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King Christian X Land
King Christian X Land ( da, Kong Christian X Land) is an area of northeastern Greenland. History This area was named after King Christian X of Denmark and Iceland (1870 – 1947), who rose to the throne in 1912. At the time of the Three-year Expedition to East Greenland it is reported that when Lauge Koch was planning to fly over the region in 1932 he said: The name 'King Christian X Land' was first used on the 1932 1:1 million scale Danish Geodesic Institute map. At that time the area was occupied by Norway and was renamed 'Erik the Red's Land' ''(Eirik Raudes Land)'' but the Permanent Court of International Justice ruled against Norway in 1933 and the country subsequently abandoned its claims. Myggbukta was a Norwegian radio and weather station that operated in the coast intermittently during the 20th century. Geography King Christian X Land stretches above the Arctic Circle between the Scoresby Sound at 70°N and the Bessel Fjord at 76°N. It is bordered by King Christi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Region
In geography, regions, otherwise referred to as zones, lands or territories, are areas that are broadly divided by physical characteristics (physical geography), human impact characteristics (human geography), and the interaction of humanity and the environment (environmental geography). Geographic regions and sub-regions are mostly described by their imprecisely defined, and sometimes transitory boundaries, except in human geography, where Jurisdiction (area), jurisdiction areas such as national borders are defined in law. Apart from the Earth, global continental regions, there are also hydrosphere, hydrospheric and atmosphere, atmospheric regions that cover the oceans, and discrete climates above the land mass, land and water mass, water masses of the planet. The land and water global regions are divided into subregions geographically bounded by large geological features that influence large-scale ecologies, such as plains and features. As a way of describing spatial areas, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
King Frederick VIII Land
King Frederick VIII Land ( da, Kong Frederik VIII Land) is a major geographic division of northeastern Greenland. It extends above the Arctic Circle from 76°N to 81°N in a N/S direction along the coast of the Greenland Sea. History This vast desolate region was still uncharted territory around 1900. It was explored by the 1906–08 Danmark Expedition, the 1909–12 Alabama Expedition and by J.P. Koch's 1912–13 Danish Expedition to Queen Louise Land, when the ruling monarch was Frederik VIII (1843 – 1912) The area between 79° and 81°30´N was first marked as 'King Frederick VIII Land', after King Frederick VIII of Denmark then the ruling monarch, by the 1906–08 Danmark Expedition in its maps of the region. Einar Storgaard used the name again in a 1927 map —he also proposed a division of the region into a northern and a southern part with a border along Nioghalvfjerd Fjord. Finally the name came into general usage only after the publication of the 1931–34 Three-ye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mestersvig
Mestersvig, also called Mesters Vig, is a military outpost located in Scoresby Land, on the southwestern shore of Davy Sound in King Christian X Land, NE Greenland. It has a 1,800 m gravel airstrip . This airport is located near the Stauning Alps mountainous area. History From 1956 to 1963, Mestersvig was a zinc and lead mine. Later Mestersvig used to be the only permanent station in the Northeast Greenland National Park but all of the 1986 population of 40 has been split up into the three newer Northeast Greenland National Park research stations (Danmarkshavn, Nord and Daneborg) except a permanent population of two people, although tourists visit the station occasionally. In September 2015, as part of the newest defence agreement to increase the enforcement of sovereignty in Greenland, Mission Mestersvig was executed. The mission was to test the responsiveness of the military of Denmark and if the equipment could handle winter weather. HDMS ''Thetis'', parts of the Guard Hus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zackenberg
Zackenberg or Zackenburg is a mountain in Wollaston Foreland, NE Greenland. Geography This dark-hued mountain is located at the southern end of the western section of the Wollaston Foreland. Zackenberg rises steeply from the shore of the Zackenberg Bay on the northern side the Young Sound ( da, Young Sund). It is a high massive mountain with a number of peaks, hence its German name 'Zackenberg', referring to its serrated top. A river flows on its northern and eastern side forming a valley between this mountain and the higher Dombjerg to the north. The Zackenberg Station Zackenberg (or ZERO - Zackenberg Ecological Research Operations), or Zackenberg Research Station, is an ecosystem research station and monitoring facility situated in the Northeast Greenland National Park in northeastern Greenland. The station i ..., a research facility, is built at the foot of the mountain. See also *List of mountain peaks of Greenland References External links *Zackenberg climatic data < ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zackenberg Station
Zackenberg (or ZERO - Zackenberg Ecological Research Operations), or Zackenberg Research Station, is an ecosystem research station and monitoring facility situated in the Northeast Greenland National Park in northeastern Greenland. The station is owned by the Greenland Self-Government and was run by the Danish Polar Center (Dansk Polarcenter) Danish Polar Center East Greenland until 2008. In 2009 the running of the Station was transferred to th Dept of Arctic Environment at th [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Daneborg Station
Daneborg (or Daneborg Station) is a station on the south coast of Wollaston Foreland peninsula of northeast Greenland, at the mouth of Young Sund emptying into Greenland Sea. Daneborg serves as the headquarters for the SIRIUS Patrol, the dog sled patrollers of the Northeast Greenland National Park, the largest national park in the world. The number of persons at the station is few and varies considerably from summer to winter. Daneborg is the most populated of stations in the park, with an over-wintering population of 12. Daneborg has an approximately long airstrip . History The previous sledge patrol headquarters, Eskimonaes ''(Eskimonæs)'', 27 km southwest of later Daneborg at Dødemandsbugten on the south coast of Clavering Ø, which had also been the location of the last Inuit settlement in Northeast Greenland (1823), was destroyed by German World War II invaders on March 23, 1943. The story of the wartime efforts of the North-East Greenland Sledge Patrol under Ib P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greenland Sea
The Greenland Sea is a body of water that borders Greenland to the west, the Svalbard archipelago to the east, Fram Strait and the Arctic Ocean to the north, and the Norwegian Sea and Iceland to the south. The Greenland Sea is often defined as part of the Arctic Ocean, sometimes as part of the Atlantic Ocean. However, definitions of the Arctic Ocean and its seas tend to be imprecise or arbitrary. In general usage the term "Arctic Ocean" would exclude the Greenland Sea. In oceanographic studies the Greenland Sea is considered part of the Nordic Seas, along with the Norwegian Sea. The Nordic Seas are the main connection between the Arctic and Atlantic oceans and, as such, could be of great significance in a possible shutdown of thermohaline circulation. In oceanography the Arctic Ocean and Nordic Seas are often referred to collectively as the "Arctic Mediterranean Sea", a marginal sea of the Atlantic. The sea has Arctic climate with regular northern winds and temperatures rarely ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaiser Franz Joseph Fjord
Kaiser Franz Joseph Fjord ( da, Kejser Franz Josef Fjord; kl, Kangerluk Kejser Franz Joseph) is a major fjord system in the NE Greenland National Park area, East Greenland. Geography The Kaiser Franz Joseph Fjord has its mouth in the Foster Bay of the Greenland Sea, between Cape Mackenzie at the eastern end of Geographical Society Island and Cape Franklin, the southern end of the mainland's Gauss Peninsula; Bontekoe Island lies in the bay off its mouth. It extends westwards for about 100 km, then at Eleonore Bay in an NNE/SSW direction for about 32 km, bending again westwards at Cape Mohn, the western end of Ymer Island, branching again with the Isfjord extending northwestwards for over 60 km. Two tributary fjords, the wide Nordfjord —with the large Waltershausen Glacier at its head and the Muskox Fjord ''(Moskusokse Fjord)'' branching eastwards— and the narrower Geologfjord —with the Nunatak Glacier, branch from the northern side of the fjord, about ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greenland Ice Sheet
The Greenland ice sheet ( da, Grønlands indlandsis, kl, Sermersuaq) is a vast body of ice covering , roughly near 80% of the surface of Greenland. It is sometimes referred to as an ice cap, or under the term ''inland ice'', or its Danish equivalent, ''indlandsis''. An acronym, GIS, is frequently used in the scientific literature. It is the second largest ice body in the world, after the Antarctic ice sheet. The ice sheet is almost long in a north–south direction, and its greatest width is at a latitude of 77°N, near its northern margin. The average thickness is about and over at its thickest point. In addition to the large ice sheet, smaller ice caps (such as Maniitsoq and Flade Isblink) as well as glaciers, cover between around the periphery. The Greenland ice sheet is adversely affected by climate change. It is more vulnerable to climate change than the Antarctic ice sheet because of its position in the Arctic, where it is subject to the regional amplification o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fjord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. 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 wh ... [...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 Land
Scoresby Land is an area of Eastern Greenland, which lies partly in Sermersooq and partly in the Northeast Greenland National Park zone. The area is uninhabited, except for Mestersvig, a military outpost. Muskoxen are found in Scoresby Land, and formerly also reindeer. Geography It is a mostly mountainous region, its northern part being made up of steep, difficult terrain, while the southern part towards Sydkap is smoother and more accessible.Hanne Tuborg Sandell, Birger Sandell. ''Archaeology and Environment in the Scoresby Sund Fjord'', p. 7 Scoresby Land is bound to the north by the King Oscar Fjord and its Segelsällskapet Fjord branch, to the south by the Scoresby Sound, Hall Bredning and the Nordvestfjord, and to the west by the Borgbjerg Glacier, the Princess Glacier, a part of Furesø and the Alpefjord, beyond which lies Nathorst Land. The Holger Danske Briller lakes are located in the region. Although formerly only the Stauning Alps and the northern part of Jam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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