Kangaamiut Kangerluarsuat Fjord
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Kangaamiut Kangerluarsuat Fjord
Kangaamiut Kangerluarsuat Fjord (old spelling: ''Kangâmiut Kangerdluarssuat'') is a fjord in the Qeqqata municipality in western Greenland. The fjord is located halfway between the lower runs of the long Kangerlussuaq Fjord in the north, and Kangerlussuatsiaq Fjord in the south, emptying into Davis Strait.''Maniitsoq'', Saga Map, Tage Schjøtt, 1992 Geography The head of the fjord at is formed by the short ''Illorlersuaq'' icefjord flowing from the tidewater Sermitsiaq Glacier draining the Maniitsoq ice cap, now separated from the Greenland ice sheet ( kl, Sermersuaq). The fjord flows southwestward, opening into Davis Strait, with its mouth dotted with several skerries. Settlement Kangaamiut is the only settlement in the vicinity, located on a small island to the south of the fjord mouth. See also *List of fjords of Greenland This is a list of the most important fjords of Greenland:In Northern Greenland, a large area made up entirely of fjords; therefore Peary La ...
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Greenland
Greenland ( kl, Kalaallit Nunaat, ; da, Grønland, ) is an island country in North America that is part of the Kingdom of Denmark. It is located between the Arctic and Atlantic oceans, east of the Canadian Arctic Archipelago. Greenland is the world's largest island. It is one of three constituent countries that form the Kingdom of Denmark, along with Denmark and the Faroe Islands; the citizens of these countries are all citizens of Denmark and the European Union. Greenland's capital is Nuuk. Though a part of the continent of North America, Greenland has been politically and culturally associated with Europe (specifically Norway and Denmark, the colonial powers) for more than a millennium, beginning in 986.The Fate of Greenland's Vikings
, by Dale Mackenzie Brown, ''Archaeological Institute of America'', ...
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Fjord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords wh ...
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Qeqqata
Qeqqata (, da, Centrum, lit=Centre) is a municipality in western Greenland, operational from 1 January 2009. The municipality was named after its location in the central-western part of the country. Its population is 9,378 as of January 2020. The administrative center of the municipality is in Sisimiut (formerly called Holsteinsborg). Creation It consists of the previously unincorporated area of Kangerlussuaq, as well as two former municipalities of western Greenland, Maniitsoq and Sisimiut. Geography In the south and east, the municipality is flanked by the Sermersooq municipality, although settlements and associated trade is concentrated mainly alongside the coast. In the north, it is bordered by the Qeqertalik municipality. The waters of the western coast are that of the Davis Strait, separating Greenland from Baffin Island. With an area of it is the second-smallest municipality of Greenland after Kujalleq. Politics Qeqqata's municipal council consists of 15 members, ele ...
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Kangerlussuaq Fjord
Kangerlussuaq Fjord (old spelling: ''Kangerdlugssuaq'', da, Søndre Strømfjord) is a long fjord in the Qeqqata municipality in central-western Greenland. The fjord is long and between and wide, flowing from the estuary of Qinnguata Kuussua river to the southwest, and emptying into the Davis Strait. It is the longest fjord of western Greenland. Geography The head of the fjord is located at , at the estuary of the Qinnguata Kuussua river flowing from the Russell Glacier of the Greenland ice sheet ( kl, Sermersuaq). The fjord mouth is located at , south of the Simiutaq Island. Another, smaller waterway connects to the sea to the north of the island.Maniitsoq, Saga Map, Tage Schjøtt, 1992 Kangerlussuaq Fjord does not have any tributary fjords, with a fairly uniform coastline. Small hills of the Kangaamiut dike swarm, such as the highlands of Tarajornitsut, dominate the coast of the inner parts of the fjord, transforming into steep mountain ranges towards the mouth. In that ...
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Kangerlussuatsiaq Fjord
Kangerlussuatsiaq Fjord (old spelling: ''Kangerdlugssuatsiaq'', da, Evighedsfjorden) is a fjord in the Qeqqata municipality in western Greenland. Taking its source in the tidewater glaciers draining the Maniitsoq ice cap, the fjord flows in a deep canyon through a mountainous, uninhabited region, emptying into Davis Strait near the settlement of Kangaamiut. Geography Kangerlussuatsiaq Fjord is long and deep. The head of the fjord is formed by two tributaries. ''Qingua Kujalleq'', the southern arm, is a short icefjord flowing northwestward, with its head at .''Maniitsoq'', Saga Map, Tage Schjøtt, 1992 ''Qingua Avannarleq'', the northern arm, flowing southwestward from the Kangerlussuatsiaup Qingua valley, blocked at the end by glacier outflow from the Maniitsoq ice cap, now separated from the Greenland ice sheet ( kl, Sermersuaq), at . After the confluence the fjord heads to the southwest, bounded from both sides by mountain cliffs exceeding . The mountains near the m ...
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Davis Strait
Davis Strait is a northern arm of the Atlantic Ocean that lies north of the Labrador Sea. It lies between mid-western Greenland and Baffin Island in Nunavut, Canada. To the north is Baffin Bay. The strait was named for the English explorer John Davis (1550–1605), who explored the area while seeking a Northwest Passage. By the 1650s it was used for whale hunting. Extent The International Hydrographic Organization defines the limits of the Davis Strait as follows: ''On the North.'' The Southern limit of Baffin Bay 70° North between Greenland and Baffin Island">Baffin Land]. ''On the East.'' The Southwest coast of Greenland. ''On the South.'' The parallel of 60th parallel north, 60° North between Greenland and Labrador. ''On the West.'' The Eastern limit of the Northwestern Passages South of 70° North he East coast of Baffin Island to East Bluff, its Southeastern extremityand of Hudson Strait line from East Bluff, the Southeast extreme of Baffin Island (), to Point ...
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Sermitsiaq Glacier
Sermitsiaq Glacier is a tidewater glacier in the Qeqqata municipality in western Greenland. It drains Maniitsoq ice cap into two fjords flowing towards Davis Strait: Kangaamiut Kangerluarsuat Fjord in the north, and the longer Kangerlussuatsiaq Fjord in the south.''Maniitsoq'', Saga Map, Tage Schjøtt, 1992 See also *List of glaciers in Greenland This is a list of glaciers in Greenland. Details on the size and flow of some of the major Greenlandic glaciers are listed by Eric Rignot and Pannir Kanagaratnam (2006) Ice sheets and caps *Greenland Ice Sheet * Christian Erichsen Ice Cap *Flad ... References External links * Glaciers of Greenland {{Greenland-glacier-stub ...
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Maniitsoq Ice Cap
Maniitsoq Ice Cap (old spelling: ''Manîtsoq'', da, Sukkertoppen iskappe or ''Sukkertoppen isflade'') is a ice cap in the Qeqqata municipality in western Greenland. Geography There are no settlements in the vicinity of the ice cap. In the southeast, Maniitsoq ice cap is separated from the westward tongue of the Greenland ice sheet by the narrow Kangerlussuatsiaup Qingua valley. The summit of the ice cap reaches between and . Google Earth The maximum height is marked as a high summit in the Defense Mapping Agency Greenland Navigation charts, although it does not rise above . In the south, several mountain glaciers drain it towards the upper reaches of the Kangerlussuatsiaq Fjord. To the west, the ice cap is drained by the long Sermitsiaq Glacier. To the northwest, numerous mountain glaciers drain it towards Kangerlussuaq Fjord.''Maniitsoq'', Saga Map, Tage Schjøtt, 1992 To the northeast of the ice sheet lies the wide highland of Angujaartorfiup Nunaa, home to herds of m ...
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Greenland Ice Sheet
The Greenland ice sheet ( da, Grønlands indlandsis, kl, Sermersuaq) is a vast body of ice covering , roughly near 80% of the surface of Greenland. It is sometimes referred to as an ice cap, or under the term ''inland ice'', or its Danish equivalent, ''indlandsis''. An acronym, GIS, is frequently used in the scientific literature. It is the second largest ice body in the world, after the Antarctic ice sheet. The ice sheet is almost long in a north–south direction, and its greatest width is at a latitude of 77°N, near its northern margin. The average thickness is about and over at its thickest point. In addition to the large ice sheet, smaller ice caps (such as Maniitsoq and Flade Isblink) as well as glaciers, cover between around the periphery. The Greenland ice sheet is adversely affected by climate change. It is more vulnerable to climate change than the Antarctic ice sheet because of its position in the Arctic, where it is subject to the regional amplification o ...
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Skerry
A skerry is a small rocky island, or islet, usually too small for human habitation. It may simply be a rocky reef. A skerry can also be called a low sea stack. A skerry may have vegetative life such as moss and small, hardy grasses. They are often used as resting places by animals such as seals and birds. Etymology The term ''skerry'' is derived from the Old Norse ', which means a rock in the sea (which in turn derives from the Proto-Indo-European root *''sker''-, "cut", in the sense of a rock cut off from the land). The Old Norse term ' was brought into the English language via the Scots language word spelled or . It is a cognate of the Scandinavian languages' words for ''skerry'' – Icelandic, fo, sker, da, skær, sv, skär, no, skjær / skjer, found also in german: Schäre, fi, kari, et, skäär, lv, šēra, lt, Šcheras and russian: шхеры (). In Scottish Gaelic, it appears as ', e.g. Sula Sgeir, in Irish as '','' in Welsh as '','' and in Manx as ''.'' ...
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Kangaamiut
Kangaamiut,"Maniitsoq", Saga Map, Tage Schjøtt, 1992. formerly known as Gammel Sukkertoppen, is a settlement with a population of 293 (2020) in the Qeqqata municipality in central-western Greenland. Geography Kangaamiut is located on an island off the coast of Davis Strait between mouths of two long fjords. To the south is the long and twisted Kangerlussuatsiaq Fjord and to the north is the Kangaamiut Kangerluarsuat Fjord. The mouth of the long Kangerlussuaq Fjord is located approximately north of the island. History The Dano-Norwegian settlement Sukkertoppen was originally located at the site of present-day Kangaamiut, when it was founded in 1755. It was moved to its present location at Maniitsoq in 1782. Transport Kangaamiut serves as a port of call for the Arctic Umiaq Line Arctic Umiaq Line A/S (AUL) or Arctic Umiaq is a passenger and freight shipping line in Greenland. Its name derives from the Kalaallisut word for the traditional Inuit passenger boat, the umiak, ...
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