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Svartknausflya
Svartknausflya is a coastal plain in Gustav Adolf Land in Nordaustlandet, Svalbard. The length of the plain is about 21 kilometers. West of the plain is Rosenthalbreen, and to the east is Vibebukta and Bråsvellbreen Bråsvellbreen ( en, The Sudden Swell Glacier) is a glacier in Nordaustlandet, Svalbard. The glacier is a 45 kilometre long stream southwards from the ice dome Sørdomen of Austfonna, debouching into the sea on the south coast. In the late 1930s it .... References Plains of Svalbard Nordaustlandet {{Nordaustlandet-geo-stub ...
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Rosenthalbreen
Rosenthalbreen is a glacier in Gustav Adolf Land in Nordaustlandet, Svalbard. It is named after German shipowner and expedition organizer Friedrich Wilhelm Albert Rosenthal. The glacier is an outlet from Vegafonna. It borders to the coastal plain of Svartknausflya, and drains into the sea east of Torellneset, into the bay Ulvebukta of Hinlopen Strait The Hinlopen Strait ( no, Hinlopenstretet) is the strait between Spitsbergen and Nordaustlandet in Svalbard, Norway. It is long and wide. The strait is difficult to pass because of pack ice. It is believed to have been named after Thijmen J .... References Glaciers of Nordaustlandet {{nordaustlandet-glacier-stub ...
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Nordaustlandet
Nordaustlandet (sometimes translated as North East Land) is the second-largest island in the archipelago of Svalbard, Norway, with an area of . It lies north east of Spitsbergen, separated by Hinlopen Strait. Much of Nordaustlandet lies under large ice caps, mainly Austfonna and Vestfonna, the remaining parts of the north being tundra inhabited by reindeer and walruses. The island is uninhabited and lies entirely within Nordaust-Svalbard Nature Reserve. History English walrus hunters first sighted the south point of Nordaustlandet in 1617. This discovery was shown on the ''Muscovy Company's map'' (1625; but based on discoveries made in and prior to 1622), with the island labeled as ''Sir Thomas Smyth's Iland''. It also shows the North Cape (''Point Purchas''). It is first named ''Oostlandt'' ("East Land") on a Dutch 1662 map, and the following year another Dutch map marked its coastline more distinctly, showing its west and north coasts, separating the latter from the Seven Isl ...
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Gustav Adolf Land
Gustav Adolf Land is the land area of the southwestern part of Nordaustlandet, Svalbard, south of Wahlenbergfjorden. The area is named after Gustaf VI Adolf of Sweden Gustav, Gustaf or Gustave may refer to: * Gustav (name), a male given name of Old Swedish origin Art, entertainment, and media * ''Primeval'' (film), a 2007 American horror film * ''Gustav'' (film series), a Hungarian series of animated short car .... References Geography of Svalbard Nordaustlandet {{Nordaustlandet-geo-stub ...
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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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Vibebukta
Vibebukta is a bay at the shore of Nordaustlandet, Svalbard. The bay is named after hydrographer Andreas Vibe. It lies between Gustav Adolf Land and the glacier Bråsvellbreen. The twenty nautical miles wide glacier front of Bråsvellbreen, between Vibebukta and Kervelbukta, exhibited a huge surge Surge means a sudden transient rush or flood, and may refer to: Science * Storm surge, the onshore gush of water associated with a low-pressure weather system * Surge (glacier), a short-lived event where a glacier can move up to velocities 100 ... in the 1930s. References Bays of Svalbard Nordaustlandet {{Nordaustlandet-geo-stub ...
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Bråsvellbreen
Bråsvellbreen ( en, The Sudden Swell Glacier) is a glacier in Nordaustlandet, Svalbard. The glacier is a 45 kilometre long stream southwards from the ice dome Sørdomen of Austfonna, debouching into the sea on the south coast. In the late 1930s it was observed that the glacier had exhibited a recent huge surge, forming a ten kilometre long tongue The tongue is a muscular organ (anatomy), organ in the mouth of a typical tetrapod. It manipulates food for mastication and swallowing as part of the digestive system, digestive process, and is the primary organ of taste. The tongue's upper surfa ... into the sea. References Glaciers of Nordaustlandet {{Nordaustlandet-glacier-stub ...
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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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Plains Of Svalbard
In geography, a plain is a flat expanse of land that generally does not change much in elevation, and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or uplands. In a valley, a plain is enclosed on two sides, but in other cases a plain may be delineated by a complete or partial ring of hills, by mountains, or by cliffs. Where a geological region contains more than one plain, they may be connected by a pass (sometimes termed a gap). Coastal plains mostly rise from sea level until they run into elevated features such as mountains or plateaus. Plains are one of the major landforms on earth, where they are present on all continents, and cover more than one-third of the world's land area. Plains can be formed from flowing lava; from deposition of sediment by water, ice, or wind; or formed by erosion by the agents from hills and mountains. Biomes on plains include grassland (temperate or subtropical), ste ...
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