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Barentsjøkulen
Barentsjøkulen is a glacier on Barentsøya, Svalbard. The glacier covers an area of about . It is named after the Barents Island, which again is named after Dutch explorer Willem Barentsz. Barents Island is on the Barents Sea. The glacier has the four offshoots Besselsbreen, Willybreen, Freemanbreen and Duckwitzbreen. See also *List of glaciers in Svalbard This is a list of glaciers in Svalbard. It includes glaciers and ice caps in Svalbard, Norway. List of glaciers and ice caps Ice caps *Austfonna *Biscayarfonna *Glitnefonna *Lomonosovfonna *Løvenskioldfonna *Valhallfonna *Vegafonna *Vestfonna ... References Glaciers of Svalbard Barentsøya {{svalbard-glacier-stub ...
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Barentsøya
Barentsøya, anglicized as Barents Island, is an Arctic island in the Svalbard archipelago of Norway, lying between Edgeøya and Spitsbergen. To the north, in the sound between Barentsøya and Spitsbergen, lies the island of Kükenthaløya. To the south, the sound (geography), sound separating Barents Island from Edgeøya is Freeman Strait, Freemansundet. Barentsøya has Uninhabited island, no permanent human inhabitants. It is part of the Søraust-Svalbard Nature Reserve and forms a habitat for several species, including polar bears and kittiwakes. History The island was named after Netherlands, Dutch explorer Willem Barents who, despite discovering Svalbard, never sighted Barentsøya itself. The name "Barents Land" was only given after an 1865 Swedish expedition. Previously, Dutch whaling captains had referred to it on maps as ''Zuyd Ooster Land'' ("Southeastern Land") as early as 1710. In 1936, Norway built four cabins on the island to formally establish control. Geography ...
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Besselsbreen
Besselsbreen is a glacier on Barentsøya, Svalbard Svalbard ( , ), previously known as Spitsbergen or Spitzbergen, is a Norway, Norwegian archipelago that lies at the convergence of the Arctic Ocean with the Atlantic Ocean. North of continental Europe, mainland Europe, it lies about midway be .... It is the largest offshoot of Barentsjøkulen, reaching down to the sea in the northeast direction, west of the point Kapp Bessels. The glacier is named after German Arctic explorer Emil Bessels. References Glaciers of Svalbard Barentsøya {{svalbard-glacier-stub ...
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Willybreen
Willybreen is a glacier on Barentsøya, Svalbard. It is an offshoot of Barentsjøkulen, reaching down to the sea in the eastern direction. The glacier is named after German zoologist Willy Kükenthal Wilhelm (Willy) Georg Kükenthal (4 August 1861, Weißenfels – 20 August 1922, Berlin) was a German zoologist. He was the older brother of botanist and theologian Georg Kükenthal (1864–1955). Kükenthal specialized in the Octocorallia an .... References Glaciers of Svalbard Barentsøya {{svalbard-glacier-stub ...
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Freemanbreen
Freemanbreen is a glacier on Barentsøya, Svalbard. It is an offshoot of Barentsjøkulen, reaching down to the sea in the southern direction, into Freeman Strait Freemansundet is the sound separating Barentsøya, to the north, from Edgeøya, in the Svalbard archipelago, Norway. Background The straight is named after Alderman Ralph Freeman, who was involved in the English whaling trade in the early 17th ce .... The glacier is named after British Alderman Ralph Freeman. The mountain of Buklerimen separates Freemanbreen from the glacier of Hübnerbreen. References Glaciers of Svalbard Barentsøya {{svalbard-glacier-stub ...
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Duckwitzbreen
Duckwitzbreen is a glacier on Barentsøya, Svalbard. It is an offshoot of Barentsjøkulen, reaching down to the sea in the western direction. The glacier is named after German politician Arnold Duckwitz Arnold Duckwitz (27 January 1802 in Bremen Germany – 19 March 1881 in Bremen) was a German statesman and merchant who served as Minister of Trade and of the Navy in the provisional government of the Frankfurt Assembly of 1848–49, and .... References Glaciers of Svalbard Barentsøya {{svalbard-glacier-stub ...
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List Of Glaciers In Svalbard
This is a list of glaciers in Svalbard. It includes glaciers and ice caps in Svalbard, Norway. List of glaciers and ice caps Ice caps *Austfonna *Biscayarfonna *Glitnefonna *Lomonosovfonna *Løvenskioldfonna *Valhallfonna *Vegafonna *Vestfonna Glaciers *Aavatsmarkbreen *Abrahamsenbreen *Adambreen *Adolfbreen *Akademikarbreen *Aldegondabreen *Angelbreen *Antoniabreen *Arbobreen *Arlabreen *Arneliusbreen *Åsgardfonna *Austgötabreen *Austjøkulen *Bakaninbreen *Balderfonna *Barentsjøkulen *Belopol'skijbreen *Besselsbreen *Bjørlykkebreen *Bjørnbreen *Blomstrandbreen *Borebreen *Bragebreen *Bråsvellbreen *Brazybreen *Buchananisen *Buchanbreen *Bullbreen *Bungebreen *Charlesbreen *Charpentierbreen *Chauveaubreen *Chomjakovbreen *Chydeniusbreen *Comfortlessbreen *Dahlbreen *Deltabreen *Devikbreen *Dollfusbreen *Duckwitzbreen *Dunderdalsbreen *Edgeøyjøkulen *Eidembreen *Elfenbeinbreen *Erdmannbreen *Esmarkbreen *Etonbreen *Fimbulisen *Fjortende Julibreen *Flakbreen *Foldnutfon ...
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Glacier
A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land“Glacier, N., Pronunciation.” Oxford English Dictionary, Oxford UP, June 2024, https://doi.org/10.1093/OED/7553486115. Accessed 25 Jan. 2025. and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on ever ...
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Svalbard
Svalbard ( , ), previously known as Spitsbergen or Spitzbergen, is a Norway, Norwegian archipelago that lies at the convergence of the Arctic Ocean with the Atlantic Ocean. North of continental Europe, mainland Europe, it lies about midway between the northern coast of Norway and the North Pole. The islands of the group range from 74th parallel north, 74° to 81st parallel north, 81° north latitude, and from 10th meridian east, 10° to 35th meridian east, 35° east longitude. The largest island is Spitsbergen (37,673 km2), followed in size by Nordaustlandet (14,443 km2), (5,073 km2), and Barentsøya (1,288 km2). Bear Island (Norway), Bjørnøya or Bear Island (178 km2) is the most southerly island in the territory, situated some 147 km south of Spitsbergen. Other small islands in the group include Hopen (Svalbard), Hopen to the southeast of Edgeøya, Kongsøya and Svenskøya in the east, and Kvitøya to the northeast. The largest settlement is Longyearbyen, situated in Isfjor ...
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Norwegian Polar Institute
The Norwegian Polar Institute (NPI; ) is Norway's central governmental institution for scientific research, mapping and environmental monitoring in the Arctic and the Antarctic. The NPI is a directorate under Norway's Ministry of Climate and Environment (Norway), Ministry of Climate and Environment. The institute advises Norwegian authorities on matters concerning polar environmental management and is the official environmental management body for Norwegian activities in Antarctica. Activities The institute's activities are focused on environmental research and management in the polar regions. The NPI's researchers investigate biodiversity, climate and environmental toxins in the Arctic and Antarctic, and in this context the institute equips and organizes large-scale expeditions to both polar regions. The institute contributes to national and international climate work, and is an active contact point for the international scientific community. The institute collects and analyses ...
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Store Norske Leksikon
The ''Great Norwegian Encyclopedia'' (, abbreviated ''SNL'') is a Norwegian-language online encyclopedia. It has several subdivisions, including the Norsk biografisk leksikon. The online encyclopedia is among the most-read Norwegian published sites, with up to 3.5 million unique visitors per month. Paper editions (1978–2007) The ''SNL'' was created in 1978, when the two publishing houses Aschehoug and Gyldendal merged their encyclopedias and created the company Kunnskapsforlaget. Up until 1978 the two publishing houses of Aschehoug and Gyldendal, Norway's two largest, had published ' and ', respectively. The respective first editions were published in 1906–1913 (Aschehoug) and 1933–1934 (Gyldendal). The slump in sales of paper-based encyclopedias around the turn of the 21st century hit Kunnskapsforlaget hard, but a fourth edition of the paper encyclopedia was secured by a grant of ten million Norwegian kroner from the foundation Fritt Ord in 2003. The f ...
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Willem Barentsz
Willem Barentsz (; – 20 June 1597), anglicized as William Barents or Barentz, was a Dutch Republic, Dutch navigator, cartographer, and Arctic explorer. Barentsz went on three expeditions to the far north in search for a Northern Sea Route, Northeast passage. He reached as far as Novaya Zemlya and the Kara Sea in his first two voyages, but was turned back on both occasions by ice. During a third expedition, the crew discovered Spitsbergen and Bear Island (Norway), Bear Island, but subsequently became stranded on Novaya Zemlya for almost a year. Barentsz died on the return voyage in 1597. The Barents Sea, among many other places, is named after him. Life and career Willem Barentsz was born around 1550 in the village Formerum on the island Terschelling in the Seventeen Provinces, present-day Netherlands. ''Barentsz'' was not his surname but rather his Dutch_name#Patronymics, patronymic name, short for ''Barentszoon'' "Barent's son". A cartographer by trade, Barentsz sailed to ...
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Glaciers Of Svalbard
A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land“Glacier, N., Pronunciation.” Oxford English Dictionary, Oxford UP, June 2024, https://doi.org/10.1093/OED/7553486115. Accessed 25 Jan. 2025. and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every co ...
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