Chaba Peak
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Chaba Peak
Chaba Peak is located in the Chaba Icefield south of Fortress Lake in Hamber Provincial Park on the Continental Divide marking the Alberta-British Columbia border. It was named in 1920 after the Chaba River by the Interprovincial Boundary Survey. Chaba is the Stoney Indian word for beaver Beavers are large, semiaquatic rodents in the genus ''Castor'' native to the temperate Northern Hemisphere. There are two extant species: the North American beaver (''Castor canadensis'') and the Eurasian beaver (''C. fiber''). Beavers ar .... See also * List of peaks on the Alberta–British Columbia border * List of mountains in the Canadian Rockies References {{BritishColumbiaInterior-geo-stub Three-thousanders of Alberta Three-thousanders of British Columbia Canadian Rockies Kootenay Land District Alberta's Rockies ...
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Continental Divide Of The Americas
The Continental Divide of the Americas (also known as the Great Divide, the Western Divide or simply the Continental Divide; ) is the principal, and largely mountainous, hydrological divide of the Americas. The Continental Divide extends from the Bering Strait to the Strait of Magellan, and separates the watersheds that drain into the Pacific Ocean from those river systems that drain into the Atlantic and (in northern North America) Arctic oceans (including those that drain into the Gulf of Mexico, the Caribbean Sea and Hudson Bay). Although there are many other hydrological divides in the Americas, the Continental Divide is by far the most prominent of these because it tends to follow a line of high peaks along the main ranges of the Rocky Mountains and Andes, at a generally much higher elevation than the other hydrological divisions. Geography Beginning at the westernmost point of the Americas’ mainland (Cape Prince of Wales, just south of the Arctic Circle), the Conti ...
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Three-thousanders Of British Columbia
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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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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List Of Mountains In The Canadian Rockies
A list of highest peaks in the Canadian Rockies is shown below: References ;Notes {{reflist, group=notes *• 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 ... Mountains, Rockies Mountains, Rockies ...
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List Of Peaks On The Alberta–British Columbia Border
This is a list of peaks on the Alberta–British Columbia border, being the spine of the Continental Divide from the Canada–United States border to the 120th meridian, which is where the boundary departs the Continental Divide and goes due north to the 60th parallel. Peaks are listed from north to south and include the four peaks not on the Continental Divide but which are on the 120th Meridian, stretching approximately due north from Intersection Mountain, which as its name implies is located at the intersection of the Divide and the Meridian. See also *List of Boundary Peaks of the Alaska-British Columbia/Yukon border *Extreme points of British Columbia References {{DEFAULTSORT:List Of Peaks On The British Columbia-Alberta Border * * Peaks Peaks Peak or The Peak may refer to: Basic meanings Geology * Mountain peak ** Pyramidal peak, a mountaintop that has been sculpted by erosion to form a point Mathematics * Peak hour or rush hour, in traffic conges ...
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Beaver
Beavers are large, semiaquatic rodents in the genus ''Castor'' native to the temperate Northern Hemisphere. There are two extant species: the North American beaver (''Castor canadensis'') and the Eurasian beaver (''C. fiber''). Beavers are the second-largest living rodents after the capybaras. They have stout bodies with large heads, long chisel-like incisors, brown or gray fur, hand-like front feet, webbed back feet and flat, scaly tails. The two species differ in the shape of the skull and tail and fur color. Beavers can be found in a number of freshwater habitats, such as rivers, streams, lakes and ponds. They are herbivorous, consuming tree bark, aquatic plants, grasses and sedges. Beavers build dams and lodges using tree branches, vegetation, rocks and mud; they chew down trees for building material. Dams impound water and lodges serve as shelters. Their infrastructure creates wetlands used by many other species, and because of their effect on other organisms in the ...
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Stoney Indian
The Nakoda (also known as Stoney or ) are an Indigenous people in Western Canada and, originally, the United States. They used to inhabit large parts of what is now Alberta, Saskatchewan and Montana, but their reserves are now located in Alberta and in Saskatchewan, where they are scarcely differentiated from the Assiniboine. Through their language they are related to the Dakota and Lakota nations of the Great Plains and the Rocky Mountains, part of the large Sioux Nation. They refer to themselves in their own language as " Nakoda", meaning ''friend'', ''ally''. The name "Stoney" was given them by white explorers, because of their technique of using fire-heated rocks to boil broth in rawhide bowls. They are very closely related to the Assiniboine, who are also known as ''Stone Sioux'' (from the Ojibwe ). Alberta's Nakoda First Nation comprises three bands: Bearspaw, Chiniki and Wesley. The Stoney were "excluded" from Banff National Park between 1890 and 1920. In 2010 ...
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Chaba River (Canada)
The Chaba River is a short river in western Alberta, Canada. It flows from the Canadian Rockies, and joins the Athabasca River. The Chaba River is a major tributary of the Athabasca River, Athabasca. The Chaba is fed by the glacial melt originating in the Chaba Icefield, comprising Chaba Peak, as well as Listening and Sundial Peaks. A small glacier on Mount Quincy also contributes to the Chaba. The river was given its name by A. P. Coleman, a geologist born in Eastern Canada in 1852. He stated there "were endless beaver dams and trees" along the river, and named it after the Stoney Indian word for beavers."Karamitsanis, Aphrodite (1991). ''Place Names of Alberta, Volume 1''. Calgary: University of Calgary Press, pg. 45 See also *List of Alberta rivers References

Rivers of Alberta {{Alberta-river-stub ...
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Hamber Provincial Park
Hamber Provincial Park is a provincial park in British Columbia, Canada, located 130 kilometres (80.7 mi) north of Golden. Straddling the Great Divide on the provincial boundary with Alberta, the park is surrounded on three sides by Jasper National Park and protects the headwaters of the Wood River at Fortress Lake. When the park was created in 1941, it constituted one of the largest protected wilderness areas in Canada. In the early 1960s, the provincial government reduced its size by 98% due to pressure exerted by the forestry industry, planned hydroelectric developments along the upper Columbia River and the re-routing of the Trans-Canada Highway away from the park. History Established on 16 September 1941 by an Order in Council issued by British Columbia premier Thomas Dufferin Pattullo, the park was named in honour of Eric W. Hamber, Lieutenant-Governor of British Columbia from 1936 to 1941. Covering approximately 1,009,112 hectares at the time of its establishmen ...
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Park Ranges
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. Subranges * Blackwater Range *Blue Range * Bow Range * Chaba Icefield * Clemenceau-Chaba * Columbia Icefield * Drummond Group * Freshfields * Harrison Group * Hooker Icefield *Kitchen Range * Le Grand Brazeau * McKale-Chalco Divide *Mitchell Range * Morkill Ranges *Ottertail Range * Rainbow Range * Royal Group * Selwyn Range *Spray Mountains The Spray Mountains is a mountain range of the Canadian Rockies located in southwestern 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. A ... * Sundance Range * The Ramparts * Trident Range * Van Horne Range * Vermilion ...
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