Kangerluarsuk Tulleq
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Kangerluarsuk Tulleq
Kangerluarsuk Tulleq (old spelling: ''Kangerdluarssuk Tugdleq'') is a long fjord in the Qeqqata municipality in western Greenland. The fjord is of roughly east–west orientation, emptying into Davis Strait in the west. Geography The fjord mouth is located at approximately , to the northwest of the town of Sisimiut. In the northeast, the fjord is bounded by the partially glaciated Aqqutikitsoq massif, culminating in . To the northwest, undulating terrain under Akornata Qaqqaa mountain () constitutes the terminal point of a long mountain range extending from the Pingu mountain group halfway between Davis Strait and the Greenland ice sheet ( kl, Sermersuaq). The range flattens considerably towards the east in the area of Kangaamiut dike swarm north of Kangerlussuaq, due to pressure exerted by the icesheet for long periods in the past. The head of the fjord is located at approximately . To the south, the fjord is bounded by the long Majoriaq range, culminating in the west in ...
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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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Kangaamiut Dike Swarm
The Kangaamiut dike swarm (old spelling: ''Kangâmiut'') is a 2.04 billion year old dike swarm located in the Qeqqata region of western Greenland. The dikes cut Archean orthogneisses and are exposed along approximately of the coast and a similar distance up to the inland ice to the east, covering an area of about . To the north it is bounded by the paleoproterozoic Ikertooq shear zone (old spelling: ''Ikertôq'') while to the south the boundary is gradational with a gradual reduction in the density of dikes. The dike swarm was intruded during a phase of extensional tectonics. They were later deformed during the Nagssugtoqidian orogeny The Nagssugtoqidian orogeny was a late Paleoproterozoic mountain-building event that affected Greenland during the period 1.91 to 1.77 Ga. The orogenic belt formed during this event marks the northern boundary of the mainly Archaean North Atlan ..., with the amount of strain increasing towards the Iqertooq shear zone. References {{coord m ...
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Palasip Qaqqaa
Palasip Qaqqaa ( da, Præstefjeldet) is a mountain in the Qeqqata municipality in western Greenland. It is located on the mainland of Greenland on the coast of Davis Strait, immediately to the north of Sisimiut Airport. The mountain massif is spread out over in the west–east direction, constituting the terminal point of a long mountain range extending from the Pingu mountain group halfway between Davis Strait and the Greenland ice sheet ( kl, Sermersuaq). The range flattens considerably towards the east in the area of Kangaamiut dike swarm north of Kangerlussuaq Kangerlussuaq (; ; da, Søndre Strømfjord), is a settlement in western Greenland in the Qeqqata municipality located at the head of the fjord of the same name. It is Greenland's main air transport hub and the site of Greenland's largest commer ..., due to pressure exerted by the icesheet for long periods in the past. Topography Palasip Qaqqaa has two distinct summits: the western () and the main, eastern sum ...
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Kangerlussuaq
Kangerlussuaq (; ; da, Søndre Strømfjord), is a settlement in western Greenland in the Qeqqata municipality located at the head of the fjord of the same name. It is Greenland's main air transport hub and the site of Greenland's largest commercial airport. The airport dates from American settlement during and after World War II, when the site was known as Bluie West-8 and then Sondrestrom Air Base. The Kangerlussuaq area is also home to Greenland's most diverse terrestrial fauna, including muskoxen, caribou, and gyrfalcons. The settlement's economy and population of 508 is almost entirely reliant on the airport and tourist industry. Geography Kangerlussuaq occupies an alluvial flatland on the far end of the 190 km long Kangerlussuaq Fjord, straddling both sides of the Qinnguata Kuussua river estuary. East of Kangerlussuaq there is a confluence of the two major regional rivers, the Qinnguata Kuussua and Akuliarusiarsuup Kuua. The valley of the latter forms large quicksa ...
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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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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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Pingu (Greenland)
''Pingu'' is a stop-motion children's television series co-created by Otmar Gutmann and Erika Brueggemann. It was originally produced from 1990 to 2000 by Swiss company The Pygos Group (originally called Trickfilmstudio) for SF DRS in Switzerland. It was later revived from 2003 to 2006 for CBeebies by British companies HIT Entertainment and Hot Animation. The series focuses on a family of anthropomorphic emperor penguins who live in the South Pole; the main character is the family's son and title character, Pingu. The series originally ran for four series from 7 March 1990 to 9 April 2000 on SF DRS. It was then renewed for two more series from 1 August 2003 to 3 March 2006 on CBeebies. ''Pingu'' was also nominated for a BAFTA award in 2005. The pilot episode was made on 28 May 1986. Pingu became popular outside of Switzerland, in part due to its lack of a real spoken language: nearly all dialogue is in an invented grammelot "penguin language" referred to as 'Penguinese', co ...
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