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Map of Svalbard with Spitsbergen in the west emphasised
|Area||39,044 km2 (15,075 sq mi)|
|Highest elevation||1,717 m (5,633 ft)|
|Population||2,642 (as of 2012)|
Map of Svalbard with Spitsbergen in the west emphasised
|Area||39,044 km2 (15,075 sq mi)|
|Highest elevation||1,717 m (5,633 ft)|
|Population||2,642 (as of 2012)|
Spitsbergen (formerly known as West Spitsbergen; Norwegian: Vest Spitsbergen or Vestspitsbergen) is the largest and only permanently populated island of the Svalbard archipelago in Norway. Constituting the westernmost bulk of the archipelago, it borders the Arctic Ocean, the Norwegian Sea, and the Greenland Sea. Spitsbergen covers an area of 39,044 km2 (15,075 sq mi), making it the largest island in Norway and the 36th-largest in the world. The administrative centre is Longyearbyen. Other settlements, in addition to research outposts, are the Russian mining community of Barentsburg, the research community of Ny-Ålesund, and the mining outpost of Sveagruva.
The island was first used as a whaling base in the 17th and 18th centuries, after which it was abandoned. Coal mining started at the end of the 19th century and several permanent communities were established. The Svalbard Treaty of 1920 recognized Norwegian sovereignty and established Svalbard as a free economic zone and a demilitarized zone.
The Norwegian Store Norske and the Russian Arktikugol remain the only mining companies. Research and tourism have become important supplementary industries, featuring among others the University Centre in Svalbard and the Svalbard Global Seed Vault. No roads connect the settlements; instead snowmobiles, aircraft, and boats serve as local transport. Svalbard Airport, Longyear provides the main point of entry and exit.
The island has an Arctic climate, although with significantly higher temperatures than other places at the same latitude. The flora benefits from the long period of midnight sun, which compensates for the polar night. Svalbard is a breeding ground for many seabirds, and also supports polar bears, reindeer and marine mammals. Six national parks protect the largely untouched, yet fragile environment. The island has many glaciers, mountains and fjords.
Spitsbergen was named by its discoverer Willem Barentsz in 1596. The name Spitsbergen, meaning “pointed mountains” (from the Dutch spits - pointed, bergen - mountains), was at first applied to both the main island and the archipelago as a whole. In the seventeenth and eighteenth centuries, the islands were known as "Greenland" to the English whalers, a practice still followed in 1780 and criticized by Bacstrom at that time. The "Spitzbergen" spelling was used in English during the 19th century, for instance by Beechey, Laing, and the Royal Society.
In 1906, the Arctic explorer Sir Martin Conway thought that the Spitzbergen spelling was incorrect, preferring Spitsbergen, though this had little effect on British practice. In 1920 the treaty, determining the fate of the islands, was entitled the "Spitsbergen Treaty." The islands were generally referred to in the USA as Spitsbergen from that time, although the spelling Spitzbergen was also commonly used through the 20th century. Under Norwegian governance, the archipelago was named Svalbard in 1925, the main island becoming Spitsbergen. By the end of the 20th century, this usage had become general.
The first confirmed and recorded sighting of the island by a European was by Willem Barentsz, who came across it while searching for the Northern Sea Route in June 1596. The first good map with the east coast roughly indicated, appeared in 1623, printed by Willem Janszoon Blaeu. Around 1660 and 1728, better maps were produced.
The archipelago may have been known to Russian Pomor hunters as early as the 14th or 15th century, although solid evidence from before the 17th century is lacking. Following the English whalers and others in referring to the archipelago as Greenland, they named it Grumant (Грумант). The name Svalbard is first mentioned in Icelandic sagas of the 10th and 11th centuries, but they more likely referred to Jan Mayen or even Greenland.
Early whaling expeditions to Svalbard in general and Spitsbergen in particular tended, because of currents and fauna, to cluster around the western coast of Spitsbergen and the islands off-shore. Shortly after whaling began (1611), the Danish crown in 1616 claimed ownership of Jan Mayen and the Spitsbergen islands, as all of Svalbard was then known.
But in 1613, the English Muscovy Company had done the same. The primary and most profitable whaling grounds of this joint-stock company came to be centered around Spitsbergen in the early 17th century, and the company's 1613 Royal Charter from the English Crown granted a monopoly on whaling in Spitsbergen, based on the (erroneous) claim that Hugh Willoughby had discovered the land in 1553. Not only had they wrongly assumed a 1553 English voyage had reached the area, but on 27 June 1607, during his first voyage in search of a "northeast passage" on behalf of the company, Henry Hudson sighted "Newland" (i.e. Spitsbergen), near the mouth of the great bay Hudson later simply named the Great Indraught (Isfjorden). In this way the English hoped to head off expansion in the region by the Dutch, at the time their major rival. Initially the English tried to drive away competitors; but after disputes with the Dutch (1613–24), they, for the most part, only claimed the bays south of Kongsfjorden.
From 1617 onwards, a Danish-chartered company began sending whaling fleets to Spitsbergen. This successful expansion by Copenhagen into the North Atlantic has recently been cited by historians as the first step of the Danish-Norwegian state into overseas colonialism. It eventually built a small 17th-century empire of East Indian trade posts, North Atlantic possessions (such as Greenland and Iceland), and a small Atlantic trade route between possessions on the Guinea Coast (in modern Ghana) and what are now the US Virgin Islands.
The entire Svalbard archipelago, nominally ruled first by Denmark–Norway, and later the Norwegians (as Union between Sweden and Norway from 1814 to 1905, independent Norway from 1905), remained a source of riches for fishery and whaling vessels from many nations. The islands also became the launching point for a number of Arctic explorers, including William Edward Parry, Adolf Erik Nordenskiöld, Otto Martin Torell, Alfred Gabriel Nathorst, Roald Amundsen and Ernest Shackleton.
Between 1913 and 1920, Spitsbergen was a neutral condominium. The Spitsbergen Treaty of 9 February 1920, recognises the full and absolute sovereignty of Norway over all the arctic archipelago of Svalbard. The exercise of sovereignty is, however, subject to certain stipulations, and not all Norwegian law applies. Originally limited to nine signatory nations, over 40 are now signatories of the treaty. Citizens of any of the signatory countries may settle in the archipelago. Currently, only Norway and Russia make use of this right.
Once named Spitsbergen for its largest island, the Svalbard was made a part of Norway—not a dependency—by the Svalbard Act of 1925. Since this date it has been a portion of Norway, with a Norwegian-appointed Governor resident at the capitol of Longyearbyen. Limitations on the imposition of certain Norwegian laws are outlined in the Spitsbergen Treaty.
The largest settlement on Spitsbergen is the Norwegian town of Longyearbyen, while the second-largest settlement is the Russian coal mining settlement of Barentsburg. (This was sold by the Netherlands in 1932 to the Soviet company Arktikugol). Other settlements on the island include the former Russian mining communities of Grumantbyen and Pyramiden (abandoned in 1961 and 1998, respectively); a Polish research station at Hornsund; and the remote northern settlement of Ny-Ålesund.
Allied soldiers were stationed on the island in 1941 to prevent Nazi Germany from occupying the islands. Norway fell under German occupation in 1940. The majority of inhabitants on the island were Russian, and the Soviet Union had a non-aggression pact with Germany until 22 June 1941. The United Kingdom and Canada sent military forces to the island to destroy installations, mainly Soviet coal mines, and prevent the Germans from occupying it.
In 1943, the German battleship Tirpitz and an escort flotilla shelled and destroyed the Allied weather station there in Operation Zitronella in 1943. On 6 September, a squadron consisting of Tirpitz, the battleship Scharnhorst and nine destroyers weighed anchor in Altenfjord and Kåfjord and headed for Spitsbergen, to attack the Allied base. At dawn on 8 September 1943, Tirpitz and Scharnhorst opened fire against the two 3-inch guns which comprised the defences of Barentsburg, and the destroyers ran inshore with landing parties, destroying a supply dump and wrecking a landing station. By noon, the hostilities had ended, with the landing parties returning to the ships, along with some prisoners. The German ships returned safely to Altenfjord and Kåfjord on 9 September 1943. This was to be the last operation for the Tirpitz.
The Svalbard Treaty of 1920 established full Norwegian sovereignty over Svalbard. All current 40 signatory countries of the treaty have the right to conduct commercial activities on the archipelago without discrimination, although all activity is subject to Norwegian legislation. The treaty limits Norway's right to collect taxes to that of financing services on Svalbard. Spitsbergen is a demilitarized zone, as the treaty prohibits the establishment of military installations. The treaty requires Norway to protect the natural environment. The island is administered by the Governor of Svalbard, who holds the responsibility as both county governor and chief of police, as well as authority granted from the executive branch. Although Norway is part of the European Economic Area (EEA) and the Schengen Agreement, Svalbard is not part of the Schengen Area nor EEA.
Residents of Spitsbergen do not need visas for Schengen, but are prohibited from reaching Svalbard from mainland Norway without such. People without a means to income can be rejected as residents by the governor. Citizens of any treaty signatory country may visit the island without a visa. Russia retains a consulate in Barentsburg.
In 2009, Spitsbergen had a population of 2,753, of which 423 were Russian and Ukrainian, 10 were Polish and 322 were non-Norwegians living in Norwegian settlements. The largest non-Norwegian groups in Longyearbyen in 2005 were from Thailand, Sweden, Denmark, Russia and Germany. Spitsbergen is among the safest places on Earth, with virtually no crime.
Longyearbyen is the largest settlement on the island, the seat of the governor, and the only incorporated town. It features a hospital, primary and secondary school, university, sports centre with a swimming pool, library, cultural centre, cinema, bus transport, hotels, a bank, and several museums. The newspaper Svalbardposten is published weekly. Only a small fraction of the mining activity remains at Longyearbyen; instead, workers commute to Sveagruva (or Svea) where Store Norske operates a mine. Sveagruva is a dorm town, with workers commuting from Longyearbyen on a weekly basis.
Since 2002, Longyearbyen Community Council has had many of the same responsibilities of a municipality, including utilities, education, cultural facilities, fire department, roads and ports. No care or nursing services are available, nor is welfare payment available. Norwegian residents retain pension and medical rights through their mainland municipalities. The hospital is part of University Hospital of North Norway, while the airport is operated by state-owned Avinor. Ny-Ålesund and Barentsburg remain company towns with all infrastructure owned by Kings Bay and Arktikugol, respectively. Other public offices with presence on Svalbard are the Norwegian Directorate of Mining, the Norwegian Polar Institute, the Norwegian Tax Administration and the Church of Norway. Svalbard is subordinate Nord-Troms District Court and Hålogaland Court of Appeal, both located in Tromsø.
Ny-Ålesund is a permanent settlement based entirely around research. Formerly a mining town, it is still a company town operated by the Norwegian state-owned Kings Bay. While there is some tourism at the village, Norwegian authorities limit the access to the outpost to minimise impact on the scientific work. Ny-Ålesund has a winter population of 35 and a summer population of 180. Poland operates the Polish Polar Station at Hornsund, with ten permanent residents.
Barentsburg is the only remaining Russian settlement, after Pyramiden was abandoned in 1998. A company town, all facilities are owned by Arktikugol, who operate a coal mine, although operation has been halted since 2006. In addition to the mining facilities, Arktikugol has opened a hotel and souvenir shop, catering to tourists taking day trips or hikes from Longyearbyen. The village has facilities such as a school, library, sports center, community center, swimming pool, farm and greenhouse. Pyramiden has similar facilities; both are built in typical Soviet style and are the site of the world's two most northerly Lenin statues and other socialist realism artwork.
The three main industries on Spitsbergen are coal mining, tourism and research. In 2007, there were 484 people working in the mining sector, 211 people working in the tourism sector and 111 people working in the education sector. The same year, mining produced a revenue of NOK 2,008 million, tourism NOK 317 million and research NOK 142 million. In 2006, the average income for economically active people was NOK 494,700—23% higher than on the mainland. Almost all housing is owned by the various employers and institutions and rented to their employees; there are only a few privately owned houses, most of which are recreational cabins. Because of this, it is almost impossible to live on Spitsbergen without working for an established institution.
Since the resettlement of Spitsbergen in the early 20th century, coal mining has been the dominant commercial activity. Store Norske Spitsbergen Kulkompani, a subsidiary of the Norwegian Ministry of Trade and Industry, operates Svea Nord in Sveagruva and Mine 7 in Longyearbyen. The former produced 3.4 million tonnes in 2008, while the latter sends 35% of its output to Longyearbyen Power Station. Since 2007, there has not been any significant mining by the Russian state-owned Arktikugol in Barentsburg. There has previously been some test drilling for petroleum on land, but this did not give results good enough to justify permanent operation. The Norwegian authorities do not allow offshore petroleum drilling activities for environmental reasons, and the land formerly test-drilled on has been protected as nature reserves or national parks.
Spitsbergen has historically been a base for both whaling and fishing. Norway claimed a 200 nautical miles (370 km; 230 mi) exclusive economic zone (EEZ) around Svalbard in 1977, Norway retains a restrictive fisheries policy in the zone, and the claims are disputed by Russia. Tourism is focused on the environment and is centered around Longyearbyen. Activities include hiking, kayaking, walks through glacier caves and snow-scooter and dog-sled safaris. Cruise ships generate a significant portion of the traffic, including stops by both offshore vessels and expeditionary cruises starting and ending in Svalbard. Traffic is strongly concentrated between March and August; overnight stays have quintupled from 1991 to 2008, when there were 93,000 guest-nights.
Research on Svalbard centers around Longyearbyen and Ny-Ålesund, the most accessible areas in the high Arctic. Norway grants permission for any nation to conduct research on Svalbard, resulting in the Polish Polar Station, Indian Himadri Station, and the Chinese Arctic Yellow River Station, plus Russian facilities in Barentsburg. The University Centre in Svalbard in Longyearbyen offers undergraduate, graduate and postgraduate courses to 350 students in various arctic sciences, particularly biology, geology and geophysics. Courses are provided to supplement studies at the mainland universities; there are no tuition fees and courses are held in English, with Norwegian and international students equally represented. The Svalbard Global Seed Vault is a "doomsday" seedbank to store seeds from as many of the world's crop varieties and their botanical wild relatives as possible. A cooperation between the government of Norway and the Global Crop Diversity Trust, the vault is cut into rock near Longyearbyen, keeping it at a natural −6 °C (21 °F) and refrigerating the seeds to −18 °C (0 °F). The Svalbard Undersea Cable System is a 1,440 km (890 mi) fibre optic line from Svalbard to Harstad, needed for communicating with polar orbiting satellite through Svalbard Satellite Station and installations in Ny-Ålesund.
Within Longyearbyen, Barentsburg and Ny-Ålesund, there are road systems, but they do not connect with each other. Off-road motorized transport is prohibited on bare ground, but snowmobiles are used extensively during winter—both for commercial and recreational activities. Transport from Longyearbyen to Barentsburg (45 km or 28 mi) and Pyramiden (100 km or 62 mi) is possible by snowmobile during winter, or by ship all year round. All settlements have ports and Longyearbyen has a bus system.
Svalbard Airport, Longyear, located 3 kilometres (2 mi) from Longyearbyen, is the only airport offering air transport off and onto the island. Scandinavian Airlines has daily scheduled services to Tromsø and Oslo; there are also irregular charter services to Russia. Lufttransport provides regular corporate charter services from Longyearbyen to Ny-Ålesund Airport and Svea Airport for Kings Bay and Store Norske; these flights are in general not available to the public. There are heliports in Barentsburg and Pyramiden, and helicopters are frequently used by the governor and to a lesser extent the mining company Arktikugol.
The climate of Svalbard is dominated by its high latitude, with the average summer temperature at 4 °C (39 °F) to 6 °C (43 °F) and January averages at −12 °C (10 °F) to −16 °C (3 °F). The North Atlantic Current moderates Spitsbergens's temperatures, particularly during winter, giving it up to 20 °C (36 °F) higher winter temperature than similar latitudes in Russia and Canada. This keeps the surrounding waters open and navigable most of the year. The interior fjord areas and valleys, sheltered by the mountains, have less temperature differences than the coast, giving about 2 °C (4 °F) lower summer temperatures and 3 °C (5 °F) higher winter temperatures. On the south of Spitsbergen, the temperature is slightly higher than further north and west. During winter, the temperature difference between south and north is typically 5 °C (9 °F), while about 3 °C (5 °F) in summer.
Spitsbergen is the meeting place for cold polar air from the north and mild, wet sea air from the south, creating low pressure and changing weather and fast winds, particularly in winter; in January, a strong breeze is registered 17% of the time at Isfjord Radio, but only 1% of the time in July. In summer, particularly away from land, fog is common, with visibility under 1 kilometre (0.62 mi) registered 20% of the time in July. Precipitation is frequent, but falls in small quantities, typically less than 400 millimetres (16 in) in western Spitsbergen. More rain falls in the uninhabited east side, where there can be more than 1,000 millimetres (39 in).
The Dicksonland peninsula (78°27’23.71” – 78°40’N and 15°7’57.07”E – 16°2’20.12”E) is located in the centre of West-Spitsbergen between the NNE branches of Isfjorden c. 1260 km away from the North Pole. The current glaciation consists of plateau-glaciers with outlet tongues. In the year 1976 the glacier snowline (ELA) has run at c. 500 m asl. Its orographic variations are dependent on the wind-exposition. During the Late Glacial glacier advance Dicksonland was situated on the peripheries of two local glaciation centers. At that time a superior inland glaciation of West-Spitsbergen can be ruled out. With regard to the formation of a V-shaped valley system by subglacial meltwater erosion the culmination of the Late Glacial glaciation has to be dated to the time before c. 17 500 (+/-2000-1375) years. Here a correlation of Post Glacial glacier ends and radiocarbon (14C)-dated marine terraces  is possible. Considering isostatic movement and the difference between calculated and real snowlines, a postglacial stage at about 10 400 years ago has been reconstructed with a snowline at c. 270 m asl above the former sea level. Stagnation at c. 9650 years ago coincides with a snowline at c. 320 above the former sea level. The historical glacier fluctuation around the year 1890 has taken place at a glacier snowline at c. 420 m asl what corresponds with a snowline-depression of c. 60 altitudinal meters compared with 1976. The development of still currently existing, strong periglacial surface forms with patterned grounds has to be led back to the warm interglacial period before 7000 to 2000 years. Cause of this was the strong freezing and thawing of the bottom due to deeply thawed permafrost. Patterned grounds like these become smaller and smaller with the increasing absolute altitude, because the sorting depth in the frost debris is getting smaller.
In addition to humans, four primarily terrestrial mammalian species inhabit the island: the Arctic Fox, the Svalbard reindeer, polar bears, and accidentally introduced Southern Vole, which are only found in Grumant. Attempts to introduce the Arctic Hare and the muskox have both failed. There are fifteen to twenty types of marine mammals, including whales, dolphins, seals and walruses.
Polar bears are the iconic symbol of Spitsbergen, and one of the main tourist attractions. While they are protected, persons going outside settlements is required to carry a rifle to kill polar bears in self-defence, as a last resort should they attack. Spitsbergen shares a common polar bear population with the rest of Svalbard and Franz Joseph Land. The Svalbard reindeer (R. tarandus platyrhynchus) is a distinct sub-species. While it was previously almost extinct, hunting is permitted for both it and the Arctic Fox. There are a limited number of domesticated animals in Russian settlements.
About thirty types of bird are found on Spitsbergen, most of which are migratory. The Barents Sea is among the areas in the world with most seabirds, with about 20 million counted during late summer. The most common are Little Auk, Northern Fulmar, Thick-billed Murre and Black-legged Kittiwake. Sixteen species are on the IUCN Red List. Particularly Storfjorden and Nordvest-Spitsbergen are important breeding ground for seabirds. The Arctic Tern has the furthest migration, all the way to Antarctica. Only two songbirds migrate to Spitsbergen to breed: the Snow Bunting and the Wheatear. Rock Ptarmigan is the only bird to overwinter.
Svalbard has permafrost and tundra, with both low, middle and high Arctic vegetation. 165 species of plants have been found on the archipelago. Only those areas which defrost in the summer have vegetation. Vegetation is most abundant in Nordenskiöld Land, around Isfjorden and where effected by guano. While there is little precipitation, giving the island a steppe climate, plants still have good access to water because the cold climate reduces evaporation. The growing season is very short, and may last only a few weeks.
There are six national parks on Spitsbergen: Indre Wijdefjorden, Nordenskiöld Land, Nordre Isfjorden Land, Nordvest-Spitsbergen, Sassen-Bünsow Land and Sør-Spitsbergen. The island also features Festningen Geotope Protected Area; some of the northeastern coast is part of Nordaust-Svalbard Nature Reserve. All human traces dating from before 1946 are automatically protected. Svalbard is on Norway's tentative list for nomination as a UNESCO World Heritage Site.
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