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Greely Fiord
Greely Fiord is a natural inlet in the west of Ellesmere Island, Qikiqtaaluk Region, Nunavut in the Arctic Archipelago. To the south lies the Cañon Fiord Cañon Fiord is a natural inlet in the west of Ellesmere Island, Nunavut in the Arctic Archipelago. To the north, it opens into Greely Fiord and to the east lies the Agassiz Ice Cap. References Ellesmere Island Fjords of Qikiqtaaluk R ... and the Agassiz Ice Cap. To the northwest is Borup Fiord and Tanquary Fiord is northeast. References External links Geologic map of Greely Fjord West (80 - 88°W 80 - 81°N) Ellesmere Island Fjords of Qikiqtaaluk Region {{QikiqtaalukNU-geo-stub ...
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Ellesmere Island
Ellesmere Island ( iu, script=Latn, Umingmak Nuna, lit=land of muskoxen; french: île d'Ellesmere) is Canada's northernmost and List of Canadian islands by area, third largest island, and the List of islands by area, tenth largest in the world. It comprises an area of , slightly smaller than Great Britain, and the total length of the island is . Lying within the Arctic Archipelago, Ellesmere Island is considered part of the Queen Elizabeth Islands. Cape Columbia at 83°06′ is the northernmost point of land in Canada and one of the northernmost points of land on the planet (the northernmost point of land on Earth is the nearby Kaffeklubben Island of Greenland). The Arctic Cordillera mountain system covers much of Ellesmere Island, making it the most mountainous in the Arctic Archipelago. More than one-fifth of the island is protected as Quttinirpaaq National Park. In 2021, the population of Ellesmere Island was recorded at 144. There are three settlements: Alert, Nunavut, Aler ...
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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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Nansen Sound
Nansen Sound is an uninhabited strait in Qikiqtaaluk, Nunavut, Canada. It lies between western Grant Land on Ellesmere Island and Axel Heiberg Island.''Merriam-Webster's Geographical Dictionary, Third Edition'', p. 789. Tanquary Fiord or Greely Fiord enters the sound from the east. Notes References *''Merriam-Webster's Geographical Dictionary, Third Edition''. Springfield, Massachusetts: Merriam-Webster, Incorporated, 1997. . Sound In physics, sound is a vibration that propagates as an acoustic wave, through a transmission medium such as a gas, liquid or solid. In human physiology and psychology, sound is the ''reception'' of such waves and their ''perception'' b ... Sounds of Qikiqtaaluk Region {{QikiqtaalukNU-geo-stub ...
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Qikiqtaaluk Region
The Qikiqtaaluk Region, Qikiqtani Region (Inuktitut syllabics: ᕿᑭᖅᑖᓗᒃ ) or Baffin Region is the easternmost, northernmost, and southernmost administrative region of Nunavut, Canada. Qikiqtaaluk is the traditional Inuktitut name for Baffin Island. Although the Qikiqtaaluk Region is the most commonly used name in official contexts, several notable public organizations, including Statistics Canada prefer the older term Baffin Region. With a population of 18,988 and an area of , it is the largest and most populated of the three regions. The region consists of Baffin Island, the Belcher Islands, Akimiski Island, Mansel Island, Prince Charles Island, Bylot Island, Devon Island, Baillie-Hamilton Island, Cornwallis Island, Bathurst Island, Amund Ringnes Island, Ellef Ringnes Island, Axel Heiberg Island, Ellesmere Island, the Melville Peninsula, the eastern part of Melville Island, and the northern parts of both Prince of Wales Island and Somerset Island, plus s ...
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Arctic Archipelago
The Arctic Archipelago, also known as the Canadian Arctic Archipelago, is an archipelago lying to the north of the Canadian continental mainland, excluding Greenland (an autonomous territory of Denmark). Situated in the northern extremity of North America and covering about , this group of 36,563 islands, surrounded by the Arctic Ocean, comprises much of Northern Canada, predominately Nunavut and the Northwest Territories. The archipelago is showing some effects of climate change, with some computer estimates determining that melting there will contribute to the rise in sea levels by 2100. History Around 2500 BCE, the first humans, the Paleo-Eskimos, arrived in the archipelago from the Canadian mainland. Between 1000–1500 CE, they were replaced by the Thule people, who are the ancestors of today's Inuit. British claims on the islands, the British Arctic Territories, were based on the explorations in the 1570s by Martin Frobisher. Canadian sovereignty was originally (187 ...
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Cañon Fiord
Cañon Fiord is a natural inlet in the west of Ellesmere Island, Nunavut in the Arctic Archipelago. To the north, it opens into Greely Fiord and to the east lies the Agassiz Ice Cap The Agassiz Ice Cap formerly Agassiz Glacier is an ice cap on the central eastern side of Ellesmere Island, Nunavut, Canada. The Agassiz ice cap is about in area. It is located between the North Ellesmere ice field to the north and the Prince .... References Ellesmere Island Fjords of Qikiqtaaluk Region {{canada-fjord-stub ...
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Agassiz Ice Cap
The Agassiz Ice Cap formerly Agassiz Glacier is an ice cap on the central eastern side of Ellesmere Island, Nunavut, Canada. The Agassiz ice cap is about in area. It is located between the North Ellesmere ice field to the north and the Prince of Wales Icefield to the south. Environmental studies Several studies have been conducted which involve the analysis of ice cores extracted from the Agassiz Ice cap. Many of these studies are focused around climate change In common usage, climate change describes global warming—the ongoing increase in global average temperature—and its effects on Earth's climate system. Climate change in a broader sense also includes previous long-term changes to .... References Bodies of ice of Qikiqtaaluk Region Ellesmere Island Arctic Cordillera Ice caps of Canada {{canada-glacier-stub ...
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Borup Fiord
Borup Fiord is located on Ellesmere Island, Qikiqtaaluk Region, Nunavut Canada. The mouth of the fiord opens into Greely Fiord. To the west is Oobloyah Bay and to the north is the Neil Peninsula and the Neil Icecap. The eastern arm, known as Esayoo Bay leads to Borup Fiord Pass. Detailed studies of the Borup Fiord area between Oobloyah Bay and Esayoo Bay have been done in summer 1988 by geographers from Heidelberg University. See also *List of fjords in Canada Fjords in Canada are long, narrow inlets characterized by steep sides, created in a valley carved by glacial activity. A fjord can have two or more basins separated by sills. The bowls can have a depth of and the dividing sills can raise up to ... References Ellesmere Island Fjords of Qikiqtaaluk Region {{canada-fjord-stub ...
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Tanquary Fiord
Tanquary Fiord is a fjord on the north coast of the Arctic Archipelago's Ellesmere Island, Nunavut, Canada. It is located in the Quttinirpaaq National Park and extends in a north-westerly direction from Greely Fiord. History Radiocarbon dating methods suggest that between 10,000 and 4,100 BP, deglaciation occurred, followed by a period of glacial readvance and the formation of ice shelves until 2,400 BP. Until 1,400 BP, a period of glacial retreat occurred, and since then glacial readvance and nearby ice rises have marked the area. Radiocarbon analysis of charcoal undertaken by the Geological Survey of Canada has shown that Inuit were present at Tanquary Fiord around 1070 BP at the latest. Geography The head of the Tanquary Fiord is the convergence point of four river valleys, three of which end in a floodplain and one in a river delta. Carbon dating findings show that the fjord was free of glacial ice approximately 6,500 years ago. In the past 40 years, the terminal ...
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