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Stauning Alps
The Stauning Alps ( da, Stauning Alper) are a large system of mountain ranges in Scoresby Land, King Christian X Land, northeastern Greenland. Administratively the Stauning Alps are part of the Northeast Greenland National Park zone. This mountainous area was named after Danish politician Thorvald Stauning (1873–1942) who had helped to finance expeditions to east Greenland planned and carried out by Danish explorers. History The Stauning Alps had been partly mapped earlier and named ''Rink Bjerge'' by Lauge Koch’s 1926–27 expeditions, being referred to as a "wild and jagged range of mountains." The range thus described obviously corresponded to the eastern end of the Stauning Alps and the adjacent Werner Range, but the name was not approved owing to the lack of detailed maps. Finally the range was thoroughly surveyed and mapped in 1932 by Koch during aerial surveys made during the 1931–34 Three-year Expedition to East Greenland. There is almost full documentation of cl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nordvestfjord
Nordvestfjord, meaning 'Northwest Fjord', ( kl, Kangertertivarmît Kangertivat) is a fjord in King Christian X Land, eastern Greenland. Administratively most of its length lies in the Northeast Greenland National Park area, at the border of Sermersooq municipality. This fjord is part of the Scoresby Sound system. The distance from the head of Nordvestfjord across Hall Bredning to the mouth of Scoresby Sound is , which makes this continuous stretch of water the longest fjord in the world. History The Nordvestfjord fjord was named by Carl Ryder during his Ryder's East Greenland Expedition, 1891–92 expedition because of its approximate northwestern direction.''Catalogue of place names in northern East Greenland''. Geological Survey of Denmark. Ryder, however, was prevented from exploring it because it was already September, new ice was forming, and a very strong wind was blowing from the interior of the fjord. Geography This long and very deep fjord is the northernmost arm of the S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
King Oscar Fjord
King Oscar Fjord ( da, Kong Oscar Fjord) is a fjord in East Greenland, marking the northern border of the Scoresby Land Peninsula. It was named by A.G. Nathorst on his 1899 expedition as ''Konung Oscars Fjord'' for Oscar II, King of Sweden from 1872 to 1907 and of Norway from 1872 until 1905. Geography King Oscar Fjord is a major fjord system in NE Greenland. The main fjord is 10–25 km wide, bounded by Traill Island and Geographical Society Island in the east. In the inner and northern end of the fjord lies Ella Island. The Davy Sound at the southeastern end connects with the Greenland Sea after extending for about 20 km in a NW/SE direction.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute'', p. 118 Lyell Land forms the western boundary and Scoresby Land with the Stauning Alps lies to the southwest. The Antarctic Sound separates the Suess Land Peninsula and Ymer Island and connects with the Kaiser Franz Joseph Fjord system to the north. Other branch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ittoqqortoormiit
Ittoqqortoormiit (East Greenlandic: ; West Greenlandic: ''Illoqqortoormiut'' ), formerly known as Scoresbysund, is a settlement in the Sermersooq municipality in eastern Greenland. Its population was 345 as of 2020 and has been described as one of the most remote settlements on earth. The former name Scoresbysund derives from the English Arctic explorer and whaler William Scoresby, who was the first European to map the area in 1822. The name "Ittoqqortoormiit" means "Big-House Dwellers" in the Eastern Greenlandic dialect. The region is known for its wildlife, including polar bears, muskoxen, and seals. Geography Ittoqqortoormiit is located on Liverpool Land, east of Hurry Inlet near the mouth of the northern shore of the Kangertittivaq fjord, which empties into the Greenland Sea. The time zone in Ittoqqortoormiit is UTC-01:00, putting it one hour behind Iceland (during summer time same as Iceland), and two hours ahead of most of Greenland's population. History Ittoqqortoo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also fea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scoresby Sound
Scoresby Sound (Danish: ''Scoresby Sund'', Greenlandic: ''Kangertittivaq'') is a large fjord system of the Greenland Sea on the eastern coast of Greenland. It has a tree-like structure, with a main body approximately Scoresby Sund Encyclopædia Britannica on-line long that branches into a system of s covering an area of about . The longest of the fjords extends 340–350 km (210-216 mi) inland from the coastline. The depth is 400–600 m (1,310-1,970 ft) in the main basin, but depths increase to up to in some fjords. It is one of the largest and longest fjord systems in the world.Archaeology, p. 7 On the northern side of the mouth of the Scoresb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nathorst Land (Greenland)
Nathorst Land is an area in King Christian X Land, Eastern Greenland. It lies in the Northeast Greenland National Park zone. The area is remote and uninhabited. Nathorst Land was named after Swedish Arctic explorer Alfred Gabriel Nathorst (1850–1921) by Lauge Koch during aerial surveys in 1932 which were part of the Three-year Expedition to East Greenland. Geography Nathorst Land is a mountainous region bounded by the F. Graae Glacier and the inner Nordvestfjord to the south, and to the north by Tærskeldal and Forsblad Fjord, beyond which lies Lyell Land. To the east it is separated from the Stauning Alps region by the Alpefjord, Prinsesse Glacier and Borgbjerg Glacier. To the west lies Charcot Land and to the northwest the Sortehest nunatak and the Greenland ice sheet.Google Earth Besides the ones bounding it, there are several glaciers in Nathorst Land, such as the Hammerskjøld Glacier, Jomfru Glacier, Violin Glacier, Toscano Glacier, Syd Glacier, Princess Glacier, Spærre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holger Danske Briller
Holger may refer to: People * Holger (given name), includes name origin, plus people with the name * Hilde Holger, stage name of dancer, choreographer and dance teacher Hilde Boman-Behram (née Hilde Sofer, 1905–2001) Fictional characters * Holger Danske, a legendary Danish hero Other uses * Holger Danske (Resistance group) * Holger Danske (opera) ''Holger Danske'' (Ogier the Dane) is the title of a 1789 Syngespil opera based on the Oberon myth, with music by F.L.Æ. Kunzen and a Danish libretto by Jens Baggesen. Synopsis The opera is set in the time of Charlemagne, and the action revo ... * 9266 Holger, a main-belt asteroid * Radio Holger {{disambig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
