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Svarthuken
Svarthuken is a headland at Edgeøya, Svalbard. It is the southernmost point of Edgeøya, and has a length of about two kilometers. The rock consists of dark shales, and reaches 326 m.a.s.l. The bay Tjuvfjorden is located between Svarthuken and Kvalpynten further northwest. To the east is the strait Halvmånesundet. Name history The headland was named ''Negro Point'' by English sailors in the 17th century The 17th century lasted from January 1, 1601 (represented by the Roman numerals MDCI), to December 31, 1700 (MDCC). It falls into the early modern period of Europe and in that continent (whose impact on the world was increasing) was characterized ... and was the official name from 1871. It was changed to the more Norwegian sounding ''Negerpynten'' in 1933. After complaints about racism the name was changed to ''Svarthuken'' in 2023. References Headlands of Svalbard Edgeøya {{svalbard-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tjuvfjorden
Tjuvfjorden () is a 45 km long and up to 30 km wide fjord separating Edgeøya’s two southern promontories, Kvalpynten (Whale Point) and Svarthuken (old name: Negro Point). The fjord was originally named ''Deicrowe's Sound'' by the English in 1616 after Benjamin Decrow, who was a leading figure of the Muscovy Company from 1610 onwards. This name appears on the Muscovy Company's map (1625) down to at least William Scoresby William Scoresby (5 October 178921 March 1857) was an English whaler, Arctic explorer, scientist and clergyman. Early years Scoresby was born in the village of Cropton near Pickering south-west of Whitby in Yorkshire. His father, Willia ...’s (1820). References and sources ;References ;Sources * Norwegian Polar InstitutePlace names in Norwegian polar areas* Purchas, S. 1625. ''Hakluytus Posthumus or Purchas His Pilgrimes: Contayning a History of the World in Sea Voyages and Lande Travells by Englishmen and others''. Volumes XIII and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kvalpynten
Kvalpynten (Whale Point) is a headland at Edgeøya, Svalbard. It is the most southwestern point of Edgeøya. The headland contains the mountain Kvalpyntfjellet, and the summit of the glacier Kvalpyntfonna further east is the highest point on Edgeøya. The bay Tjuvfjorden is located between Kvalpynten and Svarthuken Svarthuken is a headland at Edgeøya, Svalbard. It is the southernmost point of Edgeøya, and has a length of about two kilometers. The rock consists of dark shales, and reaches 326 m.a.s.l. The bay Tjuvfjorden is located between Svarthuken and ... further southeast. References Headlands of Svalbard Edgeøya {{svalbard-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Halvmånesundet
Halvmånesundet is a strait between Halvmåneøya and Edgeøya, Svalbard. It is located east of the peninsula with the headland Svarthuken Svarthuken is a headland at Edgeøya, Svalbard. It is the southernmost point of Edgeøya, and has a length of about two kilometers. The rock consists of dark shales, and reaches 326 m.a.s.l. The bay Tjuvfjorden is located between Svarthuken and .... The strait has a width of about 1.8 nautical miles at the narrowest point. References Straits of Svalbard {{svalbard-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape (geography)
In geography, a cape is a headland, peninsula or promontory extending into a body of water, usually a sea. A cape usually represents a marked change in trend of the Coast, coastline, often making them important landmarks in sea navigation. This also makes them prone to natural forms of erosion, mainly tidal actions, resulting in a relatively short geological lifespan. Formation Capes can be formed by Glacier, glaciers, Volcano, volcanoes, and changes in sea level. Erosion plays a large role in each of these methods of formation. Coastal erosion by waves and currents can create capes by wearing away softer rock and leaving behind harder rock formations. Movements of the Earth's crust can uplift land, forming capes. For example, the Cape of Good Hope was formed by tectonic forces. Volcanic eruptions can create capes by depositing lava that solidifies into new landforms. Cape Verde, (also known as Cabo Verde) is an example of a volcanic cape. Glaciers can carve out capes by erod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Nature Reserve, home to polar bears and reindeer. An ice field covers its eastern side. The island takes its name from Thomas Edge (died 1624), an England, English merchant and whaling, whaler. It is seldom visited today and development of tourist facilities is forbidden by law because of its nature reserve status. History The history of Edgeøya's discovery has been a matter of dispute. Thomas Edge, writing in 1622, claimed the island was discovered by one of his ships in 1616. However, Joris Carolus, in a map published in 1614 and allegedly based on discoveries made by him the same year, shows what appears to be Edgeøya's south coast. Carolus showed the coastline split into two parts: "Onbekende Cust" (meaning "Unknown Coast" in Dutc ... [...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] |
Headland
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 erosio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
17th Century
The 17th century lasted from January 1, 1601 (represented by the Roman numerals MDCI), to December 31, 1700 (MDCC). It falls into the early modern period of Europe and in that continent (whose impact on the world was increasing) was characterized by the Baroque cultural movement, the latter part of the Spanish Golden Age, the Dutch Golden Age, the French ''Grand Siècle'' dominated by Louis XIV, the Scientific Revolution, the world's first public company and megacorporation known as the Dutch East India Company, and according to some historians, the General Crisis. From the mid-17th century, European politics were increasingly dominated by the Kingdom of France of Louis XIV, where royal power was solidified domestically in the civil war of the Fronde. The semi-feudal territorial French nobility was weakened and subjugated to the power of an absolute monarchy through the reinvention of the Palace of Versailles from a hunting lodge to a gilded prison, in which a greatly expanded ro ... [...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] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
