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Sikuijivitteq
Sikuijivitteq ( da, Mogens Heinesen Fjord), also known as ''Kangerdlugsuatsiak'', is a fjord of the King Frederick VI Coast in the Kujalleq municipality, southeastern Greenland. The name 'Mogens Heinesen' is based on Magnus Heinason, a 16th-century Faroese naval hero. Geography Sikuijivitteq is located south of Timmiarmiut Fjord (Timmiarmiit Kangertivat); to the east it opens into the North Atlantic Ocean. Ikermiit Island is located off the fjord's mouth.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute'', p. 101 Mountains There are high mountains rising on both sides of the fjord, becoming especially craggy towards the inner side. One of the most impressive is a dark pyramidal peak in the nunatak at the head of the fjord rising steeply to a height of on the southern side above the glacier at . 6 km to the east in the same nunatak there is a steep mountain with multiple peaks rising to a height of at and at the eastern end there is a massive summit rising ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Magnus Heinason
Magnus Heinason (Mogens Heinesøn) (1548 – 18 January 1589) was a Faroe Islands, Faroese naval hero, trader and privateer. Magnus Heinason served William the Silent and his son Maurice of Nassau, Prince of Orange for 10 years as a privateer, fighting the Spanish in the Dutch Revolt. Magnus Heinason was given the trading rights to the Faroe Islands by King Frederick II of Denmark and Norway from 1559 to 1588. Later he received letters of marque to sink or capture pirate ships and England, English merchant ships. Magnus built the first fortifications in Tórshavn. Only one year later, he was captured and sent to Copenhagen on the orders of the Denmark, Danish treasurer and statholder, Christoffer Walkendorf (1525–1601) who was ruling Denmark after the sudden death of Frederick II. Magnus Heinason was tried, and was beheaded 18 January 1589. His widow, Sofie von Günsterberg, and his business partner Hans Lindenov (d. 1610) contested this act and brought the matter to an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Timmiarmiut Fjord
Timmiarmiut Fjord (old spelling 'Tingmiarmiut Fjord'; kl, Timmiarmiit Kangertivat)) is a fjord of the King Frederick VI Coast in the Sermersooq municipality, southeastern Greenland. Geography Timmiarmiut Fjord is located north of Sikuijivitteq (Mogens Heinesen Fjord); to the east it opens into the North Atlantic Ocean with Aaluik, a 220 m high island by the shore of the large Timmiarmiit island, off the northern side of its mouth. On the southern side of its mouth lies the island of Immikkoortukajik and further east at the entrance 643 m high Uttorsiutit Island. The inner part of Timmiarmiut Fjord is a fjord system with a pattern of large tributary fjords branching to the north, the main ones being the Hanseraq Fjord and the Ernineq Fjord. These fjord branches are often blocked by ice floes discharged from the active glaciers at the head, among which the Heimdal Glacier deserves mention. The Garm glacier in the north has two branches near its terminus, one flowing southwa ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kujalleq
Kujalleq ( Greenlandic: , da, Den Syden, lit=The South) is a municipality on the southern tip of Greenland, operational from 1 January 2009. The administrative center of the municipality is in Qaqortoq (formerly called Julianehåb). Creation The municipality consists of the former municipalities of southern Greenland, each named after the biggest settlement: * Nanortalik Municipality * Narsaq Municipality * Qaqortoq Municipality In addition to the area of these municipalities, uninhabited parts of the former municipalities of Paamiut and Ammassalik were added to the new administrative entity. In the case of Paamiut Municipality, it was exclusively a part of the ice sheet including a few nunataks, while in the case of Ammassalik Municipality, it included the coast from the fjord Kangerlussuatsiaq (in Danish ''Lindenow Fjord'') on the old border with Nanortalik Municipality in the south to north of Timmiarmiut. Coat of arms The coat of arms of the municipality depicts a r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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 when ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
King Frederick VI Coast
King Frederick VI Coast ( da, Kong Frederik VI Kyst) is a major geographic division of Greenland. It comprises the coastal area of Southeastern Greenland in Sermersooq and Kujalleq municipalities fronting the Irminger Sea of the North Atlantic Ocean. It is bordered by King Christian IX Land on the north and the Greenland Ice Sheet to the west. Named after King Frederick VI of Denmark-Norway, the coast stretches for about south of the Arctic Circle. It is characterized by a succession of short fjords, steep mountains and small coastal islands. There is a narrow belt of ice-free land between the shore and the Inland ice cap, interrupted by active glaciers reaching the shore with the ice limit varying seasonally from year to year. Owing to the movement of pack ice carried by the East Greenland Current and frequent gale-force winds that sweep down from the Greenland ice cap, it is mostly very difficult to approach or navigate along the coast by ship. History This area was in ... [...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 At ... [...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 when ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Faroe Islanders
Faroese people or Faroe Islanders ( fo, føroyingar; da, færinger) are a North Germanic ethnic group and nation native to the Faroe Islands. The Faroese are of mixed Norse and Gaelic origins. About 21,000 Faroese live in neighbouring countries, particularly in Denmark, Iceland and Norway. Most Faroese are citizens of the Kingdom of Denmark, in which the Faroe Islands are a constituent nation. The Faroese language is one of the North Germanic languages and is closely related to Icelandic and to western Norwegian varieties. Origins The first known settlers of the Faroe Islands were Gaelic hermits and monks who arrived in the 6th century. From the ninth century onwards the Norse-Gaels came and brought Norse culture and language to the islands. Little is known about this period, thus giving room for speculation. A single source mentions early settlement, the Icelandic Færeyinga saga. It was written sometime around 1200 and explains events taking place approximately 3 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nunatak
A nunatak (from Inuit ''nunataq'') 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 are also called glacial islands. Examples are natural pyramidal peaks. When rounded by glacial action, smaller rock promontories may be referred to as rognons. The word is of Greenlandic origin and has been used in English since the 1870s. Description The term is typically used in areas where a permanent ice sheet is present and the nunataks protrude 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 nunataks are isolated, sometimes they form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, which hampers the formation of glacial ice on their tops, although snow c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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