranges of the Continental Ranges, it is located west of Jasper National Park, east of Valemount and south of Mount Robson Provincial Park.BivuacSelwyn Range Retrieved August 7, 2007 It was named after Alfred Selwyn, the first director of the Geological Survey of Canada. The Fraser River originates in this mountain range, near Fraser Pass. See also *Overlander Mountain *Klapperhorn Mountain Klapperhorn Mountain is a summit in British Columbia, Canada. Description Klapperhorn Mountain, elevation 2,301-meters (7,549-feet), is located in Mount Robson Provincial Park, just south and within view of the park's visitor centre. It is th ... * Mount McKirdy References * Mountain ranges of British Columbia Ranges of the Canadian Rockies {{BritishColumbiaInterior-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia Highway 16
Highway 16 is a highway in British Columbia, Canada. It is an important section of the Yellowhead Highway, a part of the Trans-Canada Highway that runs across Western Canada. The highway closely follows the path of the northern B.C. alignment of the Canadian National Railway. The number "16" was first given to the highway in 1941, and originally, the route that the highway took was more to the north of today's highway, and it was not as long as it is now. Highway 16 originally ran from New Hazelton east to Aleza Lake. In 1947, Highway 16's western end was moved from New Hazelton to the coastal city of Prince Rupert, and in 1953, the highway was re-aligned to end at Prince George. In 1969, further alignment east into Yellowhead Pass was opened to traffic after being constructed up through 1968 and raised to all-weather standards in 1969. Highway 16's alignment on Haida Gwaii was commissioned in 1983 and is connected to the mainland segment via BC Ferries route #11. A series of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Terry Fox Provincial Park
Mount Terry Fox Provincial Park is a provincial park in British Columbia, Canada. It is located in the Rocky Mountains near Mount Robson and the city of Valemount, British Columbia. The park and Mount Terry Fox, which is within the park, are named in honor of amputee long-distance runner and cancer research activist Terry Fox, a native of Winnipeg, Manitoba Winnipeg () is the capital and largest city of the province of Manitoba in Canada. It is centred on the confluence of the Red and Assiniboine rivers, near the longitudinal centre of North America. , Winnipeg had a city population of 749,6 ... who grew up in British Columbia. External links *BC Parks entry Terry Fox Regional District of Fraser-Fort George Provincial parks of British Columbia Robson Valley 1982 establishments in British Columbia Protected areas established in 1982 {{BritishColumbia-park-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Robson
Mount Robson is the most prominent mountain in North America's Rocky Mountain range; it is also the highest point in the Canadian Rockies. The mountain is located entirely within Mount Robson Provincial Park of British Columbia, and is part of the Rainbow Range. Mount Robson is the second highest peak entirely in British Columbia, behind Mount Waddington in the Coast Range. The south face of Mount Robson is clearly visible from the Yellowhead Highway (Highway 16), and is commonly photographed along this route. Mount Robson was likely named after Colin Robertson, who worked for both the North West Company and the Hudson's Bay Company at various times in the early 19th century, though there was confusion over the name as many assumed it to have been named for John Robson, an early premier of British Columbia. The Texqakallt, a Secwepemc people and the earliest known inhabitants of the area, call it (striped rock), spelled in Dawson 1891 as , ''The Mountain of the Spiral ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cinnamon Peak
Cinnamon Peak is a mountain summit located in the northwestern part of Mount Robson Provincial Park, in the Canadian Rockies of British Columbia, Canada. It is situated immediately north of the confluence of the Robson River and the Fraser River, and is visible from the Yellowhead Highway near the park's visitor centre. The peak was labelled "Little Grizzly" on Arthur Oliver Wheeler's 1911 topographic map of Mount Robson. He thought it appeared similar to Mount Grizzly in the Selkirk Mountains, but the name was later changed to Cinnamon, which is the coloration of the peak and the Cinnamon bear, which can be easily mistaken for a grizzly bear. "Little Grizzly" is a colloquial term for the black bear, Ursus americanus. Eastern populations are typically black in color, however western populations can be cinnamon colored. The mountain's toponym was officially adopted in 1951 by the Geographical Names Board of Canada. The nearest higher peak is Whitehorn Mountain, to the north. __NO ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of British Columbia
British Columbia is the westernmost province of Canada, bordered by the Pacific Ocean. With an area of it is Canada's third-largest province. The province is almost four times the size of the United Kingdom and larger than every United States state except Alaska. It is bounded on the northwest by the U.S. state of Alaska, directly north by Yukon and the Northwest Territories, on the east by Alberta, and on the south by the U.S. states of Washington, Idaho, and Montana. Formerly part of the British Empire, the southern border of British Columbia was established by the 1846 Oregon Treaty. The province is dominated by mountain ranges, among them the Canadian Rockies but dominantly the Coast Mountains, Cassiar Mountains, and the Columbia Mountains. Most of the population is concentrated on the Pacific coast, notably in the area of Vancouver, located on the southwestern tip of the mainland, which is known as the Lower Mainland. It is the most mountainous province of Canada. Statist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should ave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyramidal Peak
A pyramidal peak, sometimes called a glacial horn in extreme cases, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point. Pyramidal peaks are often examples of nunataks. Formation Glaciers, typically forming in drainages on the sides of a mountain, develop bowl-shaped basins called cirques (sometimes called ‘corries’ - from Scottish Gaelic ʰəɾə(a bowl) - or s). Cirque glaciers have rotational sliding that abrades the floor of the basin more than walls and that causes the bowl shape to form. As cirques are formed by glaciation in an alpine environment, the headwall and ridges between parallel glaciers called arêtes become more steep and defined. This occurs due to freeze/thaw and mass wasting beneath the ice surface. It is widely held that a common cause for headwall steepening and extension headward is the crevasses known as bergschrund that occur between the moving ice and the he ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geographical Names Board Of Canada
The Geographical Names Board of Canada (GNBC) is a national committee with a secretariat in Natural Resources Canada, part of the Government of Canada, which authorizes the names used and name changes on official federal government maps of Canada created since 1897. The board consists of 27 members, one from each of the provinces and territories, and others from departments of the Government of Canada. The board also is involved with names of areas in the Antarctic through the Antarctic Treaty. Structure The secretariat is provided by Natural Resources Canada. In addition to the provincial and territorial members are members from the following federal government departments: Aboriginal Affairs and Northern Development Canada, Canada Post Corporation, Fisheries and Oceans Canada, Elections Canada, Library and Archives Canada, Department of National Defence, Natural Resources Canada (including Geological Survey of Canada and Canada Centre for Mapping and Earth Observation), Pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
BC Parks
BC Parks is an agency of the British Columbia Ministry of Environment and Climate Change Strategy that manages all of the, as of 2020, 1,035 provincial parks and other conservation and historical properties of various title designations within the province's Parks oversaw of the British Columbia Parks and Protected Areas System. The Lieutenant Governor-in-Council created the agency on March 1, 1911, through the Strathcona Park Act. The agency is charged with a dual role of preserving the ecological and historical integrity of the places entrusted to its management, while also making them available and accessible for public use and enjoyment. History In July 1910, a party of the British Columbia Provincial Government Expedition led by the Chief Commissioner of Lands Price Ellison explored the region surrounding Crown Mountain on Vancouver Island for the purposes of setting aside land to establish British Columbia's first provincial park. Ellison then reported his findings to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Line Parent
A peak's line parent is the closest higher peak on the highest ridge leading away from the peak's "key col". A col is the lowest point on the ridge between two summits and is roughly synonymous with pass, gap, saddle and notch. The highest col of a peak is its key col. If there is more than one ridge which can be followed to a higher peak then the line parent is the peak closest to the key col. Usually, a line parent must meet some prominence criteria, which might vary depending on the author and the location of the peak. There are at least two other kinds of peak parentage. Island parentage, which is also referred to as encirclement or topographic parentage; and source parentage. See also * Topographic prominence In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contou ... References ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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