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Mallemuk Mountain
Mallemuk Mountain ( da, Mallemukfjeldet) is a mountain plateau with seaward cliffs in NE Greenland. Administratively it is part of the Northeast Greenland National Park zone. This mountain was named by the ill-fated Denmark expedition after the numerous colonies of northern fulmars breeding in the cliffs. Geography Mallemuk Mountain is located by the Dijmphna Sound in the southeastern shore of Holm Land, in the King Frederick VIII Land area of northeastern Greenland. The plateau is about in height and there are small glaciers on its sides, the Depot Glacier and the Mallemuk Glacier. Its cliffs are precipitous and rising steeply from the shore up to about .Mott T. Greene . ''Alfred Wegener: Science, Exploration, and the Theory of Continental Drift'', p. 136 For former expeditions to remote NE Greenland Mallemuk Mountain was useful as a landmark for its conspicuous cliffs. The name, however, was used inconsistently and there was a confusion with nearby Depot Fjeld at . Although t ...
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Holm Land
Holm Land ( da, Holms Land), sometimes referred to as "Hahn Land", is a peninsula in King Frederick VIII Land, northeastern Greenland. Administratively it belongs to the NE Greenland National Park area. This peninsula was named by the 1906-1908 Denmark expedition after Danish naval officer and Arctic explorer Gustav Frederik Holm.''Catalogue of place names in northern East Greenland'', Geological Survey of Denmark (GEUS) Geography Holm Land is bounded in the north by the Ingolf Fjord, on the other side of which rises Amdrup Land, and in the south the Hekla Sound and the Dijmphna Sound. To the west it is attached to the mainland and to the east lies the Greenland Sea. Hanseraq Fjord is a small fjord in the eastern coast. To the south lie Lynn Island and larger Hovgaard Island. A great part of inner Holm Land is covered by an ice cap. Eskimonæsset is the peninsula's northeasternmost point where there are archaeological remains of ancient Inuit dwellings found by the ill-fa ...
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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'', ...
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Google Earth
Google Earth is a computer program that renders a 3D computer graphics, 3D representation of Earth based primarily on satellite imagery. The program maps the Earth by superimposition, superimposing satellite images, aerial photography, and geographic information system, GIS data onto a 3D globe, allowing users to see cities and landscapes from various angles. Users can explore the globe by entering addresses and coordinates, or by using a Computer keyboard, keyboard or computer mouse, mouse. The program can also be downloaded on a smartphone or Tablet computer, tablet, using a touch screen or stylus to navigate. Users may use the program to add their own data using Keyhole Markup Language and upload them through various sources, such as forums or blogs. Google Earth is able to show various kinds of images overlaid on the surface of the earth and is also a Web Map Service client. In 2019, Google has revealed that Google Earth now covers more than 97 percent of the world, and has c ...
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Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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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 ...
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Northeast Greenland National Park
Northeast Greenland National Park ( kl, Kalaallit Nunaanni nuna eqqissisimatitaq, da, Grønlands Nationalpark) is the world's largest national park and the 10th List of largest protected areas in the world, largest protected area (the only larger protected areas all consist mostly of sea). Established in 1974 and expanded to its present size in 1988, it protects of the interior and northeastern coast of Greenland and is bigger than all but List of countries and outlying territories by total area, 29 of the world's 195 countries. It was the first List of national parks of Denmark, national park to be created in the Kingdom of Denmark and remains Greenland's only national park. It is the northernmost national park in the world. It is the second largest by area of any second level subdivision of any country in the world trailing only the Qikiqtaaluk Region, Qikiqtaaluk Region, Nunavut, Canada. Geography The park shares borders, largely laid out as Great Circle, straight lines, with ...
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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 ...
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Northern Fulmar
The northern fulmar (''Fulmarus glacialis''), fulmar, or Arctic fulmar is a highly abundant seabird found primarily in subarctic regions of the North Atlantic and North Pacific oceans. There has been one confirmed sighting in the Southern Hemisphere, with a single bird seen south of New Zealand. Fulmars come in one of two color morphs: a light one, with white head and body and gray wings and tail, and a dark one, which is uniformly gray. Though similar in appearance to gulls, fulmars are in fact members of the family Procellariidae, which include petrels and shearwaters. The northern fulmar and its sister species, the southern fulmar (), are the extant members of the genus . The fulmars are in turn a member of the order Procellariiformes, and they all share certain identifying features. First, they have nasal passages that attach to the upper bill called naricorns; however, nostrils on albatrosses are on the sides of the bill, as opposed to the rest of the order, including fulm ...
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Dijmphna Sound
The Dijmphna Sound ( da, Dijmphna Sund) is a sound in King Frederick VIII Land, Northeast Greenland. Administratively it is part of the Northeast Greenland National Park zone. History The sound was named by the 1906-1908 Denmark expedition after steamer ''Dijmphna'', on which Danish Naval officer Andreas Peter Hovgaard attempted to reach and map the area to the north of the Taymyr Peninsula in 1882–1883, but ended up stuck in the Kara Sea pack ice.''Catalogue of place names in northern East Greenland'', Geological Survey of Denmark and Greenland A polynya forms at the foot of the steep cliffs of Mallemuk Mountain so that there is sometimes open water in that area, even in the winter.Spencer Apollonio, ''Lands That Hold One Spellbound: A Story of East Greenland,'' 2008, pp. 110-116 Geography The sound is structurally a fjord forming a channel that runs roughly westwards between the southern shore of Holm Land by Mallemuk Mountain to the north and Cape H. N. Andersen, at the NE ...
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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 ...
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Depot Fjeld
Depot ( or ) may refer to: Places * Depot, Poland, a village * Depot Island, Kemp Land, Antarctica * Depot Island, Victoria Land, Antarctica * Depot Island Formation, Greenland Brands and enterprises * Maxwell Street Depot, a restaurant in Chicago, United States * Office Depot, an American office supply chain * The Home Depot, an American home improvement retail chain Computing and technology * Depot, an application in the Radio Service Software * Depot, the format for Hewlett-Packard's Software Distributor Military * Depot, or logistics center * Depot, or Main Operating Base, an overseas base for the US military * Regimental depot, the headquarters and training grounds of a regiment * Supply depot Transport * Depot, a transport hub for freight * Train depot or train shed, a place where train engines and cars are sheltered and maintained when not it use * Bus depot or bus garage, a place where buses are sheltered and maintained when not in use ** Bus station, whose name ...
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Polynya
A polynya () is an area of open water surrounded by sea ice. It is now used as a geographical term for an area of unfrozen seawater within otherwise contiguous pack ice or fast ice. It is a loanword from the Russian полынья (), which refers to a natural ice hole and was adopted in the 19th century by polar explorers to describe navigable portions of the sea. There are two main types of polynyas: coastal polynyas, which can be found year-round near the Antarctic and Arctic coasts and are mainly created by strong winds pushing the ice away from the coast, and mid-sea or open-ocean polynyas, which may be found more sporadically in the middle of ice pack in certain locations, especially around Antarctica. These locations are generally preconditioned by certain oceanic dynamics. One of the most famous mid-sea polynyas is the Weddell Polynya, also known as the Maud Rise Polynya, which occurs in the Lazarev Sea over the Maud Rise seamount. It was first spotted in September 197 ...
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