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Fuglehuken
Fuglehuken ( en, bird hook) is a headland at the northern end of 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 ..., Svalbard. 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 ...
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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 ...
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Svalbard
Svalbard ( , ), also known as Spitsbergen, or Spitzbergen, is a Norway, Norwegian archipelago in the Arctic Ocean. North of continental Europe, mainland Europe, it is 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, followed by Nordaustlandet and . The largest settlement is Longyearbyen. The islands were first used as a base by the Whaling, 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 ...
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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 environ ...
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Headlands Of Svalbard
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the ...
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