Cornice Peak (Canadian Rockies)
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Cornice Peak (Canadian Rockies)
Cornice Peak, 3188 m (10459 feet), is a mountain in the Continental Ranges of the Canadian Rockies in Alberta, Canada. See also *Cornice Peak (other) Cornice Peak may refer to any of three mountain peaks in British Columbia and Alberta: * Cornice Peak (Canadian Rockies), in the Continental Ranges of the Rocky Mountains in Alberta * Cornice Peak (Selkirk Mountains), in the Sir Sandford Range of t ... References Three-thousanders of Alberta Alberta's Rockies {{AlbertaRockies-geo-stub ...
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Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Continental Ranges
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 (the Kootenay, Park or Main Ranges, and Front Ranges) 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.Landforms of British Columbia'', S Holland, Govt of BC Bulletin No. 58, 1976 Sub-ranges There are three main subdivisions of the Continental Ranges: the Front Ranges, the Park Ranges, and the Kootenay Ranges. Each of those three subdivisions is further divided into individual ranges as follows: *Front Ranges ** Bare Range ** Bighorn Range ** Bosche Range ** De Smet Range ** Elk Range ** Fairholme Range ** First Range ...
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Canadian Rockies
The Canadian Rockies (french: Rocheuses canadiennes) 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. Canada officially defines the Rocky Mountains system as the mountain chains east of the Rocky Mountain Trench extending from the Liard River valley in northern British Columbia to the Albuquerque Basin in New Mexico, not including the Mackenzie, Richardson and British Mountains/Brooks Range in Yukon and Alaska (which are all included as the "Arctic Rockies" in the United States' definition of the Rocky Mountains system). The Canadian Rockies, bein ...
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Alberta
Alberta ( ) is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Territories (NWT) to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada (Saskatchewan being the other). The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds. Alberta is the fourth largest province by area at , and the fourth most populous, being home to 4,262,635 people. Alberta's capital is Edmonton, while Calgary is its largest city. The two are Alberta's largest census metropolitan areas. More tha ...
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Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ...
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Cornice Peak (other)
Cornice Peak may refer to any of three mountain peaks in British Columbia and Alberta: * Cornice Peak (Canadian Rockies), in the Continental Ranges of the Rocky Mountains in Alberta * Cornice Peak (Selkirk Mountains), in the Sir Sandford Range of the Selkirk Mountains in British Columbia *Cornice Peak (Kitimat Ranges), in the Kitimat Ranges of the Coast Mountains in British Columbia See also * Cornice Mountain (Stikine Icecap) * Cornice Mountain (Cambria Icefield) * Cornice Ridge *Cornice In architecture, a cornice (from the Italian ''cornice'' meaning "ledge") is generally any horizontal decorative moulding that crowns a building or furniture element—for example, the cornice over a door or window, around the top edge of a ...
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Three-thousanders Of Alberta
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ...
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