List Of Glaciers In Canada
A comprehensive list of glaciers in Canada began with glacial surveys by the Water Survey of Canada (WSC) from 1945 to 1980, including an inventory begun for the International Geophysical Year (1957–58) and contributions to the World Glacier Inventory (WGI, now part of the World Glacier Monitoring Service) for the International Hydrological Decade (1965–1974). In mainland Canada, glaciers are grouped by the WSC basin system. In the Arctic Archipelago, where the majority of glaciers are unnamed, glaciers are grouped by island with the WSC basin identifier augmented by Scott Polar Research Institute catalogue numbers. Published in the ''Glacier Atlas of Canada'', the inventory identified glaciers on Bylot Island and on Axel Heiberg Island. The following is a list of notable glaciers in Canada. List of glaciers Saint Elias Mountains *Donjek Glacier *Hubbard Glacier *Logan Glacier (Alaska), Logan Glacier Coast Mountains Boundary Ranges *Juneau Icefield **Llewellyn Glacier ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Athabasca Glacier On The Columbia Icefield
Athabasca (also Athabaska) is an anglicized version of the Cree language, Cree name for Lake Athabasca in Canada, āthap-āsk-ā-w (pronounced ), meaning "grass or reeds here and there". Most places named Athabasca are found in Alberta, Canada. Athabasca may also refer to: Geographical features *Mount Athabasca (), a mountain in Jasper National Park, Canada **Athabasca Glacier, a glacier in Jasper National Park, Canada *Athabasca River, river in Alberta, Canada **Athabasca Falls, waterfalls on the Athabasca River **Peace-Athabasca Delta – of the Peace River, Athabasca River, near Lake Athabasca *Athabasca Oil Sands – oil-producing region in Alberta, Canada *Lake Athabasca, large lake in Alberta and Saskatchewan, Canada *Athabasca Pass, a mountain pass in Jasper National Park *Athabasca Valles, a feature on the surface of the planet Mars *Athabasca Sand Dunes Provincial Park, a unique geophysical land feature in the boreal shield ecosystem Saskatchewan, Canada *Athabasca Basi ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Great Glacier
Great Glacier Provincial Park is a provincial park in the Stikine Country region of British Columbia, Canada. It was established on January 25, 2001 to protect Great Glacier and the surrounding mountainous terrain. The park lies in the traditional territory of the Tahltan First Nation about south of the Tahltan community of Telegraph Creek. History According to the legends of the Tahltan and Tlingit First Nations, Great Glacier once spanned the entire width of the Stikine River to meet the toe of Choquette Glacier on the eastern side of the valley. The glacier was also the site of the last major battle between the Tahltan and Tlingit First Nations many generations ago. Geography Great Glacier Park is located in the Boundary Ranges of British Columbia between the lower Stikine River and the Canada–United States border with Alaska. Immediately across the river from Great Glacier Park is Choquette Hot Springs Provincial Park, which protects a collection of hot springs and as ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Klinaklini Glacier
The Klinaklini Glacier is a glacier west of the Klinaklini River and head of Knight Inlet the Coast Land District of British Columbia, Canada Canada is a country in North America. Its Provinces and territories of Canada, ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, making it the world's List of coun ... (51° 28′ 0″ N, 125° 47′ 0″ W). It flows generally southward from Mt. Silverthrone. The glacier is one of the largest glaciers in western North America. The Hakai Institute has installed a weather station and camera above Klinaklini Glacier that will provide data in near real time to scientists and operational users. References Glaciers of the Pacific Ranges Central Coast of British Columbia {{BritishColumbiaCentralCoast-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ha-Iltzuk Icefield
The Ha-Iltzuk Icefield is an icefield in the central Pacific Ranges of the Coast Mountains in British Columbia, Canada. It is the largest icefield in the Coast Mountains south of the Alaska Panhandle, with an area of . It is located on the west side of the Klinaklini River and the Waddington Range. The highest summit in the icefield is Mount Silverthrone, which is a mountain on the northeast edge of a circular, wide, deeply dissected caldera complex called the Silverthrone Caldera. The southern half of the icefield is named the Silverthrone Glacier and flows west, joining the Klinaklini Glacier just above that glacier's terminus, where its outflow is short but very large, and joins the Klinaklini River within a few kilometres. The Klinaklini Glacier constitutes the northern half of the icefield, and off its northwest edge a glacial tongue produces the head of the Machmell River. The name Ha-Iltzuk Icefield does not appear in government gazettes. The term is almost cer ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Monarch Icefield
The Monarch Icefield is the northernmost of a series of large continental icecaps studding the heights of the Pacific Ranges of the Coast Mountains in southern British Columbia, Canada. Located southeast of the town of Bella Coola and west of the headwaters of the Atnarko River, a tributary of the Bella Coola River, it lies to the north of the Ha-Iltzuk Icefield The Ha-Iltzuk Icefield is an icefield in the central Pacific Ranges of the Coast Mountains in British Columbia, Canada. It is the largest icefield in the Coast Mountains south of the Alaska Panhandle, with an area of . It is located on the west ..., which is the largest icefield of the group and home to the Silverthrone volcano. The Monarch Icefield is very remote and is rarely visited by mountaineering parties. References BCGNIS listing "Monarch Icefield" Central Coast of British Columbia Glaciers of the Pacific Ranges Ice fields of British Columbia {{BritishColumbiaCentralCoast-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pacific Ranges
The Pacific Ranges are the southernmost subdivision of the Coast Mountains portion of the Pacific Cordillera. Located entirely within British Columbia, British Columbia, Canada, they run northwest from the lower stretches of the Fraser River to Bella Coola, British Columbia, Bella Coola and Burke Channel, north of which are the Kitimat Ranges. The Coast Mountains lie between the Interior Plateau and the British Columbia Coast, Coast of British Columbia. The Pacific Ranges include four of the five major coastal icecaps in the southern Coast Mountains. These are the largest temperate-latitude icecaps in the world and fuel a number of very major rivers (by volume, not length). One of these contains Mount Waddington, the highest summit entirely within British Columbia. Also within this region is Hunlen Falls, among the highest in Canada, located in Tweedsmuir South Provincial Park. Other than logging and various hydroelectric developments, and a large ski resort at Whistler, Briti ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cambria Icefield
The Cambria Icefield is an icefield in the Boundary Ranges of the Coast Mountains in northwestern British Columbia, Canada, located southeast of Stewart. Climate Based on the Köppen climate classification, the Cambria Icefield is located in a subarctic climate zone of western North America. Most weather fronts originate in the Pacific Ocean The Pacific Ocean is the largest and deepest of Earth's five Borders of the oceans, oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean, or, depending on the definition, to Antarctica in the south, and is ..., and travel east toward the Coast Mountains where they are forced upward by the range ( Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the icefield experiences high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Gallery Fi ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Salmon Glacier
The Salmon Glacier is a glacier located ~ north of Stewart, British Columbia, and Hyder, Alaska, just on the Canadian side of the border. The glacier, one of hundreds in the Boundary Ranges, is notable for its major potential as a natural hazard. Summit Lake is located at the northern end of the glacier and every year around mid-July the lake breaks an ice-dam and then flows under the Salmon Glacier into the Salmon River. This causes the river to rise approximately for several days. The glacier can be accessed by road from Hyder, Alaska, from early July to late September. The glacier's name was officially adopted January 20, 1955, by the Geographical Names Board of Canada. Climate Based on the Köppen climate classification, Salmon Glacier is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range ( Orographic lift), ca ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Twin Glacier
Twin Glacier is a glacier in northwestern British Columbia, Canada, located on the northern and eastern flanks of Hoodoo Mountain. It lies at the headwaters of the Twin River. The glacier originates from the Andrei Icefield. See also *List of glaciers in Canada A comprehensive list of glaciers in Canada began with glacial surveys by the Water Survey of Canada (WSC) from 1945 to 1980, including an inventory begun for the International Geophysical Year (1957–58) and contributions to the World Glacier I ... * Hoodoo Glacier References External links * Glaciers of British Columbia Boundary Ranges Cassiar Land District {{canada-glacier-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Porcupine Glacier
Porcupines are large rodents with coats of sharp spines, or quills, that protect them against predation. The term covers two families of animals: the Old World porcupines of the family Hystricidae, and the New World porcupines of the family Erethizontidae. Both families belong to the infraorder Hystricognathi within the profoundly diverse order Rodentia and display superficially similar coats of rigid or semi-rigid quills, which are modified hairs composed of keratin. Despite this, the two groups are distinct from one another and are not closely related to each other within the Hystricognathi. The largest species of porcupine is the third-largest living rodent in the world, after the capybara and beaver. The Old World porcupines (Hystricidae) live in Italy, Asia (western and southern), and most of Africa. They are large, terrestrial, and strictly nocturnal. The New World porcupines (Erethizontidae) are indigenous to North America and northern South America. They live in wood ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Johnson Glacier (British Columbia)
The Getz Ice Shelf () is an ice shelf over long and from wide, bordering the Hobbs Coast and Bakutis Coast of Marie Byrd Land, Antarctica, between the McDonald Heights and Martin Peninsula. Several large islands are partially or wholly embedded in the ice shelf. Location File:C74126s1 Ant.Dean Island Getz Ice Shelf.jpg, Western ice shelf Shepard to Carney islands File:C74112s5 Ant.Map Martin Peninsula context.jpg, Eastern ice shelf Carney Island to Martin Peninsula The Getz Ice Shelf extends along the north shore of Marie Byrd Land, from Hanessian Foreland and McDonald Heights in the west to Cape Herlacher on the Martin Peninsula to the east. The western section lies along the Hobbs Coast, while the section east of Dean Island lies along the full length of the Bakutis Coast. In the west the ice sheet is fed by glaciers that include, from west to east, Johnson Glacier, Venzke Glacier, Berry Glacier and DeVicq Glacier. Discovery and name The ice shelf westward of Siple ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Hoodoo Glacier
Hoodoo Glacier is a glacier in northwestern British Columbia, Canada, located on the western flank of Hoodoo Mountain. It lies at the headwaters of the Hoodoo River. The glacier originates from the Andrei Icefield. See also *List of glaciers in Canada *Twin Glacier Twin Glacier is a glacier in northwestern British Columbia, Canada, located on the northern and eastern flanks of Hoodoo Mountain. It lies at the headwaters of the Twin River. The glacier originates from the Andrei Icefield. See also *List of ... References External links * Glaciers of British Columbia Cassiar Land District Boundary Ranges {{canada-glacier-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |