Difference between revisions of "Scandinavian Peninsula" - New World Encyclopedia

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==References==
 
==References==
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*Ostergren, Robert C. and John G. Rice. 2004. ''The Europeans''. Guilford Press. ISBN 0898622727
  
 
[[Category:Geography]]
 
[[Category:Geography]]

Revision as of 03:16, 27 December 2008

Scandinavian Peninsula

The Scandinavian Peninsula is a geographic region in northern Europe, consisting principally of the mainland territories of Norway and Sweden. The name Scandinavian is derived from Scania,[1][2][3][4] a region at the southernmost extremity of the peninsula. The Scandinavian Peninsula is the largest peninsula in Europe.

The peninsula is part of a larger geographical feature, Fennoscandia, and extends from Russia and Finland in the northeast toward Denmark and Germany to the south and southwest.

Geography

Scandinavian Peninsula in relation to the larger Fennoscandia, which includes the Scandinavian Peninsula, the Kola Peninsula, Karelia and Finland.
Galdhøpiggen, the highest mountain on the Scandinavian Peninsula.

The Scandinavian Peninsula is the largest peninsula in Europe, and is occupied by the countries of Norway and Sweden. It is approximately 1,850 kilometers (1,150 miles) long and between approximately 370–805 km (230-500 mi) wide. About one quarter of the peninsula lies north of the Arctic Circle, with the northernmost point at Cape Nordkyn.

The peninsula is bordered by several bodies of water including:

  • the Baltic Sea (including the Gulf of Bothnia) to the east, with the autonomous Åland islands between Sweden and Finland, and Gotland.
  • the North Sea (including the Kattegat and Skagerrak) to the west and southwest
  • the Norwegian Sea to the west
  • the Barents Sea to the north

The Scandinavian mountain range, which runs through the peninsula, generally defines the borders between Norway, Sweden and Finland in the north, and continues into the central parts of southern Norway. The western sides of the mountains drop precipitously into the North Sea and Norwegian Sea, forming the famous fjords of Norway, while to the northeast they gradually curve towards Finland.

Galdhøpiggen is the highest mountain on the Scandinavian Peninsula, at 2,469 m (8,100 ft) above sea level. Glittertind, also known as Glittertinden, is the second highest mountain in the range, at 2,465 m above sea level, including the glacier at its peak (without the glacier, it is 2452 m). Both mountains are located within the municipality of Lom, in the Jotunheimen mountain area. Glittertind had earlier been a challenger for the title as the highest mountain in Norway, as measurements including the glacier was slightly higher than Galdhøpiggen. The glacier has, however, shrunk in recent years, and the dispute has been settled in Galdhøpiggen's favor. [5] These mountains also house the largest glacier on mainland Europe, Jostedalsbreen.

The climate across the peninsula varies from tundra (Köppen: ET) and subarctic (Dfc) in the north, with cool marine west coast climate (Cfc) in northwestern coastal areas reaching just north of Lofoten, to humid continental (Dfb) in the central portion, and to marine west coast (Cfb) in the south and southwest.[6]

The region is rich in timber, iron and copper with the best farmland in southern Sweden. Large petroleum and natural gas deposits have been found off Norway's coast in the North Sea and the Atlantic Ocean.

Geology

With a landscape largely shaped by glaciers over the last ice age, the Scandinavian Peninsula is as picturesque in the winter as it is cold. Image courtesy of MODIS Rapid Response Project at NASA/GSFC.

The Scandinavian Peninsula occupies part of the Baltic Shield, a stable and large crust segment formed of very old, crystalline metamorphic rocks. Most of the soil covering this substrate was scraped by glaciers during continental glaciation, especially in the northern part, where the shield is nearest the surface. As a consequence of this scouring, elevation, and climate, only a very small percentage of land is arable (3 percent in Norway).[7]

Although the Baltic Shield is largely stable and resistant to the influences of other neighboring tectonic formations, the weight of nearly four kilometers of ice sheet caused the terrain to sink. When the ice sheet disappeared, the shield rose again, a tendency that continues to this day at a rate of about 1 meter per century.[8] Conversely, the south part has tended to sink down to compensate, causing the flooding of the Low Countries and Denmark.

Extremely heavy, thick glaciers that formed during the last ice age, deepening river valleys, which were invaded by the sea when the ice melted. The glaciers ran off the mountains and scoured troughs into Norway’s coastline with depths that reached well below sea level. When the glaciers melted, the seawater rushed into these deep troughs to form the famous fjords which line the peninsula's west side, along Norway’s coast. In the south the glaciers deposited many sedimental deposits, configuring a very chaotic landscape. Many of these fjords are well over 2,000 feet (610 meters) deep. The deepest fjord on Norway’s coast, known as Sogn Fjord, lies in southwest Norway and is 4,291 feet (1,308 m) deep.

Glaciers also carved the mountains in Norway and northernmost Sweden. South of this mountainous region, however, Sweden consists mostly of flat, heavily forested land dotted with lakes. Lake Vänern and Lake Vättern, the largest of the country’s lakes, do not freeze completely during the winter months and can be seen clearly at the bottom of the peninsula. Lake Vättern, the smaller of the two lakes, was connected to the Baltic Sea during the last ice age. After the ice melted, a tremendous weight was lifted off of the peninsula, and the landmass rose up to separate the lake from the Baltic Sea. To the northeast of the peninsula lies Finland with more than 55,000 lakes, most of which were also created by glacial deposits.

The crystalline substrate and absence of soil exposes mineral deposits of metals, such as iron, copper, nickel, zinc, silver and gold.

People

The first recorded human presence in the southern area of the peninsula and Denmark dates from 12,000 years ago.[9] As the ice sheets from the glaciation retreated, the climate allowed a tundra biome that attracted reindeer hunters. The climate warmed gradually up, favoring the growth of perennial trees first, and then deciduous forest which brought animals like aurochs. Groups of hunters-fishers-gatherers started to inhabit the area since the Mesolithic (8200 B.C.E.), up to the advent of agriculture in the Neolithic (3200 B.C.E.).

The northern and central part of the peninsula is partially inhabited by the Sami, often referred to as "Lapps" or "Laplanders". In the earliest recorded periods they occupied the arctic and subarctic regions as well as the central part of the peninsula as far south as Dalarna, Sweden. They speak the Sami language, a non-Indo-European language of the Finno-Ugric family, which is related to Finnish and Estonian. The other inhabitants of the peninsula, according to ninth century records, were the Norwegians on the west coast of Norway, the Danes in what is now southern and western Sweden and southeastern Norway, the Svear in the region around Mälaren as well as a large portion of the present day eastern seacoast of Sweden and the Geats in Västergötland and Östergötland. These peoples spoke closely related dialects of an Indo-European language, Old Norse. Although political boundaries have shifted, these peoples still are the dominant populations in the peninsula in the early 21st century.[10]

Much of the population is concentrated in the southern part of the peninsula; Stockholm and Gothenburg, both in Sweden, and Oslo in Norway are the largest cities.[11]

Political development

The Scandinavian Peninsula political borders in 1888.

Although the Nordic countries look back on more than 1000 years of history as distinct political entities, the international boundaries came late and emerged gradually. It was not until the middle of 17th century that Sweden secured an outlet on the Kattegat and control of the south Baltic coast. The Swedish and Norwegian boundaries were finally agreed to and marked out in 1751. The Finnish and Norwegian border on the peninsula was established after extensive negotiation in 1809, and the common Norwegian-Russian districts were not partitioned until 1826. Even then the borders were still fluid, with Finland gaining access to the Barents Sea in 1920, but ceding this territory to Russia in 1944.[12]

Denmark, Sweden and Russia dominated political relations within the Scandinavian Peninsula for centuries, with Iceland, Finland and Norway only gaining full independence in the 20th century.


Scandinavia and the Baltic region.


Notes

  1. ↑ Haugen, Einar (1976). The Scandinavian Languages: An Introduction to Their History. Cambridge, Mass: Harvard University Press, 1976.
  2. ↑ Helle, Knut (2003). "Introduction". The Cambridge History of Scandinavia. Ed. E. I. Kouri et al. Cambridge University Press, 2003. ISBN 0-521-47299-7. p. XXII. "The name Scandinavia was used by classical authors in the first centuries of the Christian era to identify Skåne and the mainland further north which they believed to be an island."
  3. ↑ Olwig, Kenneth R. "Introduction: The Nature of Cultural Heritage, and the Culture of Natural Heritage—Northern Perspectives on a Contested Patrimony". International Journal of Heritage Studies, Vol. 11, No. 1, March 2005, p. 3: The very name 'Scandinavia' is of cultural origin, since it derives from the Scanians or Scandians (the Latinised spelling of Skåninger), a people who long ago lent their name to all of Scandinavia, perhaps because they lived centrally, at the southern tip of the peninsula."
  4. ↑ Østergård, Uffe (1997). "The Geopolitics of Nordic Identity – From Composite States to Nation States". The Cultural Construction of Norden. Øystein Sørensen and Bo Stråth (eds.), Oslo: Scandinavian University Press 1997, 25-71.
  5. ↑ Etojm.com. GLITTERTIND - 2464 METER Retrieved December 27, 2008.
  6. ↑ Troy M. Kimmel, Jr. Köppens classification University of Texas. Retrieved December 27, 2008.
  7. ↑ Joseph J. Hobbs and Christopher L. Salter. 2005. Essentials Of World Regional Geography. p. 108.Thomson Brooks/Cole. ISBN 0534466001
  8. ↑ Cite error: Invalid <ref> tag; no text was provided for refs named Ostergren
  9. ↑ Tilley, Christopher Y. Ethnography of the Neolithic: Early Prehistoric Societies in Southern Scandinavia, p. 9, Cambridge University Press. 2003. ISBN 0-521-56821-8
  10. ↑ Sawyer, Bridget and Peter (1993). Medieval Scandinavia: from conversion to Reformation, circa 800-1500. ISBN 0816617384. 
  11. ↑ Scandinavia. FactMonster.com. Retrieved 2004-03-21.
  12. ↑ Sømme, Axel (Ed.) (1961). The Geography of Norden. Oslo: Den Norske nasjonalkommittee for geographi. ISBN none. 

References
ISBN links support NWE through referral fees

  • Ostergren, Robert C. and John G. Rice. 2004. The Europeans. Guilford Press. ISBN 0898622727

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