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Forlandsundet
Forlandsundet is an 88 km long sound separating Prins Karls Forland and Spitsbergen. Its northern limits are Fuglehuken to the west and Kvadehuken to the east. Its southern limits are Salpynten to the west and Daudmannsodden to the east. References * Norwegian Polar InstitutPlace names in Norwegian polar areas Straits of Svalbard Spitsbergen {{Spitsbergen-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Daudmannsodden
Daudmannsodden ("Dead Man's Cape") is a headland in Oscar II Land at Spitsbergen, Svalbard. It has a length of about three kilometers. Daudmannsodden and Salpynten mark the southern entrance of the strait of Forlandsundet. The coast between Daudmannsodden and Eidembukta is characterized by foul waters, skerries and islets outside small bays. References Headlands of Spitsbergen {{Spitsbergen-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spitsbergen Labelled
Spitsbergen (; formerly known as West Spitsbergen; Norwegian: ''Vest Spitsbergen'' or ''Vestspitsbergen'' , also sometimes spelled Spitzbergen) is the largest and the only permanently populated island of the Svalbard archipelago in northern Norway. Constituting the westernmost bulk of the archipelago, it borders the Arctic Ocean, the Norwegian Sea, and the Greenland Sea. Spitsbergen covers an area of , making it the largest island in Norway and the 36th-largest in the world. The administrative centre is Longyearbyen. Other settlements, in addition to research outposts, are the Russian mining community of Barentsburg, the research community of Ny-Ålesund, and the mining outpost of Sveagruva. Spitsbergen was covered in of ice in 1999, which was approximately 58.5% of the island's total area. The island was first used as a whaling base in the 17th and 18th centuries, after which it was abandoned. Coal mining started at the end of the 19th century, and several permanent comm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prins Karls Forland
Prins Karls Forland or Forlandet, occasionally anglicized as Prince Charles Foreland, is an island off the west coast of Oscar II Land on Spitsbergen in the Arctic archipelago of Svalbard, Norway. The entire island and the surrounding sea area constitutes Forlandet National Park (''Forlandet nasjonalpark''). History The island was first seen by the Dutch explorer Willem Barentsz in 1596. In 1610, the English explorer Jonas Poole named it ''Black Point Isle''. By 1612 the English whalers were referring to the island as ''Prince Charles' Foreland'', after King James's son, Charles (later king of England and Scotland). The Dutch called it ''Kijn Island'', after a merchant, who, climbing a tall hill in 1612, fell and broke his neck. The English built a temporary whaling station on the island's northern tip, known to the English as ''Fair Foreland'' (today Fuglehuken). See also * List of islands of Norway This is a list of islands of Norway sorted by name. For a list sorted by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spitsbergen
Spitsbergen (; formerly known as West Spitsbergen; Norwegian: ''Vest Spitsbergen'' or ''Vestspitsbergen'' , also sometimes spelled Spitzbergen) is the largest and the only permanently populated island of the Svalbard archipelago in northern Norway. Constituting the westernmost bulk of the archipelago, it borders the Arctic Ocean, the Norwegian Sea, and the Greenland Sea. Spitsbergen covers an area of , making it the largest island in Norway and the 36th-largest in the world. The administrative centre is Longyearbyen. Other settlements, in addition to research outposts, are the Russian mining community of Barentsburg, the research community of Ny-Ålesund, and the mining outpost of Sveagruva. Spitsbergen was covered in of ice in 1999, which was approximately 58.5% of the island's total area. The island was first used as a whaling base in the 17th and 18th centuries, after which it was abandoned. Coal mining started at the end of the 19th century, and several permanent commun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fuglehuken
Fuglehuken ( en, bird hook) is a headland at the northern end of Prins Karls Forland, 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 .... The headland includes the mountain Fuglehukfjellet (583 meters). A radio beacon was installed at Fuglehuken in 1946. References Headlands of Svalbard Prins Karls Forland {{svalbard-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kvadehuken
Kvadehuken is a cape at the northwestern corner of Brøggerhalvøya, located at the southwestern side of outlet of Kongsfjorden, in Oscar II Land on Spitsbergen, Svalbard. The name is a Norwegian spelling of nl, Quade hoek (bad corner). The Norwegian geophysical station at Kvadehuken, a research facility, was established in 1920 by the Geophysical Institute of Tromsø. Brothers Hallvard and Finn Devold Finn Devold (born 24 April 1902 in Bergen, died 26 May 1977) was a Norwegian Arctic explorer, marine biologist and meteorologist. His father was parish priest Harald Ophus Devold. Together with his brother Hallvard Devold, Finn shared an interest ... worked at the facility. In October 1924, the station was wrapped up for financial reasons.Roger Norum & James Proctor, ''Svalbard: Spitsbergen, Jan Mayen and Franz Josef Land'', p. 191 References Headlands of Spitsbergen {{Spitsbergen-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Straits Of Svalbard
A strait is an Ocean, oceanic landform connecting two Sea, seas or two other large areas of water. The surface water generally flows at the same elevation on both sides and through the strait in either direction. Most commonly, it is a narrow ocean Channel (geography), channel that lies between two land masses. Some straits are not navigable, for example because they are either too narrow or too shallow, or because of an unnavigable reef or archipelago. Straits are also known to be loci for sediment accumulation. Usually, sand-size deposits occur on both the two opposite strait exits, forming subaqueous fans or deltas. Terminology The terms ''channel (geography), channel'', ''pass'', or ''passage'' can be synonymous and used interchangeably with ''strait'', although each is sometimes differentiated with varying senses. In Scotland, ''firth'' or ''Kyle'' are also sometimes used as synonyms for strait. Many straits are economically important. Straits can be important shipping ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
