Wilcox Head
Wilcox Head is a cape in Avannaata municipality in northwestern Greenland. Geography The cape is the western promontory on Kiatassuaq Island,''Upernavik Avannarleq'', Saga Map, Tage Schjøtt, 1992 delimiting the southern end of Melville Bay, with the other end defined as Cape York, to the northwest, in northern Baffin Bay. An alternative endpoint for the bay is Nuussuup Nuua, the western promontory on Nuussuaq Peninsula Nuussuaq Peninsula (, old spelling: ''Nûgssuaq'') is a large (180x48 km) peninsula in western Greenland. Geography The waters around the peninsula are that of Baffin Bay. To the south and southwest the peninsula is bounded by Disko Bay, .... References {{Upernavik Archipelago Headlands of Greenland Inussulik Bay Melville Bay Upernavik Archipelago ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Headland
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Avannaata
Avannaata (, da, Det Nordlige, lit=The Northern) is a municipality of Greenland created on 1 January 2018 from the bulk of the former Qaasuitsup municipality. It encompasses an area of 522,700 km2 and has 10,726 inhabitants. Geography In the south, Avannaata is flanked by the Qeqertalik municipality. In the southeast, it is bordered by the Sermersooq municipality, however this border runs north–south ( 45° West meridian) through the center of the Greenland ice sheet ( kl, Sermersuaq), and as such is free of traffic. In the east and northeast it is bordered by the Northeast Greenland National Park. At the southern end of the municipal coastline are the waters of Disko Bay, although some Disko Bay communities belong to the municipality of Qeqertalik. This bay is an inlet of the larger Baffin Bay, which to the north edges into the island of Greenland in the form of Melville Bay. The coastline of northeastern Baffin Bay is dotted with islands of the Upernavik Archipe ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Kiatassuaq Island
Kiatassuaq Island (old spelling: ''Kiatagssuaq'', da, Holm Ø, Holm Island) is an uninhabited island in the northern Upernavik Archipelago in Avannaata municipality in northwestern Greenland. It marks the southern border of Melville Bay. History The name of the island means "''a large torso''" in the Greenlandic language. Initially, before the northbound migration phase of the 1920s, the island was named differently: "''Nuussuaq Ungalleq''", or ''the farther large point'', in reference to Nuussuaq Peninsula and Nuussuaq settlement some 45 kilometers to the south, with both names translating as "''large tip''". Its Danish name 'Holm Ø' ('Holm Island') had been given in honour of officer of the Danish Navy and Arctic explorer Gustav Holm (1849 – 1940). Geography Located in the southern part of Melville Bay, Kiatassuaq Island has an elongated shape, with an east–west orientation. It has an area of , with a shoreline of . Kullorsuaq is the closest settlement to Kiatassua ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Melville Bay
Melville Bay ( kl, Qimusseriarsuaq; da, Melville Bugt), is a large bay off the coast of northwestern Greenland. Located to the north of the Upernavik Archipelago, it opens to the south-west into Baffin Bay. Its Kalaallisut name, ''Qimusseriarsuaq'', means "the great dog sledding place". The bay was named after Robert Dundas, 2nd Viscount Melville, (1771 - 1851) head of the Admiralty. Geography Melville Bay is delimited by Cape York in the northeast and Wilcox Head, the western promontory on Kiatassuaq Island in the south.''Upernavik Avannarleq'', Saga Map, Tage Schjøtt, 1992 Some islands of the Upernavik Archipelago are in the Melville Bay area, such as Kiatassuaq Island, Kullorsuaq Island, Saarlia Island and Saqqarlersuaq Island. Melville Bay is free of fast ice between mid August and the end of September on average. Navigation is dangerous as there are numerous icebergs in the bay throughout the year.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute,'' p. ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cape York (Greenland)
Cape York () is a cape on the northwestern coast of Greenland, in northern Baffin Bay. Geography It is a pronounced projection. It delimits the northwestern end of Melville Bay, with the other end commonly defined as Wilcox Head, the western promontory on Kiatassuaq Island.''Upernavik Avannarleq'', Saga Map, Tage Schjøtt, 1992 De Dodes Fjord and Sidebriksfjord are north of the cape, and the Crimson Cliffs to the west. A chain of small coastal islands stretches between Cape York and Cape Melville to the east, the largest of which is Meteorite Island. The cape is west-south-west of Savissivik, the settlement on Meteorite Island. There was one nearer permanent settlement, '' Perlernerit'', approximately northeast of the cape. History The cape was the one of many places visited in 1894 by Admiral Robert Peary during his second expedition to the Arctic. A way east across the bay is the island of discovery of the Cape York Meteorite fragments. In the Greenlandic langu ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Baffin Bay
Baffin Bay (Inuktitut: ''Saknirutiak Imanga''; kl, Avannaata Imaa; french: Baie de Baffin), located between Baffin Island and the west coast of Greenland, is defined by the International Hydrographic Organization as a marginal sea of the Arctic Ocean. It is sometimes considered a sea of the North Atlantic Ocean. It is connected to the Atlantic via Davis Strait and the Labrador Sea. The narrower Nares Strait connects Baffin Bay with the Arctic Ocean. The bay is not navigable most of the year because of the ice cover and high density of floating ice and icebergs in the open areas. However, a polynya of about , known as the North Water, opens in summer on the north near Smith Sound. Most of the aquatic life of the bay is concentrated near that region. Extent The International Hydrographic Organization defines the limits of Baffin Bay as follows: History The area of the bay has been inhabited since BC. Around AD 1200, the initial Dorset settlers were rep ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Nuussuup Nuua
Nuussuup Nuua (old spelling: ''Nûgssûp Nûa'') is a cape in Avannaata municipality in northwestern Greenland. Geography The cape is the western promontory on the long Nuussuaq Peninsula, jutting from the mainland of Greenland into Baffin Bay and separating Sugar Loaf Bay in the south from Inussulik Bay in the north.''Upernavik Avannarleq'', Saga Map, Tage Schjøtt, 1992 It is located approximately west-south-west of the Nuussuaq settlement, The cape is an alternative endpoint for Melville Bay, although the common definition limits the bay to Wilcox Head Wilcox Head is a cape in Avannaata municipality in northwestern Greenland. Geography The cape is the western promontory on Kiatassuaq Island,''Upernavik Avannarleq'', Saga Map, Tage Schjøtt, 1992 delimiting the southern end of Melville Bay, ..., the western promontory on Kiatassuaq Island, at the northern end of Inussulik Bay, thus excluding the latter. The other end is defined as Cape York, to the northwest ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Nuussuaq Peninsula (Upernavik Archipelago)
Nuussuaq Peninsula (old spelling ''Nûgssuaq'' or simply ''Nugsuak'') is a mainland peninsula in northwestern Greenland, located at the northern end of Upernavik Archipelago, approximately to the south of Melville Bay.Upernavik Avannarleq, Saga Map, 1:250.000, Tage Schjøtt, 1992 It is much smaller than its namesake in western Greenland. Geography The base of the peninsula is a nunatak located at , and rising to above the Greenland ice sheet ( kl, Sermersuaq) reaching the sea level to the south and north of the nunatak. The peninsula has a southwest–northwest orientation, jutting into Baffin Bay to the southwest, separating the Nuussuup Kangia fjord in the southeast from the Inussulik Bay in the northwest. The peninsula is narrow, approximately long, and wide, narrowing to a isthmus in several places. It is very mountainous, culminating in two peaks in its central part. The mountain tops at the spine of the peninsula are partially glaciated, with the ''Sermikassaq'' ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Air Greenland
Air Greenland A/S (formerly named Grønlandsfly), also known as Greenlandair, is the flag carrier airline of Greenland, owned by the Greenlandic Government. It operates a fleet of 32 aircraft, including 1 airliner used for transatlantic and charter flights, 8 fixed-wing aircraft primarily serving the domestic network, and 18 helicopters feeding passengers from the smaller communities into the domestic airport network. Flights to heliports in the remote settlements are operated on contract with the government of Greenland. Besides running scheduled services and government-contracted flights to most villages in the country, the airline also supports remote research stations, provides charter services for tourists and Greenland's energy and mineral-resource industries and permits medivac during emergencies. Air Greenland has seven subsidiaries, an airline, hotels, tour operators, and a travel agency specialised in Greenlandic tourism. History Founded in 1960 as ''Grønlandsfly'', ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Headlands Of Greenland
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |