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Kangerluarsunnguaq Bay
Kangerluarsunnguaq Bay ( aŋeʁluɑʁsuŋːuɑq̚ da, Ulkebugten) is a bay of the Davis Strait in the Qeqqata municipality on the western coast of Greenland. It is located directly to the north of Sisimiut. Geography The bay branches off Davis Strait to the east, just north of Sisimiut. It is navigable in its entirety, protected from the open sea by a series of skerries and channels in the west. In the past, at the time of the Saqqaq culture settlements in the area, the bay extended further inland, the shoreline was up to several dozen meters above the present line, covering portions of the Sisimiut valley, and gradually decreasing in time due to post-glacial rebound. To the north the bay is bounded by the Palasip Qaqqaa range. Sisimiut Airport is located at the far western end on the northern side, behind the several skerries and small islands of Qeqertarmiut and the Annertusoq skerry group protecting it from the storm waves of the open sea, and separating it from the mouth o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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'', ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arctic
The Arctic ( or ) is a polar regions of Earth, polar region located at the northernmost part of Earth. The Arctic consists of the Arctic Ocean, adjacent seas, and parts of Canada (Yukon, Northwest Territories, Nunavut), Danish Realm (Greenland), Finland, Iceland, Norway, Russia (Murmansk Oblast, Murmansk, Siberia, Nenets Autonomous Okrug, Nenets Okrug, Novaya Zemlya), Sweden and the United States (Alaska). Land within the Arctic region has seasonally varying snow and sea ice, ice cover, with predominantly treeless permafrost (permanently frozen underground ice) containing tundra. Arctic seas contain seasonal sea ice in many places. The Arctic region is a unique area among Earth's ecosystems. The cultures in the region and the Arctic indigenous peoples have adapted to its cold and extreme conditions. Life in the Arctic includes zooplankton and phytoplankton, fish and marine mammals, birds, land animals, plants and human societies. Arctic land is bordered by the subarctic. De ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sisimiut
Sisimiut (), formerly known as Holsteinsborg, is the capital and largest city of the Qeqqata municipality, the second-largest city in Greenland, and the largest Arctic city in North America.The term 'city' is loosely used to describe any populated area in Greenland, given that the most populated place is Nuuk, the capital, with 16,454 inhabitants. The term 'Arctic' is interpreted as strictly the area within the Arctic Circle. It is located in central-western Greenland, on the coast of Davis Strait, approximately north of Nuuk. ''Sisimiut'' literally means "the residents at the foxholes" ( da, Beboerne ved rævehulerne). The site has been inhabited for the last 4,500 years, first by peoples of the Saqqaq culture, then Dorset culture, and then the Thule people, whose Inuit descendants form the majority of the current population. Artifacts from the early settlement era can be found throughout the region, favored in the past for its plentiful fauna, particularly the marine mammals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ''.'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saqqaq Culture
The Saqqaq culture (named after the Saqqaq settlement, the site of many archaeological finds) was a Paleo-Eskimo culture in southern Greenland. Up to this day, no other people seem to have lived in Greenland continually for as long as the Saqqaq. Timeframe The earliest known archaeological culture in southern Greenland, the Saqqaq existed from around 2500 BCE until about 800 BCE.Saqqaq culture profile — from the Greenland Research Centre at the . This culture coexisted with the |
Post-glacial Rebound
Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound and isostatic depression are phases of glacial isostasy (glacial isostatic adjustment, glacioisostasy), the deformation of the Earth's crust in response to changes in ice mass distribution. The direct raising effects of post-glacial rebound are readily apparent in parts of Northern Eurasia, Northern America, Patagonia, and Antarctica. However, through the processes of ''ocean siphoning'' and ''continental levering'', the effects of post-glacial rebound on sea level are felt globally far from the locations of current and former ice sheets.Milne, G.A., and J.X. Mitrovica (2008) ''Searching for eustasy in deglacial sea-level histories.'' Quaternary Science Reviews. 27:2292–2302. Overview During the last glacial period, much of northern Eu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sisimiut Airport
Sisimiut Airport ( kl, Mittarfik Sisimiut) is an airport located northwest of Sisimiut, a town in the Qeqqata municipality in central-western Greenland. The airport has a single runway designated 13/31 which measures , built on the northern shore of Kangerluarsunnguaq Bay. For scheduled flights, the airport is served exclusively by Air Greenland, serving as a fly-through destination with no aircraft stationed onsite. Operated by Mittarfeqarfiit, it is also used for general aviation purposes. Airlines and destinations Roads in Sisimiut, including the road to the airport, are surfaced, but there is no road linking Sisimiut to any other settlement. With 5,460 inhabitants in 2010, Sisimiut is the second-largest town in Greenland, one of the few towns in the country exhibiting growth patterns, with corresponding increasing passenger traffic at Sisimiut Airport. Air Greenland pledges to maintain a relatively high number of flights at the airport even should the construction of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amerloq Fjord
Amerloq Fjord is a long fjord in the Qeqqata municipality in western Greenland. The fjord empties into the Davis Strait just south of Sisimiut, whose former Inuit name was also "Amerloq". History The Amerloq Fjord then known as Rammel's Fjord was the scene of the Inuit murder of the Dano-English navigator James Hall on 12 or 22 July, 1612. The Inuit were still incensed at the Danish abduction of several people during one of Christian IV's expeditions in 1605, during which Hall served as pilot for John Cunningham. Geography The fjord mouth is located at approximately south of the town of Sisimiut. To the north, the fjord is bounded by the Nasaasaaq ridge, whose 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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