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Geography of Svalbard

Coordinates:78°00′N20°00′E/ 78.000°N 20.000°E/78.000; 20.000
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Svalbard
Map
Geography
LocationArctic Ocean
Coordinates78°00′N20°00′E/ 78.000°N 20.000°E/78.000; 20.000
Major islandsSpitsbergen,Nordaustlandet,Edgeøya
Area64,029 km2(24,722 sq mi)
Coastline3,587 km (2228.9 mi)
Highest elevation1,713 m (5620 ft)
Highest pointNewtontoppen
Administration
Norway
Largest settlementLongyearbyen(pop. 2060)
Demographics
Population2600 (2007)
Pop. density0.04/km2(0.1/sq mi)
MODISsatellite photo of Svalbard, courtesyNASA

Svalbardis anarchipelagoin theArctic Oceanroughly centered on78° north latitudeand20° east longitude.It constitutes the northernmost territory of theKingdom of Norway.The three main islands in the group consist ofSpitsbergen(the largest island),NordaustlandetandEdgeøya.There are also a number of smaller islands, such asBarents Island(Barentsøya) (1,288 km2(497 sq mi)),Kvitøya(682 km2(263 sq mi)),Prins Karls Forland(English: Prince Charles Foreland) (615 km2(237 sq mi)),Kongsøya(191 km2(74 sq mi)),Bear Island(178 km2(69 sq mi)),Svenskøya(137 km2(53 sq mi)),Wilhelm Island(120 km2(46 sq mi)) and other smaller islands orskerries(621 km2(240 sq mi)).

Climate

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There is no arable land in the island group due to heavy glaciation and the northern latitude. There are no trees native to the archipelago, but there are shrubs such ascrowberryandcloudberry.The west coast of Spitsbergen remains navigable most of the year, due to favorable winds which keep the area ice-free. Norway claims a 200nmi(370.4 km; 230.2 mi) fishery protection zone, but this is not recognized by neighboringRussia.

The climate of the Svalbard archipelago is arctic, tempered by warmNorth Atlantic Currentalong the west and northern coasts. This means cool summers and cold winters along the wild, ruggedmountainousislands. The high land of the island interiors is generally ice covered year round, with the west coast clear of ice about one half of the year. There are manyfjordsalong west and north coasts

Resources

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Svalbard has many mineral resources, andcoalwas mined extensively on the west side of Spitsbergen.[1]Ice floesoften block up the entrance toBellsund(a transit point for coal exports) on the west coast and occasionally make parts of the northeastern coast inaccessible to maritime traffic

Environmental issues

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Although many prior adverse practises are now banned, the issues surrounding past exploitation of animal resources in the Svalbard area remain a problem. With whale, seal and walrus populations are still far below than they were even two centuries ago (the average age of a Greenland whale). The population ofpolar bearsare locally recovering from the major culls of the 1960s and 1970s that came about due to the availability of snow scooters; however, the polar bear remains threatened at a global level, due to unsustainable levels of killing by humans and marinewater pollution.[2]There are a wide variety of birds in Svalbard includingpuffin,Arctic skua,kittiwakeandfulmar,[3]many of which populations are being monitored.

Physical geography

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Svalbard (DMA;comp. 1973, rev. 1982)

Lands

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The main islands of Svalbard is parted into severallands:

Fjords

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There are numerousfjordsamong the Svalbard islands; the five longest of which (measured from the head to open sea) are listed here:[4][5]

Coastlines

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Largest islands[6]
Island Area
(km2)
Area
(sq mi)
Spitsbergen 37,673 14,546
Nordaustlandet 14,443 5,576
Edgeøya 5,074 1,959
Barentsøya 1,288 497
Kvitøya 682 263
Prins Karls Forland 615 237
Kongsøya 191 74
Bjørnøya 178 69
Svenskøya 137 53
Wilhelm Island 120 46
Others 621 240

Coastlines of the Svalbard islands (listed from largest island to smallest) show the extensive variability characteristic of glacial formation:[4]

Mountains

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Although they are small when compared with the mountains of Norway, the elevation of the Svalbard island mountains accounts for much of the glacial erosion:[4]

Mountains onSpitsbergen.

Glaciers

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Stappenbird cliffatBear Island.

Rivers

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Settlements

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Ny-Ålesundin summer.

Inhabited

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No roads link the settlements on the island; transportation includesboat,airplane,helicopter,andsnowmobile.The gateway to Svalbard is Svalbard Airport, Longyearbyen.

Former

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  • Harlingen kokerij(Dutch settlement established in 1636 in Houcker Bay, abandoned sometime after 1662)
  • Kobbefjorden(also Robbe Bay or Copenhagen Bay) (Danish settlement established in 1631, abandoned in 1658)
  • Engelskbukta(English settlement established around 1615, occupied until mid-century)
  • Gravneset(English settlement established in the early 17th century, abandoned between 1624 and 1632, after which time it was appropriated by the Dutch)
  • Grumant(Grumantbyen) (Грумант) (Russian settlement, abandoned in 1961, revival ofminingoperations announced in 2003)
  • Gåshamna(Two English settlements, established sometime around 1618 and occupied until at least 1655)
  • Lægerneset(Dutch settlement appropriated by the English in 1615, occupied by the latter until the 1650s)
  • Port Louis(French settlement established in 1633, abandoned in 1637)
  • Pyramiden(Пирамида) (Russian settlement, abandoned in 1998)
  • Smeerenburg(Danish-Dutch settlement established in 1619 on the southeastern promontory ofAmsterdam Island,abandoned around 1660)
  • Ytre Norskøya(Dutch settlement possibly rivaling Smeerenburg in size; probably established by members of theZeelandchamber in the 1620s or later, and abandoned in 1670)

Line notes

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  1. ^"Svalbard Archaeology".svalbardarchaeology.org.
  2. ^C. Michael Hogan. 2008
  3. ^Walter Brian Harland, Lester M. Anderson, Daoud Manasrah, Nicholas J. Butterfield. 1997
  4. ^abcWeb publication of Statistics Norway, the official body for such data in Norway. Units provided are metric only; no unit conversions provided here.
  5. ^The percentage of Svalbard covered by glaciation varies by year; 59.8% is reported for 2005.
  6. ^"Population in the settlements. Svalbard".Statistics Norway.22 October 2009. Archived fromthe originalon 28 July 2011.Retrieved24 March2010.

References

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