Rundisen
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Rundisen
Rundisen is a small glacier at Kongsøya in Kong Karls Land, Svalbard. The glacier covers part of Rundisflya at the eastern part of Kongsøya, south of Svenskebukta Svenskebukta is a bay at the northern side of Kongsøya of Kong Karls Land, Svalbard. It is located between Kapp Oscar and eastwards towards a point west of Nordaustpynten. Former name variants of the bay are ''Holmbukta'', sv, Svenska Segelsälls .... Former names are the English name ''The Circular Ice Cap'' and sv, Runda Iskalotten. References Glaciers of Svalbard Kongsøya {{svalbard-glacier-stub ...
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Kongsøya
Kongsøya is an island in Svalbard, Norway. It is the largest of the islands in King Charles Land (Kong Karls Land). Its area is . The other main island in the chain is Svenskøya. Geography Kongsøya is the largest island in Kong Karls Land, and has a length of about 40 kilometers. It is separated from Abel Island to the east-northeast by the seven nautical miles wide strait Lydiannasundet, and from Svenskøya to the west-southwest by Rivalensundet (15 nautical miles wide). The strait of Erik Eriksenstretet separates Kongsøya from Nordaustlandet. Kongsøya has a long, narrow and bent shape, with a number of headlands and bays. At the southern side of Kongsøya is the wide open bay Breibukta, with several islets and skerries. The islands of Helgoland Island and Tirpitzøya are located south of Breibukta. Further east, between Tømmerneset and Bremodden, is the bay Andréebukta, and on the northern side is Svenskebukta. Further east is the bay Bünsowbukta, between the headlan ...
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Rundisflya
Rundisflya is a plain at the eastern part of Kongsøya in Kong Karls Land, Svalbard. It is located west of the mountain Johnsenberget, and generally has a height of 50 m.a.s.l. or higher. Rundisflya is named after the glacier Rundisen Rundisen is a small glacier at Kongsøya in Kong Karls Land, Svalbard. The glacier covers part of Rundisflya at the eastern part of Kongsøya, south of Svenskebukta Svenskebukta is a bay at the northern side of Kongsøya of Kong Karls Land, Svalb ..., which covers part of the plain. References Plains of Svalbard Kongsøya {{svalbard-geo-stub ...
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Svenskebukta
Svenskebukta is a bay at the northern side of Kongsøya of Kong Karls Land, Svalbard. It is located between Kapp Oscar and eastwards towards a point west of Nordaustpynten. Former name variants of the bay are ''Holmbukta'', sv, Svenska Segelsällskapets Bay and ''Swedish Yacht Club Bay''. The glacier Rundisen Rundisen is a small glacier at Kongsøya in Kong Karls Land Kong Karls Land or King Charles Land is an island group in the Svalbard archipelago, in the Arctic Ocean. The island group covers an area of and is made up of the islands of Kongsøya, ... debouches into the bay. References Bays of Svalbard Kongsøya {{svalbard-geo-stub ...
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Kong Karls Land
Kong Karls Land or King Charles Land is an island group in the Svalbard archipelago, in the Arctic Ocean. The island group covers an area of and is made up of the islands of Kongsøya, Svenskøya, Abel Island, Helgoland Island, and Tirpitzøya. The islands, which have the largest concentration of polar bear in Svalbard, are part of the Nordaust-Svalbard Nature Reserve, along with Nordaustlandet and Kvitøya. There is a ban on traffic to the islands, which includes the areas of the sea up to 500 metres away from shore and the airspace up to 500 metres above the area. Kong Karls Land was discovered by an expedition sent by the Muscovy Company in 1617, probably from a high point on Barentsøya. They named the group ''Wiche Islands,'' after a member of the company, Richard Wyche. Ecology The polar bear is found during portions of the year at Kong Karls Land; this bear feeds on local harp seals and ring seals. The sub-population of polar bears found here is a genetically distinct ...
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Svalbard
Svalbard ( , ), also known as Spitsbergen, or Spitzbergen, is a Norwegian archipelago in the Arctic Ocean. North of mainland Europe, it is about midway between the northern coast of Norway and the North Pole. The islands of the group range from 74° to 81° north latitude, and from 10° to 35° east longitude. The largest island is Spitsbergen, followed by Nordaustlandet and . The largest settlement is Longyearbyen. The islands were first used as a base by the whalers who sailed far north in the 17th and 18th centuries, after which they were abandoned. Coal mining started at the beginning of the 20th century, and several permanent communities were established. The Svalbard Treaty of 1920 recognizes Norwegian sovereignty, and the 1925 Svalbard Act made Svalbard a full part of the Kingdom of Norway. They also established Svalbard as a free economic zone and a demilitarized zone. The Norwegian Store Norske and the Russian remain the only mining companies in place. Res ...
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Norwegian Polar Institute
The Norwegian Polar Institute (NPI; no, Norsk Polarinstitutt) 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. 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 data on the environm ...
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Glaciers Of Svalbard
A glacier (; ) is a persistent body of dense ice that is constantly moving 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 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 continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur ...
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