Rijpdalen
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Rijpdalen
Rijpdalen is a valley in the central part of Nordaustlandet, Svalbard, separating Gustav V Land from Prins Oscars Land. The valley extends between the head of Wahlenbergfjorden and the head of Rijpfjorden. The valley is named after Dutch explorer Jan Rijp. At the watershed in Rijpdalen is the plain of Helvetesflya. The ice caps of Vestfonna and Austfonna Austfonna is an ice cap located on Nordaustlandet in the Svalbard archipelago in Norway. Covering an area of 7,800 km2, it is Europe's third-largest glacier by area and volume, after the Severny Island ice cap of Novaya Zemlya, Russia, an ... are separated by Rijpdalen and Helvetesflya. References Valleys of Svalbard Nordaustlandet {{Nordaustlandet-geo-stub ...
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Gustav V Land
Gustav V Land is a land area comprising the peninsula on the northwestern part of Nordaustlandet, Svalbard in Arctic Norway. It constitutes roughly one quarter of the island's area, approximately 4000 km2, being some 80 km wide east–west and 85 km north–south, connected to the rest of the island by a 22-km-wide isthmus in the southeast. The peninsula is bordered to the south by Wahlenbergfjorden, to the west by Hinlopen Strait and Hinlopenrenna, to the north by Nordkappsundet, and to the east by Nordenskiöldbukta and Rijpfjorden. Gustav Adolf Land is to the south and Prins Oscars Land is to the east. The boundary of Gustav V Land passes through Rijpdalen and Flaumdalen to Winsnesbreen in the east, continues further southwest to Brånevatnet, and thence follows the river from Brånevatnet to the sea at Bodleybukta. The highest elevation is on the glacier Vestfonna, which covers large parts of the land. The coast is heavily indented, especially in the west and ...
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Prins Oscars Land
Prins Oscars Land is a land area constituting mainly Platenhalvøya, a peninsula between Rijpfjorden in the west and Duvefjorden with Fortherbyfjorden and Innvika on Nordaustlandet, Svalbard in Arctic Norway. Bordering Gustav V Land to the west, Gustav Adolf Land to the south, Orvin Land and Austfonna to the east. Limit over land through Rijpdalen and Flaumdalen in the west, to Winsnesbreen in the south, the lower part of Austfonna, through Fonndalen and Innvikdalen to the east. Named after Prince Oscar (1829 – 1907), later King Oscar II of Norway (1872 - 1905) and Sweden Sweden, formally the Kingdom of Sweden, is a Nordic countries, Nordic country located on the Scandinavian Peninsula in Northern Europe. It borders Norway to the west and north, and Finland to the east. At , Sweden is the largest Nordic count ... (1872 - 1907). References Geography of Svalbard Nordaustlandet {{Nordaustlandet-geo-stub ...
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Nordaustlandet
Nordaustlandet (Anglicised 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 Svalbard reindeer, reindeer and walruses. The island is uninhabited and lies entirely within Nordaust-Svalbard Nature Reserve. History English people, 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 Republic, Dutch 1662 map, and the following year another Dutch map marked its coastline more distinctly, showing its west and north coasts, ...
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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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Wahlenbergfjorden
Wahlenbergfjorden, sometimes known in English as Waalenburg Bay, is a fjord on the southwest coast of the Arctic island of Nordaustlandet, in Norway's Svalbard archipelago. At in length, and wide, it is the fifth longest fjord in the archipelago, and the longest on the island. The fjord separates Gustav V Land in the north from Gustav Adolf Land in the south, at geographical co-ordinates . Its mouth faces Spitsbergen across Hinlopen Strait, the strait separating the two islands. The fjord is named for the Swedish naturalist Göran Wahlenberg (1780-1851) and has been known by this name since at least the early 1930s. The glacier of Wahlenbergbreen in Oscar II Land, Spitsbergen, is also named for him. References * Wahlenbergfjord', Svalbard place names database, Norwegian Polar Institute, 2005 (URL accessed 29 July 2006) * Wahlenbergbreen', Svalbard place names database, Norwegian Polar Institute The Norwegian Polar Institute (NPI; ) is Norway's central governmental in ...
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Rijpfjorden
Rijpfjorden is a fjord at the northern side of Nordaustlandet, 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 .... The fjord has a length of about and a width of about . Former names of the fjord include ''Rypefjorden'', ''Red Currant Bay'' and ''Ripsbai''. The fjord is named after Dutch explorer Jan Rijp, who never came anywhere near it. References Fjords of Svalbard Nordaustlandet {{Nordaustlandet-fjord-stub ...
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Jan Rijp
Jan Cornelisz Rijp (–) was a Dutch mariner best known for his involvement with Willem Barentsz in finding a route to the East, avoiding the Spanish and the Portuguese fleets in the South. In May 1596, Rijp was named captain of the second of two ships commissioned to Barents by Dutch merchants to discover the fabled Northeast Passage to the East Indies. Jacob van Heemskerck captained the first ship, and Barents served as its pilot. After discovering Spitsbergen, the ships encountered pack ice blocking the way. Barents decided to turn east and round the northern tip of Novaya Zemlya, as he had successfully managed once before. When Barents urged Rijp to follow, he refused. Rijp insisted that the northern tip of Novaya Zemlya was far too dangerous and returned to the Netherlands.''Ein heißes Bad in der Eiswüste'' in Frankfurter Allgemeine Sonntagszeitungvom 2. Oktober 2011, Seiten 60 und 62 Barents and his ship continued in the attempt to round Novaya Zemlya. He realized too lat ...
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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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Vestfonna
Vestfonna is an ice cap located on the western part Nordaustlandet in the Svalbard archipelago in Norway. The glacier covers an area of about 2,500 km2. It is the third largest ice cap in Svalbard and Norway by area, after Austfonna and Olav V Land. See also * List of glaciers A glacier ( ) or () is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly defor ... * List of glaciers in Norway References Glaciers of Nordaustlandet {{Nordaustlandet-geo-stub ...
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Austfonna
Austfonna is an ice cap located on Nordaustlandet in the Svalbard archipelago in Norway. Covering an area of 7,800 km2, it is Europe's third-largest glacier by area and volume, after the Severny Island ice cap of Novaya Zemlya, Russia, and Vatnajökull in Iceland Iceland is a Nordic countries, Nordic island country between the Atlantic Ocean, North Atlantic and Arctic Oceans, on the Mid-Atlantic Ridge between North America and Europe. It is culturally and politically linked with Europe and is the regi .... The combined area of Austfonna and the Vegafonna ice cap is 8,492 km2. Austfonna has a thickness of up to 560 metres (235 meters average thickness), and is 200 km in circumference. The ice dome reaches an elevation of 783 meters above sea level. The southern third of Austfonna is sometimes called Sørfonna, which is a separate ice cap, separated from the main part of Austfonna by a long, ice-filled depression, and forming a separate crestal dome. Ve ...
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Valleys Of Svalbard
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. Format ...
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