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Kangikitsua
Anorituup Kangerlua, also known as Anoritoq or Anortek Fjord, is a fjord in King Frederick VI Coast, southern Greenland. Geography This fjord marks the border between the Sermersooq municipality to the north and the Kujalleq municipality to the south in the eastern coast of Greenland. Anorituup Kangerlua extends in a roughly E/W direction for about 50 km between Napasorsuaq Fjord to the north and Avaqqat Kangerluat Fjord to the south. Kangikitsua is a tributary fjord branching on the southern shore within the fjord. To the east Anorituup Kangerlua opens into the North Atlantic Ocean. The Qulleq group of coastal islands lies to the northeast of the northern end of its mouth. The Akia Peninsula is at the southern end of its mouth and the Anorituup Qeqertag islet cluster at its northern end. Off the southern side of the entrance is Isortoq Bay, with Nuuk Point at its eastern end.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute'', p. 101 There are a number of l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Fjords Of Greenland
This is a list of the most important fjords of Greenland:In Northern Greenland, a large area made up entirely of fjords; therefore Peary Land above not a fjord but a fjord area.In Northeastern Greenland, a large area made up entirely of fjords; therefore is the Scoresby Sund above not a fjord but a fjord area. Fjords * Alanngorsuaq Fjord * Aleqatsiaq Fjord * Alluitsup Kangerlua (Lichtenau Fjord) * Ameralik Fjord * Amerloq Fjord * Ammassalik Fjord * Ananap Kangertiva Kiateq * Anaanap Kangertiva Oqqorseq (Depot Fjord) * Anorituup Kangerlua **Kangikitsua * Attertia * Ardencaple Fjord ** Bredefjord ** Smallefjord * Arfersiorfik Fjord * Avaqqat Kangerluat **Puiattoq **Qassialik * Bernstorff Fjord * Bessel Fjord * Bessel Fjord, NW Greenland * Bowdoin Fjord * Carlsberg Fjord (Kangerterajitta Itterterilaa) * Cass Fjord * Danmark Fjord * De Dodes Fjord * Deichmann Fjord * Dijmphna Sound ** Hekla Sound * Eqalugaarsuit Fjord * Fleming Fjord * Foulk Fjord * Frederick E. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kangikitsua
Anorituup Kangerlua, also known as Anoritoq or Anortek Fjord, is a fjord in King Frederick VI Coast, southern Greenland. Geography This fjord marks the border between the Sermersooq municipality to the north and the Kujalleq municipality to the south in the eastern coast of Greenland. Anorituup Kangerlua extends in a roughly E/W direction for about 50 km between Napasorsuaq Fjord to the north and Avaqqat Kangerluat Fjord to the south. Kangikitsua is a tributary fjord branching on the southern shore within the fjord. To the east Anorituup Kangerlua opens into the North Atlantic Ocean. The Qulleq group of coastal islands lies to the northeast of the northern end of its mouth. The Akia Peninsula is at the southern end of its mouth and the Anorituup Qeqertag islet cluster at its northern end. Off the southern side of the entrance is Isortoq Bay, with Nuuk Point at its eastern end.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute'', p. 101 There are a number of l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Atlantic Ocean
The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the "Old World" of Africa, Europe and Asia from the "New World" of the Americas in the European perception of the World. The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Europe and Africa to the east, and North and South America to the west. As one component of the interconnected World Ocean, it is connected in the north to the Arctic Ocean, to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south (other definitions describe the Atlantic as extending southward to Antarctica). The Atlantic Ocean is divided in two parts, by the Equatorial Counter Current, with the North(ern) Atlantic Ocean and the South(ern) Atlantic Ocean split at about 8°N. Scientific explorations of the Atlant ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyramidal Peak
A pyramidal peak, sometimes called a glacial horn in extreme cases, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point. Pyramidal peaks are often examples of nunataks. Formation Glaciers, typically forming in drainages on the sides of a mountain, develop bowl-shaped basins called cirques (sometimes called ‘corries’ - from Scottish Gaelic ʰəɾə(a bowl) - or s). Cirque glaciers have rotational sliding that abrades the floor of the basin more than walls and that causes the bowl shape to form. As cirques are formed by glaciation in an alpine environment, the headwall and ridges between parallel glaciers called arêtes become more steep and defined. This occurs due to freeze/thaw and mass wasting beneath the ice surface. It is widely held that a common cause for headwall steepening and extension headward is the crevasses known as bergschrund that occur between the moving ice and the he ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyramiden (Greenland)
Pyramiden is a mountain in King Frederick VI Coast, Kujalleq municipality, southern Greenland. Geography This mountain is a 1,410 m high largely unglaciated rocky pyramidal peak rising from a nunatak located above the glacier that joins the confluence at the head of Anorituup Kangerlua fjord from the east. See also * List of mountains in Greenland This is a list of mountains in Greenland. List For each mountain, the municipality in which it is located is given, along with coordinates indicating the approximate centre of the mountain (follow the link to see satellite images of the location ... * List of nunataks of Greenland References Mountains of Greenland Nunataks of Greenland Kujalleq {{Greenland-geo-stub ceb:Pyramiden (nunatak sa Greenland, Kujalleq) sv:Pyramiden (nunatak i Grönland, Kujalleq) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ultra-prominent Peak
An ultra-prominent peak, or Ultra for short, is a mountain summit with a topographic prominence of or more; it is also called a P1500. The prominence of a peak is the minimum height of climb to the summit on any route from a higher peak, or from sea level if there is no higher peak. There are approximately 1,524 such peaks on Earth. Some well-known peaks, such as the Matterhorn and Eiger, are not Ultras because they are connected to higher mountains by high cols and therefore do not achieve enough topographic prominence. The term "Ultra" originated with earth scientist Steve Fry, from his studies of the prominence of peaks in Washington in the 1980s. His original term was "ultra major mountain", referring to peaks with at least of prominence. Distribution Currently, 1,518 Ultras have been identified above sea level: 639 in Asia, 356 in North America, 209 in South America, 120 in Europe (including 12 in the Caucasus), 84 in Africa, 69 in Oceania, and 41 in Antarctica. Man ... [...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] |
Nuuk Point
Nuuk (; da, Nuuk, formerly ) is the capital and largest city of Greenland, a constituent country of the Kingdom of Denmark. Nuuk is the seat of government and the country's largest cultural and economic centre. The major cities from other countries closest to the capital are Iqaluit and St. John's in Canada and Reykjavík in Iceland. Nuuk contains a third of Greenland's population and its tallest building. Nuuk is also the seat of government for the Sermersooq municipality. In January 2021, it had a population of 18,800. The city was founded in 1728 by the Dano-Norwegian missionary Hans Egede when he relocated from the earlier Hope Colony () where he arrived in 1721. The governor Claus Paarss was part of the relocation. The new colony was placed at the Inuit settlement of Nûk and was named ''Godthaab'' ("Good Hope"). "Nuuk" is the Greenlandic word for "cape" ( da, næs) and is commonly found in Greenlandic place names. It is so named because of its position at the end of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Isortoq Bay
Isertoq (West Greenlandic: ''Isortoq'') is a settlement in the Sermersooq municipality, in southeastern Greenland. Its population was 64 in 2020. Population The population of Isertoq has decreased by nearly half relative to the 1990 levels, and by 27 percent relative to the 2000 levels,Statistics Greenland reflecting the depopulation of the nearby and . Transport During weekdays serves the village as part of government contract, with fligh ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qulleq
Qulleq, Qutdleq or Kutdlek is an uninhabited island in the King Frederick VI Coast, Sermersooq municipality in southern Greenland. Geography Qulleq is an irregularly-shaped island that lies off the southeastern coast of Greenland. It is located 5.5 km from the shore off the mouth of the Anorituup Kangerlua fjord, to the north-northeast of Cape Tordenskjold, northeast of Nuuk Point. Qulleq is the largest and southernmost island of a small offshore archipelago of four main islands, including Qipinnguak close by to the west, Takisoq to the northwest and Qeqertarsuaq to the north. The island's length is and its maximum width . History Qutsigsormiut is an important Paleo-Eskimo archaeological site on Qulleq's southern coast. It is located by a south-facing bay known as Qulleq Sound that forms a sheltered natural harbour A harbor (American English), harbour (British English; see spelling differences), or haven is a sheltered body of water where ships, boats, and barges c ... [...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] |
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