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Ginevra Bay
Ginevra Bay () is the inner part of Storfjorden, Svalbard, between Barentsøya and Spitsbergen Spitsbergen (; formerly known as West Spitsbergen; Norwegian language, Norwegian: ''Vest Spitsbergen'' or ''Vestspitsbergen'' , also sometimes spelled Spitzbergen) is the largest and the only permanently populated island of the Svalbard archipel .... It is named after James Lamont's vessel ''Ginevra''. References Fjords of Svalbard Barentsøya Landforms of Spitsbergen {{svalbard-fjord-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ginevrabotnen
Ginevra Bay () is the inner part of Storfjorden (Svalbard), Storfjorden, Svalbard, between Barentsøya and Spitsbergen. It is named after James Lamont (explorer), James Lamont's vessel ''Ginevra''. References Fjords of Svalbard Barentsøya Landforms of Spitsbergen {{svalbard-fjord-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Storfjorden (Svalbard)
Storfjorden ( English: ''Great Fjord'') is the body of water in the Svalbard archipelago in northern Norway separating Spitsbergen in the west from Barentsøya and Edgeøya Edgeøya (), anglicised as Edge Island, is a Norway, Norwegian island located in southeast of the Svalbard archipelago; with an area of , it is the third-largest island in this archipelago. An Arctic island, it forms part of the Søraust-Svalbard ... to the east. Its southern limits are Kikutodden in Sørkapp Land east to Håøya, Tiholmane, Brækmoholmane, and Menkeøyane in Thousand Islands and northeast to Svarthuken—the southeastern promontory of Edgeøya. Its limits on its eastern side are Sundneset on the northern side of Freemansundet south to Palibinramten on the northwest coast of Edgeøya. The northern part is called Ginevra Bay, which lies between Olav V Land and Barentsøya. It ends at Heleysundet. Storfjorden was historically known as ''Wybe Jans Water'', named after the Frisian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barentsøya
Barentsøya, anglicized as Barents Island, is an Arctic island in the Svalbard archipelago of Norway, lying between Edgeøya and Spitsbergen. To the north, in the sound between Barentsøya and Spitsbergen, lies the island of Kükenthaløya. To the south, the sound (geography), sound separating Barents Island from Edgeøya is Freeman Strait, Freemansundet. Barentsøya has Uninhabited island, no permanent human inhabitants. It is part of the Søraust-Svalbard Nature Reserve and forms a habitat for several species, including polar bears and kittiwakes. History The island was named after Netherlands, Dutch explorer Willem Barents who, despite discovering Svalbard, never sighted Barentsøya itself. The name "Barents Land" was only given after an 1865 Swedish expedition. Previously, Dutch whaling captains had referred to it on maps as ''Zuyd Ooster Land'' ("Southeastern Land") as early as 1710. In 1936, Norway built four cabins on the island to formally establish control. Geography ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spitsbergen
Spitsbergen (; formerly known as West Spitsbergen; Norwegian language, 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 in the Arctic Ocean. 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 List of islands by area, 36th largest in the world. The administrative centre is Longyearbyen. Other settlements, in addition to research outposts, are the 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 e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
James Lamont (explorer)
James Lamont (28 April 1828 – 29 July 1913) was a Scottish explorer and author, particularly known for his voyages in the Arctic in 1858–1859 and 1869–1871, which were the topic of his two books, ''Seasons with the Sea-Horse'' (1861) and ''Yachting in the Arctic Seas'' (1876). He was a fellow of the Geological Society of London and the Royal Geographical Society. He served as the Liberal Member of Parliament for Buteshire (1865–1868), and was created a baronet in 1910. Early life James Lamont was born on 28 April 1828 in Knockdow, Toward, on the Cowal peninsula in Argyll, to Jane (''née'' Chrystie) and Alexander Lamont (1784–1861), a lawyer, Lieutenant-Colonel in the Bute militia and laird of Knockdow. His grandfather, also James Lamont, was a noted agriculturalist. James attended Rugby School, followed by the Edinburgh Military Academy. He served in the 91st Argyllshire Highlanders regiment in 1846–48, initially based in South Africa. A large inheritance then ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fjords Of Svalbard
In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords when flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or glacia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
