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Antarctic Bay (Greenland)
Antarctic Bay ( da, Antarctic Bugt) is a bay in the Greenland Sea coast of the Crown Prince Christian Land peninsula, King Frederick VIII Land, Northeastern Greenland. Administratively the bay and its surroundings belong to the Northeast Greenland National Park. The area of the bay is uninhabited. History The bay was named by the 1906-1908 Denmark expedition after Alfred Gabriel Nathorst's ship ''Antarctic''.''Catalogue of place names in northern East Greenland''. Geological Survey of Denmark and Greenland. Geography Antarctic Bay opens to the Fram Strait of the Greenland Sea. It lies between Amdrup Land to the west and the Flade Isblink ice cap to the north. It is a fairly wide bay, with the Nordostrundingen about to the northeast of its unnamed northeastern point. Sophus Müller Naes is the southwestern point of the bay.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute,'' p. 128. Kilen lies just a few km north of the ice-covered head and northeastern shore of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greenland
Greenland ( kl, Kalaallit Nunaat, ; da, Grønland, ) is an island country in North America that is part of the Kingdom of Denmark. It is located between the Arctic and Atlantic oceans, east of the Canadian Arctic Archipelago. Greenland is the world's largest island. It is one of three constituent countries that form the Kingdom of Denmark, along with Denmark and the Faroe Islands; the citizens of these countries are all citizens of Denmark and the European Union. Greenland's capital is Nuuk. Though a part of the continent of North America, Greenland has been politically and culturally associated with Europe (specifically Norway and Denmark, the colonial powers) for more than a millennium, beginning in 986.The Fate of Greenland's Vikings , by Dale Mackenzie Brown, ''Archaeological Institute of America'', ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fram Strait
The Fram Strait is the passage between Greenland and Svalbard, located roughly between 77°N and 81°N latitudes and centered on the prime meridian. The Greenland and Norwegian Seas lie south of Fram Strait, while the Nansen Basin of the Arctic Ocean lies to the north. Fram Strait is noted for being the only deep connection between the Arctic Ocean and the World Oceans. The dominant oceanographic features of the region are the West Spitsbergen Current on the east side of the strait and the East Greenland Current on the west. Description Fram Strait is the northernmost ocean area having ice-free conditions throughout the year. The width of the strait is about 450 km, but because of the wide continental shelves of Greenland and Spitsbergen, the deep portion of Fram Strait is only about 300 km wide. The ocean over the Greenland continental shelf is often covered with ice. Within Fram Strait, the sill connecting the Arctic and Fram Strait is 2545 m deep. The Knipo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nordostrundingen C 501 Map Sheet
Nordostrundingen (corrupted from da, Nordøstrundingen which means Northeastern rounding, in English Northeast Foreland), is a headland located at the northeastern end of Greenland. Administratively it is part of the Northeast Greenland National Park. This headland was named by the Denmark expedition 1906–1908. It is an inconspicuous point where the ice slope of the Flade Isblink meets the frozen sea. Easterly point At 11°19'W it is the most easterly point of land relative to either of the Americas (North and South America). Nordøstrundingen is further east than three countries in Africa and even further east than the westernmost point in Europe (excluding the Azores), which is Látrabjarg in Iceland. It is only 1° 49′ from the westernmost point of the European mainland which is in Portugal. Greenland is not part of North America politically, which leads some people to assert that the most easterly point of the continent is the easternmost point in Canada − Cape Spear ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fast Ice
Fast ice (also called ''land-fast ice'', ''landfast ice'', and ''shore-fast ice'') is sea ice that is "fastened" to the coastline, to the sea floor along shoals or to grounded icebergs.Leppäranta, M. 2011. The Drift of Sea Ice. Berlin: Springer-Verlag. Fast ice may either grow in place from the sea water or by freezing pieces of drifting ice to the shore or other anchor sites.Kovacs, A.and M. Mellor. 1974. "Sea ice morphology and ice as a geologic agent in the Southern Beaufort Sea." pp. 113-164, in: ''The Coast and Shelf of the Beaufort Sea'', J.C. Reed and J.E. Sater (Eds.), Arlington, Va.: U.S.A. Unlike drift (or pack) ice, fast ice does not move with currents and winds. The width (and the presence) of this ice zone is usually seasonal and depends on ice thickness, topography of the sea floor and islands. It ranges from a few meters to several hundred kilometers. Seaward expansion is a function of a number of factors, notably water depth, shoreline protection, time of y ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nordostrundingen
Nordostrundingen (corrupted from da, Nordøstrundingen which means Northeastern rounding, in English Northeast Foreland), is a headland located at the northeastern end of Greenland. Administratively it is part of the Northeast Greenland National Park. This headland was named by the Denmark expedition 1906–1908. It is an inconspicuous point where the ice slope of the Flade Isblink meets the frozen sea. Easterly point At 11°19'W it is the most easterly point of land relative to either of the Americas (North and South America). Nordøstrundingen is further east than three countries in Africa and even further east than the westernmost point in Europe (excluding the Azores), which is Látrabjarg in Iceland. It is only 1° 49′ from the westernmost point of the European mainland which is in Portugal. Greenland is not part of North America politically, which leads some people to assert that the most easterly point of the continent is the easternmost point in Canada − Cape Spear ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Cap
In glaciology, an ice cap is a mass of ice that covers less than of land area (usually covering a highland area). Larger ice masses covering more than are termed ice sheets. Description Ice caps are not constrained by topographical features (i.e., they will lie over the top of mountains). By contrast, ice masses of similar size that ''are'' constrained by topographical features are known as ice fields. The ''dome'' of an ice cap is usually centred on the highest point of a massif. Ice flows away from this high point (the ice divide) towards the ice cap's periphery. Ice caps have significant effects on the geomorphology of the area that they occupy. Plastic moulding, gouging and other glacial erosional features become present upon the glacier's retreat. Many lakes, such as the Great Lakes in North America, as well as numerous valleys have been formed by glacial action over hundreds of thousands of years. On Earth, there are about of total ice mass. The average temperature ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flade Isblink
Flade Isblink is an ice cap on the Crown Prince Christian Land peninsula, King Frederick VIII Land, NE Greenland. Station Nord, the only inhabited place in the region, lies to the northwest, off the ice cap area. History The Flade Isblink was named by Lauge Koch in 1933. He was the first to map the area in the course of survey flights during the 1931–34 Three-year expedition to East Greenland.''Catalogue of place names in northern East Greenland'', Geological Survey of Denmark and Greenland Geography This large and flat ice cap is separated from the Greenland ice sheet and is the largest independent ice cap in Greenland. It is located between the Wandel Sea to the north and Amdrup Land and Antarctic Bay to the south. Romer Lake and the Princess Elizabeth Alps extend southwestwards at the western end and to the east lies the Fram Strait and the Greenland Sea. The ice cap covers most of the northern part of Crown Prince Christian Land and is about in area. The underlying bedroc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amdrup Land
Amdrup Land is a land area in the Crown Prince Christian Land peninsula, King Frederick VIII Land, northeastern Greenland. Administratively it belongs to the NE Greenland National Park area. Numerous fossils of the Carboniferous and Palaeozoic periods have been found in Amdrup Land, including fossil algae and fishes. Geography Amdrup Land is largely unglaciated. It is bound in the north by the large Flade Isblink ice cap, in the east by Antarctic Bay of the Greenland Sea and in the south by the Ingolf Fjord, on the other side of which rises Holm Land. The Henrik Krøyer Holme island group lies off its southeastern point. To the northwest rise the Princess Elizabeth Alps.Google Earth History Amdrup Land was named by the 1906-1908 Denmark expedition after Georg Carl Amdrup, a member of the expedition committee. The 1938–39 Mørkefjord expedition found numerous stone mounds which proved to be ancient Inuit meat caches at a place named Kødgravene, in the northeastern shore of Amd ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctic (ship)
''Antarctic'' was a Swedish steamship built in Drammen, Norway, in 1871. She was used on several research expeditions to the Arctic region and to Antarctica from 1898 to 1903. In 1895 the first confirmed landing on the mainland of Antarctica was made from this ship. The ship ''Antarctic'' was a barque with three masts and equipped with a steam engine, built in 1871 at Holmen in Drammen in Norway under the name ''Cap Nor''. Alfred Nathorst, ”Två Somrar i Norra Ishafvet”, first part (in Swedish), 1900, accessdate=2010-12-10 Henrik Bull, ”The cruise of the "Antarctic" to the South Polar regions”, 1896, accessdate=2010-12-10 [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peary Land
Peary Land is a peninsula in northern Greenland, extending into the Arctic Ocean. It reaches from Victoria Fjord in the west to Independence Fjord in the south and southeast, and to the Arctic Ocean in the north, with Cape Morris Jesup, the northernmost point of Greenland's mainland, and Cape Bridgman in the northeast. History Ancient settlements Peary Land was historically inhabited by three separate cultures, during which times the climate was milder than presently: *Independence I culture, Paleo-Eskimo (around 2000 BC, oldest remains dating from 2400 BC) *Independence II culture, Paleo-Eskimo (800 BC to 200 BC) *Thule culture (ancestral to the modern Inuit, around AD 1300) Peary's explorations The area is named after Robert E. Peary, who first explored it during his expedition of 1891 to 1892. Originally, Peary Land was believed to be an island, separated from the main island by the so-called Peary Channel, an assumed connection between Nordenskiöld Fjord and Independe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alfred Gabriel Nathorst
Alfred Gabriel Nathorst (7 November 1850 – 20 January 1921) was a Swedish Arctic explorer, geologist, and palaeobotanist. Life He was born in Väderbrunn in Sweden. Nathorst's interest in geology was awoken by Charles Lyell’s ‘’Principles of Geology‘’ and, at the age of 21, Nathorst visited Charles Lyell, Lyell in England in 1872. Nathorst was employed at the Geological Survey of Sweden in 1873-84. He was then appointed professor, by royal decree on the 5 December 1884, and was simultaneously made curator of the new “Department of Archegoniates and Fossil Plants" at the Swedish Museum of Natural History. He remained on the post until his retirement in 1917. Nathorst visited Spitsbergen in 1870 and participated in 1882–83 in the ''2nd Dickson Expedition'' ("Den andra Dicksonska Expeditionen till Grönland") led by Adolf Erik Nordenskiöld. He led an expedition on the ship ''Antarctic (ship), Antarctic'' to Bear Island (Norway), Bear Island and Svalbard includ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Denmark Expedition
The Denmark expedition ( da, Danmark-ekspeditionen), also known as the Denmark Expedition to Greenland's Northeast Coast, and as the Danmark Expedition after the ship, was an expedition to the northeast of Greenland in 1906–1908. Despite being overshadowed by the death in tragic circumstances of the main exploration team, including three of the expedition's leading members: Ludvig Mylius-Erichsen (1872–1907), Niels Peter Høeg Hagen (1877–1907) and Jørgen Brønlund (1877–1907), the Denmark expedition was not a failure. It achieved its main cartographic objectives and succeeded in exploring the vast region, drawing accurate charts of formerly unexplored coastlines and fjords, naming numerous geographic features, and gathering a wealth of scientific data. Purposes The two-year expedition was conceived and led by Ludvig Mylius-Erichsen, who had previously led the 'Literary Expedition' to Northwest Greenland together with Knud Rasmussen in 1902–1904. The main target of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
