Kaparoqtalik Glacier
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Kaparoqtalik Glacier
Kaparoqtalik Glacier is a glacier located in the southern coast of the Byam Martin Mountains on Bylot Island, Nunavut, Canada. It lies in Sirmilik National Park. See also *List of glaciers in Canada References

Glaciers of Qikiqtaaluk Region Arctic Cordillera {{canada-glacier-stub ...
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Bylot Island 8 1997-08-05
Bylot may refer to: Places * Bylot Island, Nunavut, Canada, named after explorer Robert Bylot * Bylot, Manitoba ** Bylot railway station Bylot may refer to: Places * Bylot Island Bylot Island lies off the northern end of Baffin Island in Nunavut Territory, Canada. Eclipse Sound to the southeast and Navy Board Inlet to the southwest separate it from Baffin Island. Parry Channel ... * Bylot Sound, also called North Star Bay, in Wolstenholme Fjord, Greenland People * Robert Bylot, 17th-century explorer in the Canadian Arctic region {{disambiguation, geo ...
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Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ...
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Byam Martin Mountains
The Byam Martin Mountains are a rugged mountain range extending the length of Bylot Island, Nunavut, Canada. It is one of the most northern ranges in the world and is an extension of the Baffin Mountains which in turn form part of the Arctic Cordillera mountain system. The highest mountain in the range is Angilaaq Mountain, , located near the island's center. Sharp peaks and ridges, divided by deep glacier-filled valleys are typical features in the range Retrieved 2007-11-16 and has been extensively modified by glacial erosion. The Byam Martin Mountains have not been conducive to habitation. While there are no permanent settlements in the Byam Martin Mountains, Inuit from Pond Inlet and elsewhere regularly travel to the range. The Byam Martin Mountains are made up of Archean-Aphebian igneous crystalline rock and Proterozoic metasedimentary and metamorphic rock, such as gneiss. History The first known expedition to the Byam Martin Mountains was by Pat Baird in 1939. He traversed ...
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Bylot Island
Bylot Island lies off the northern end of Baffin Island in Nunavut Territory, Canada. Eclipse Sound to the southeast and Navy Board Inlet to the southwest separate it from Baffin Island. Parry Channel lies to its northwest. At it is ranked 71st largest island in the world and Canada's 17th largest island. The island measures east to west and north to south and is one of the largest uninhabited islands in the world. While there are no permanent settlements on this Canadian Arctic island, Inuit from Pond Inlet and elsewhere regularly travel to Bylot Island. An Inuit seasonal hunting camp is located southwest of Cape Graham Moore. The island's mountains are part of the Byam Martin Mountains, which is part of the Baffin Mountains of the Arctic Cordillera. In addition to Angilaaq Mountain, Malik Mountain, Mount St. Hans, and Mount Thule are notable. Tay Bay is on the west coast. Vertical cliffs along the coastline are made up of Precambrian dolomite. There are numerous glaciers ...
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Nunavut
Nunavut ( , ; iu, ᓄᓇᕗᑦ , ; ) is the largest and northernmost Provinces and territories of Canada#Territories, territory of Canada. It was separated officially from the Northwest Territories on April 1, 1999, via the ''Nunavut Act'' and the ''Nunavut Land Claims Agreement, Nunavut Land Claims Agreement Act'', which provided this territory to the Inuit for independent government. The boundaries had been drawn in 1993. The creation of Nunavut resulted in the territorial evolution of Canada, first major change to Canada's political map in half a century since the province of Newfoundland and Labrador, Newfoundland was admitted in 1949. Nunavut comprises a major portion of Northern Canada and most of the Arctic Archipelago. Its vast territory makes it the list of the largest country subdivisions by area, fifth-largest country subdivision in the world, as well as North America's second-largest (after Greenland). The capital Iqaluit (formerly Frobisher Bay), on Baffin Islan ...
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Sirmilik National Park
Sirmilik National Park (; Inuktitut: "the place of glaciers") is a national park located in Qikiqtaaluk, Nunavut, Canada, established in 1999. Situated within the Arctic Cordillera, the park is composed of three areas: most of Bylot Island with the exception for a few areas that are Inuit-owned lands, Oliver Sound, and Baffin Island's Borden Peninsula. Much of the park is bordered by water. Geographically, it is representative of the Northern Eastern Arctic Lowlands Natural Region as well as parts of the Lancaster Sound Marine Region. Etymology In the Inuktitut (or Inuit language, traditionally spoken across the North American Arctic) ''Sirmilik'' means "place of glaciers," as it represents Bylot Island's plethora of glaciers and ice caps. As Canadian Arctic Inuktitut-speakers referred to northern Baffin Island as ''Sirmilik'', the name of the geographic region became the name of the national park. History Extensive archaeological exploration of the park area has indicated ...
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List Of Glaciers In Canada
This is a list of glaciers in Canada. List of glaciers Saint Elias Mountains * Donjek Glacier *Hubbard Glacier * Logan Glacier Coast Mountains Boundary Ranges *Juneau Icefield **Llewellyn Glacier * Hang Ten Icefield *Stikine Icecap **Great Glacier *Andrei Icefield ** Andrei Glacier ** Choquette Glacier **Hoodoo Glacier **Johnson Glacier ** Porcupine Glacier **Twin Glacier *Salmon Glacier *Cambria Icefield Pacific Ranges *Monarch Icefield *Ha-Iltzuk Icefield **Klinaklini Glacier **Silverthrone Glacier * Waddington Massif-Pantheon Range-Whitemantle Range **Waddington Glacier **Tiedemann Glacier **Scimitar Glacier ** Parallel Glacier ** Franklin Glacier ** Bell Glacier (Canada) ** Cannonade Glacier ** Remote Glacier ** Shadow Glacier **Fan Glacier ** Geddes Glacier ** Chaos Glacier ** Radiant Glacier ** Cataract Glacier ** Isolation Glacier ** Shiverick Glacier ** Malemute Glacier ** Sunrise Glacier ** Tellot Glacier ** Smoking Cannon Glacier ** Jambeau Glacier ** Chanterelle G ...
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Glaciers Of Qikiqtaaluk Region
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only in ...
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