Hardangervidda

Hardangervidda ( en, Hardanger Plateau) is a mountain plateau (Norwegian: ''vidde'') in central southern Norway, covering parts of Vestland, Vestfold og Telemark, and Viken counties. It is the largest plateau of its kind in Europe, with a cold year-round alpine climate, and one of Norway's largest glaciers, Hardangerjøkulen, is situated here. Much of the plateau is protected as part of Hardangervidda National Park. Hardangervidda is a popular tourist and leisure destination, and it is ideal for many outdoor activities.

Geography and geology

The plateau is the largest peneplain (eroded plain) in Europe, covering an area of about at an average elevation of . The highest point on the plateau is the Sandfloegga, which reaches a height of .

The landscape of the Hardangervidda is characterised by barren, treeless moorland interrupted by numerous pools, lakes, rivers and streams. There are significant differences between the west side, which is dominated by rocky terrain and expanses of bare rock, and the east side, which is much flatter and more heavily vegetated. The climate also varies between the two sides: it is considerably wetter on the west side than on the east, with over per year recorded in some parts."The Halne Area, Hardangervidda. Use of a High Mountain Area during 5000 Years – An Interdisciplinary Case Study", Dagfinn Moe, Svein Indrelid & Arthur Fasteland, in "The Cultural Landscape: Past, Present and Future", ed. Hilary H. Birks The prominent peak of Hårteigen is visible across much of the plateau.

Much of the Hardangervidda's geology is extremely ancient. The rolling fells of the Hardangervidda are the remnants of mountains that were worn down by the action of glaciers during the ice ages. The bedrock is mainly of Precambrian and Cambro-Silurian origin.

The area of Hardangervidda was once part of the Sub-Cambrian peneplain before it was thrust over by the nappes of the Caledonian orogeny in Paleozoic times. Much later, in the Miocene epoch, the modern flatness of Hardangervidda took form as a peneplain formed at sea level. Then in Early Pliocene times Hardangervidda and the whole of southern Scandinavian Mountains were uplifted more than thousand meters.

Flora and fauna

The whole of the Hardangervidda is above the tree line. Its alpine climate enables the presence of many species of arctic animals and plants further south than anywhere else in Europe. Its wild reindeer herds are among the largest in the world, with some 15,000 animals recorded in 1996 and about 8,000 in 2008. They migrate across the plateau during the year, moving from their winter grazing lands on the east side of the Hardangervidda, where they graze on lichen, prompting a Norwegian Environment Agencyes, mosses (especially sphagnum) and lichens.

Ciclosporin, an immunosuppressant drug widely used in organ transplantation to prevent rejection was initially isolated from the fungus ''Tolypocladium inflatum'' (''Beauveria nivea''), found in a soil sample obtained in 1969 from Hardangervidda.

In the Holocene climatic optimum (Stone Age) 9,000–5,000 years ago, the regional climate was warmer, and large parts of Hardangervidda were wooded; pine logs can still be found preserved in bogs well above today's treeline. With the predicted warming, Hardangervidda could again be largely wooded.

Visitor centres

The national park has two visitor centres on the plateau: the Hardangervidda Natursenter (Nature Centre) in Eidfjord, and the Hardangervidda Nasjonalparksenter (National Park Centre) in Tinn at Skinnarbu, near the lake Møsvatnet, the town Rjukan and the mountain village Rauland.

Human settlement

The Hardangervidda has been occupied for thousands of years; several hundred nomadic Stone Age settlements have been found in the area, most likely related to the migration of the reindeer. Ancient trails cross the plateau, linking western and eastern Norway. One example is the "Nordmannsslepa" linking Eidfjord and Veggli in the Numedal valley with Hol and Uvdal. It is still a key transit route between Oslo and Bergen. The Bergen Line and the main Norwegian National Road 7 cross the plateau.

National park

In 1981, much of the Hardangervidda was designated a national park, Norway's largest at . The park's boundaries stretch from Numedal and Uvdal in the east and Røvelseggi and Ullensvang in the west. The Norwegian Mountain Touring Association (DNT) maintains a comprehensive network of huts and paths across the plateau. It is a popular destination for hiking, climbing and fishing, and in winter for cross-country skiing from hut to hut.

In culture

Norwegian music projects Ildjarn and Nidhogg combined their talents to produce two ambient albums, one titled "Hardangervidda Part I" (2003) and the other "Hardangervidda Part II" (2003), inspired entirely by this zone.

The final two acts of the play ''When We Dead Awaken'' ( da, Når vi døde vågner) by Henrik Ibsen, are set in a mountain health resort in Hardangervidda.

Location shooting for the Hoth sequences in ''The Empire Strikes Back'' took place on the Hardangerjøkulen glacier.

The title theme of the Norwegian film '' O'Horten'', by Norwegian composer Kaada, is titled "Across the Hardanger Mountain Plateau" and features a train crossing the area.

References

External links

Hardangervidda national park route
The perfect driving route to the fjords

Norwegian Directorate for Nature, information on Hardangervidda National Park

trekkingvisions
Information about the Hardangervidda Trek

Hardangervidda mountain plateau
The official travel guide to Norway



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Plateaus of Norway
Eidfjord
Inselberg plains
Ullensvang
Protected areas established in 1981
Nore og Uvdal
Vinje
Tinn
Landforms of Viken (county)
Landforms of Vestland