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Danmark Island
Danmark Island ( kl, Ujuaakajiip Nunaa; da, Danmark Ø) is an island in Scoresby Sund. Administratively it lies in the area of Sermersooq municipality. History The island was named in 1891 by Carl Ryder during his 1891–92 East Greenland Expedition. It was chosen as a wintering harbor in 1891/2 during the exploration of the Scoresby Sund fjord system. Numerous remains of Inuit habitations were found on the island by the East Greenland Expedition, indicating that the Scoresby Sound area had been inhabited in relatively recent times.Spencer Apollonio: ''Lands that Hold One Spellbound.'' University of Calgary Press, 2008, , p. 78 The Greenlandic name ''Ujuaakajiip Nunaa'' was registered in 1955 by the Danish Geodætisk Institut. It means "Little Johan’s Land" after Johan Petersen, Scoresbysund colony manager, who was known to the locals as "Ujuât". Geography Danmark Island lies at the eastern end of Fon Fjord by its mouth. Ten kilometers before the mouth, the fjord has a bra ...
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Scoresby Sound
Scoresby Sound (Danish: ''Scoresby Sund'', Greenlandic: ''Kangertittivaq'') is a large fjord system of the Greenland Sea on the eastern coast of Greenland. It has a tree-like structure, with a main body approximately Scoresby Sund
Encyclopædia Britannica on-line
long that branches into a system of s covering an area of about . The longest of the fjords extends 340–350 km (210-216 mi) inland from the coastline. The depth is 400–600 m (1,310-1,970 ft) in the main basin, but depths increase to up to in some fjords. It is one of the largest and longest fjord systems in the world.Archaeology, p. 7 On the northern side of the mouth of the Scoresb ...
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Geodætisk Institut
Geodætisk Institut (1928–1987) was a Danish state-run cartographic institute. It was created by law number 82, of 31 March 1928, combining Generalstabens Topografiske Afdeling and Den danske Gradmaaling, two institutions that did somewhat overlapping cartographic and topographic mapping of Denmark. It was initially part of Ministry of War (Krigsministeret), later Ministry of Defence (Forsvarsministeret). In the years 1940–1953 ''Geodætisk Institut'' made the second nationwide precision landscape levelling of Denmark. The first was done 1885–1905 by ''Den danske Gradmaaling''. The height fix point remains Århus Domkirke ( Dansk Normal Nul (DNN)), as established in 1905. A third levelling was done 1982–1994. This formed the basic for the new height system DVR90, replacing DNN. The height fix point remains Aarhus Domkirke, however its kote was changed from 5.6150m to 5.570m in DVR90. ''Geodætisk Institut'' made the third topographic mapping of Denmark in the years ...
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Operational Navigation Chart C-1, 1st Edition
An operational definition specifies concrete, replicable procedures designed to represent a construct. In the words of American psychologist S.S. Stevens (1935), "An operation is the performance which we execute in order to make known a concept." For example, an operational definition of "fear" (the construct) often includes measurable physiologic responses that occur in response to a perceived threat. Thus, "fear" might be operationally defined as specified changes in heart rate, galvanic skin response, pupil dilation, and blood pressure. Overview An operational definition is designed to model or represent a concept or theoretical definition, also known as a construct. Scientists should describe the operations (procedures, actions, or processes) that define the concept with enough specificity such that other investigators can replicate their research. Operational definitions are also used to define system states in terms of a specific, publicly accessible process of preparation ...
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Scoresby
Scoresby may refer to: People * William Scoresby (1789–1857), British Arctic explorer, scientist and clergyman * William F. Scoresby (1840–1884), New York politician * William Scoresby Routledge (1859–1939), British ethnographer, anthropologist and adventurer Places * Scoresby (crater), Lunar crater * Scoresby Bay, Nunavut, Canada * Scoresby Hills, Nunavut, Canada * Scoresby Point, South Georgia * Scoresby Sound, a fjord in the Eastern coast of Greenland * Scoresby, Victoria, Australia ** former Electoral district of Scoresby * William Scoresby Archipelago, Antarctica * William Scoresby Bay, Antarctica Ships * RRS ''William Scoresby'', early 20th century British research vessel * SS ''Scoresby'' (1923–1940), British steam merchant ship In fiction * Lee Scoresby This is a list of characters from the two Philip Pullman trilogies, ''His Dark Materials'' and ''The Book of Dust''. Introduced in ''Northern Lights'' Lyra Belacqua Lyra Belacqua, later known as Lyra Silve ...
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Hekla (barque)
''Scotia'' was a barque that was built in 1872 as the Norwegian whaler ''Hekla''. She was purchased in 1902 by William Speirs Bruce and refitted as a research vessel for use by the Scottish National Antarctic Expedition. After the expedition, she served as a sealer, patrol vessel and collier. She was destroyed by fire in January 1916. Description The ship was , with a beam of . She had a draught of . The ship was assessed at . History ''Hekla'' was built as a barque in 1872 by Jørgensen & Knudsen, Drammen for S. S. Svendsen of Sandefjord. She was used as a sealer, making voyages to the east coast of Greenland from 1872 to 1882 and to Scoresby Sound in 1892. In 1896, she was sold to N. Bugge, Tønsberg. She was sold in 1898 to A/S Sæl- og Hvalfangerskib Hekla, Christiania and was placed under the management of M. C. Tvethe. ''Hekla'' was sold in 1900 to A/S Hecla, Sandefjord, operated under the management of Anders Marcussen. In 1902, she was purchased by William Speirs Bru ...
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Hekla Havn
Hekla (), or Hecla, is a stratovolcano in the south of Iceland with a height of . Hekla is one of Iceland's most active volcanoes; over 20 eruptions have occurred in and around the volcano since 874. During the Middle Ages, the Icelandic Norse called the volcano the "Gateway to Hell". Hekla is part of a volcanic ridge, long. The most active part of this ridge, a fissure about long named , is considered to be within Hekla proper. Hekla looks rather like an overturned boat, with its keel being a series of craters, two of which are generally the most active. The volcano's frequent large eruptions have covered much of Iceland with tephra, and these layers can be used to date eruptions of Iceland's other volcanoes. Approximately 10% of the tephra created in Iceland in the last thousand years has come from Hekla, amounting to 5 km3. Cumulatively, the volcano has produced one of the largest volumes of lava of any in the world in the last millennium, around 8 km3. Etymolo ...
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Milne Land
Milne Land or Milneland is a large island in eastern Greenland. It is the third largest island of Greenland, after the main island of Greenland and Disko Island. It is named after British admiral David Milne. This island is popular among climbers. Geography The island is long from Moraene Point in the southwest to Bregne Point in the northeast, up to wide, and in area. It is part of an archipelago, which includes Storo and Sorte Island in the Northwest, Denmark Island in the south, and the Bjorne Islands in the northeast. Cape Leslie is Milneland's southeastern headland. Milne Land is separated from the Renland peninsula in the north by the 6 to wide Ofjord, from the Gaaseland peninsula in the south by the 4 to wide Fonfjord, and from the mainland coast in the west by the 4 to wide Rode Fjord. Jameson Land , the large peninsula in the east with the settlement of Ittoqqortoormiit on its southern coast, is located more than away across the Scoresby Sound. Image gallery ...
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Fon Fjord
Fonfjord ( kl, Ujuaakajiip Kangertiva; da, Fønfjord, meaning 'Foehn Fjord') is a fjord in King Christian X Land, eastern Greenland. This fjord is part of the Scoresby Sound system.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute'', p. 115 Administratively it lies in the area of Sermersooq municipality. History This long fjord was surveyed and named in 1891 by Carl Ryder during his 1891–92 East Greenland Expedition. It was named "Føhnfjord" owing to the powerful Foehn wind gusts blowing during the first exploration of the fjord in August 1891. Ryder wrote: Another name given by former surveyors was ''Blastfjord'', by Hans Christian Gulløv. Geography In the southern Scoresby Sound, between Cape Leslie in Milne Land to the north and Cape Stevenson to the south, there are the mouths of two fjords that go in a roughly southwestern direction. The northern branch is the Fonfjord and the southern is the much wider mouth of the Gaasefjord ''(Gåsefjord)''. Gaasel ...
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Greenlandic Language
Greenlandic ( kl, kalaallisut, link=no ; da, grønlandsk ) is an Eskimo–Aleut language with about 56,000 speakers, mostly Greenlandic Inuit in Greenland. It is closely related to the Inuit languages in Canada such as Inuktitut. It is the most widely spoken Eskimo–Aleut language. Greenlandic has been the sole official language of the Greenlandic autonomous territory since June 2009, which is a move by the Naalakkersuisut, the government of Greenland, to strengthen the language in its competition with the colonial language, Danish. The main variety is Kalaallisut, or West Greenlandic. The second variety is Tunumiit oraasiat, or East Greenlandic. The language of the Thule Inuit of Greenland, Inuktun or Polar Eskimo, is a recent arrival and a dialect of Inuktitut. Greenlandic is a polysynthetic language that allows the creation of long words by stringing together roots and suffixes. The language's morphosyntactic alignment is ergative, treating both the argument (subject) ...
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Greenland Sea
The Greenland Sea is a body of water that borders Greenland to the west, the Svalbard archipelago to the east, Fram Strait and the Arctic Ocean to the north, and the Norwegian Sea and Iceland to the south. The Greenland Sea is often defined as part of the Arctic Ocean, sometimes as part of the Atlantic Ocean. However, definitions of the Arctic Ocean and its seas tend to be imprecise or arbitrary. In general usage the term "Arctic Ocean" would exclude the Greenland Sea. In oceanographic studies the Greenland Sea is considered part of the Nordic Seas, along with the Norwegian Sea. The Nordic Seas are the main connection between the Arctic and Atlantic oceans and, as such, could be of great significance in a possible shutdown of thermohaline circulation. In oceanography the Arctic Ocean and Nordic Seas are often referred to collectively as the "Arctic Mediterranean Sea", a marginal sea of the Atlantic. The sea has Arctic climate with regular northern winds and temperatures rarely ...
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Inuit
Inuit (; iu, ᐃᓄᐃᑦ 'the people', singular: Inuk, , dual: Inuuk, ) are a group of culturally similar indigenous peoples inhabiting the Arctic and subarctic regions of Greenland, Labrador, Quebec, Nunavut, the Northwest Territories, and Alaska. Inuit languages are part of the Eskimo–Aleut languages, also known as Inuit-Yupik-Unangan, and also as Eskaleut. Inuit Sign Language is a critically endangered language isolate used in Nunavut. Inuit live throughout most of Northern Canada in the territory of Nunavut, Nunavik in the northern third of Quebec, Nunatsiavut and NunatuKavut in Labrador, and in various parts of the Northwest Territories, particularly around the Arctic Ocean, in the Inuvialuit Settlement Region. With the exception of NunatuKavut, these areas are known, primarily by Inuit Tapiriit Kanatami, as Inuit Nunangat. In Canada, sections 25 and 35 of the Constitution Act of 1982 classify Inuit as a distinctive group of Aboriginal Canadians wh ...
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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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