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King Frederick VIII Land
King 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 North-South 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 Denmark 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 Frederik VIII Land', after King Frederik VIII of Denmark then the ruling monarch, by the 1906–08 Denmark Expedition in its maps of the region. Einar Storgaard used the name again in a 1927 map, and 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-year Expedition ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Region
In geography, regions, otherwise referred to as areas, zones, lands or territories, are portions of the Earth's surface 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. More confined or well bounded portions are called ''locations'' or ''places''. 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 feature ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Einar Storgaard
Einar is a Scandinavian given name deriving from the Old Norse name Einarr, which according to Guðbrandur Vigfússon is directly connected with the concept of the einherjar, warriors who died in battle and ascended to Valhalla in Norse mythology. Vigfússon comments that 'the name Einarr is properly = einheri" and points to a relation to the term with the Old Norse common nouns ''einarðr'' (meaning "bold") and ''einörð'' (meaning "valour").Vigfusson (1874:121). Einar as given name * Einár (rapper) (2002–2021), Swedish rapper *Einar Jan Aas (born 1955), Norwegian footballer *Einar Arnórsson (1880–1955), Icelandic politician *Einar Axelsson (1895–1971), Swedish actor *Einar Benediktsson (1864–1940), Icelandic poet and lawyer *Einar Blidberg (1906–1993), Swedish Navy vice admiral *Einar Bollason (born 1943), Icelandic former basketball player, coach and TV analyst *Einar Bragi (1921–2005), Icelandic poet *Einar Bruno Larsen (1939–2021), Norwegian footballer and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and 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“Glacier, N., Pronunciation.” Oxford English Dictionary, Oxford UP, June 2024, https://doi.org/10.1093/OED/7553486115. Accessed 25 Jan. 2025. 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 ever ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queen Louise Land
Queen Louise Land (; ) is a vast mountainous region located west of Dove Bay, King Frederik VIII Land, northeastern Greenland. Administratively it is part of the Northeast Greenland National Park zone. The highest point of Queen Louise Land is Gefiontinde, with a height of , the highest of the Gefiontinder group of peaks located at .Google Earth Geologically Queen Louise Land is made up of orthogneiss overlain by sedimentary rocks. History This remote area was named ''Dronning Louises Land'' after Queen Louise of Denmark (1851–1926), wife of King Frederik VIII of Denmark, by the ill-fated 1906–08 Denmark Expedition —the expedition that aimed to map one of the last unknown parts of Greenland. Danish Arctic explorer Alf Trolle claimed that this area had been originally named as ''Den Store Nanuták'' —The Big Nunatak. Queen Louise Land was subsequently visited by the 1912–13 Danish Expedition to Queen Louise Land led by J.P. Koch, as well as the 1952–54 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nunatak
A nunatak (from Inuit language, Inuit ) is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They often form natural pyramidal peaks. Isolated nunataks are also called glacial islands, and smaller nunataks rounded by glacial action may be referred to as rognons. The word is of Greenlandic language, Greenlandic origin and has been used in English since the 1870s. Description The term ''nunatak'' is typically used in areas where a permanent ice sheet is present and the ridge protrudes above the sheet.J. J. Zeeberg, ''Climate and Glacial History of the Novaya Zemlya Archipelago, Russian Arctic''. pp. 82–84 Nunataks present readily identifiable landmark reference points in glaciers or ice caps and are often named. While some are isolated, they can also form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, hampering the formation of glacial ice on thei ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Princess Caroline-Mathilde Alps
The Princess Caroline-Mathilde Alps () are a mountain range system in the Holm Land Peninsula, King Frederick VIII Land, northeastern Greenland. Administratively this range is part of the Northeast Greenland National Park zone. The range was named by the 1938–39 Mørkefjord Expedition after Princess Caroline-Mathilde of Denmark (1912-1995), wife of Prince Knud of Denmark (1900-1976), patron of the expedition. Geography The Princess Caroline-Mathilde Alps run from north to south across the western half of the Holm Land peninsula. The Princess Elizabeth Alps located to the north across the Ingolf Fjord display a similar structure. The range is bound to the north and northwest by the inner Ingolf Fjord, to the east by the flatter eastern part of Holm Land, to the west by the Vandre Valley ''(Vandredalen)'' and the Saefaxi River ''(Sæfaxi Elv)'', and to the south by the Marmorvigen and the inner Hekla Sound, the NW branch of the Dijmphna Sound. The range has numerous ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greenland Ice Sheet
The Greenland ice sheet is an ice sheet which forms the second largest body of ice in the world. It is an average of thick and over thick at its maximum. It is almost long in a north–south direction, with a maximum width of at a latitude of 77th parallel north, 77°N, near its northern edge. The ice sheet covers , around 80% of the surface of Greenland, or about 12% of the area of the Antarctic ice sheet. The term 'Greenland ice sheet' is often shortened to GIS or GrIS in scientific literature. Greenland has had major glaciers and ice caps for at least 18 million years, but a single ice sheet first covered most of the island some 2.6 million years ago. Since then, it has both grown and contracted significantly. The oldest known ice on Greenland is about 1 million years old. Due to anthropogenic greenhouse gas emissions, the ice sheet is now the warmest it has been in the past 1000 years, and is losing ice at the fastest rate in at least the past 12,000 years. Every summer ... [...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. It contains the northernmost ruins on earth, an archaeological site found in 2023. *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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wandel Sea
The Wandel Sea (; also known as McKinley Sea) is a body of water in the Greenland Sea, stretching from northeast of Greenland to Svalbard. It is obstructed by ice most of the year. This sea is named after Danish polar explorer and hydrographer, Vice Admiral Carl Frederick Wandel, who in the years 1895–96 explored the coastal waters of Greenland as part of the Danish Ingolf Expedition. Geography This arctic sea is located at 82nd parallel north, 82° north longitude and 21st meridian west, 21° west latitude. Seas farther north and northwest of the Wandel Sea were once frozen year-round but now may have open water in late summer, as of August 2018. The Wandel Sea stretches westward as far as Cape Morris Jesup. Further west is the Lincoln Sea. In the south, it stretches to Nordostrundingen. The Wandel Sea connects to the Greenland Sea in the south through the Fram Strait. Independence Fjord and Frederick E. Hyde Fjord are two great fjords of the far-northeast Greenland coast h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
King Christian X Land
King Christian X Land (; ) is an area of northeastern Greenland. History This area was named after King Christian X of Denmark and Iceland (). 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 Christian IX Land on the south, King Frederik VIII Land to the nor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Academy Glacier (Greenland)
Academy Glacier ( or ''Academy Brae''), is one of the major glaciers in northern Greenland. It was named in 1892 after the Academy of Natural Sciences of Drexel University, Academy of Natural Sciences in Philadelphia by Robert PearyPeary, Robert E. (Robert Edwin), 1856-1920, ''Northward over the great ice: a narrative of life and work along the shores and upon the interior ice-cap of northern Greenland in the years 1886 and 1891-1897, with a description of the little tribe of Smith Sound Eskimos, the most northerly human beings in the world, and an account of the discovery and bringing home of the Saviksue or great Cape York meteorites'',1898 during his expedition to north Greenland. This glacier forms the geographical limit between Peary Land and King Frederick VIII Land. Geography The Academy Glacier is roughly northeast–southwest oriented and has its terminus at the head of the Independence Fjord. Navy Cliff rises north of the last stretch of the fjord beyond which lies th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Independence Fjord
Independence Fjord or Independence Sound is a large fjord or sound in the eastern part of northern Greenland. It is about long and up to wide. Its mouth, opening to the Wandel Sea of the Arctic Ocean is located at . In the area around Independence Fjord there are traces of two paleo-Eskimo cultures that were named Independence I culture and Independence II culture after the fjord. Geography This fjord marks the northern boundary of King Frederick VIII Land. The Marie Sophie Glacier and the Academy Glacier have their terminus at the head of the fjord. Jørgen Brønlund Fjord is a small fjord branching northwest from the northern shore of Independence Fjord, at the western limit of Melville Land. Astrup Fjord and Hagen Fjord have their mouths on the southern coast of the fjord.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute'', p. 129 The latter is a larger fjord, with the Hagen Glacier at its head, branching closer to its mouth. Princess Thyra Islan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
