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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
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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"
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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
762:"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
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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 1,000 millimetres (39 in) per year recorded in some parts. The prominent peak of
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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.
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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
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The varying climate of the plateau has a marked effect on the flora, which is richer on the wetter west side than in the drier east; much of the plateau is covered by coarse
303:, covering an area of about 6,500 km (2,500 sq mi) at an average elevation of 1,100 metres (3,600 ft). The highest point on the plateau is the
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Svarstad, H; Bugge, HC; Dhillion, SS (2000). "From Norway to
Novartis: Cyclosporin from Tolypocladium inflatum in an open access bioprospecting regime".
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times. Much later, in the
Miocene epoch, the modern flatness of Hardangervidda took form as a peneplain formed at sea level. Then in
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linking
Eidfjord and Veggli in the Numedal valley with Hol and Uvdal. It is still a key transit route between
281:. Hardangervidda is a popular tourist and leisure destination, and it is ideal for many outdoor activities.
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482:) 9,000–5,000 years ago, the regional climate was warmer, and large parts of Hardangervidda were wooded;
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774:"Mountains of southernmost Norway: uplifted Miocene peneplains and re-exposed Mesozoic surfaces"
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565:, Norway's largest at 3,422 km (1,321 sq mi). The park's boundaries stretch from
822:"Lightning strike kills more than 300 reindeer in Norway", by Associated Press, via Global News
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logs can still be found preserved in bogs well above today's treeline. With the predicted
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Japsen, Peter; Green, Paul F.; Chalmers, James A.; Bonow, Johan M. (17 May 2018).
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Norwegian
Directorate for Nature, information on Hardangervidda National Park
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animals and plants further south than anywhere else in Europe. Its wild
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1,690 m (5,545 ft) is visible across much of the plateau.
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471:), found in a soil sample obtained in 1969 from Hardangervidda.
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The national park has two visitor centres on the plateau: the
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to prevent rejection was initially isolated from the fungus
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discussion on whether to leave so many corpses in the open.
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835:"Lightning Strike Kills More Than 300 Reindeer in Norway"
631:, are set in a mountain health resort in Hardangervidda.
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261:counties. It is the largest plateau of its kind in
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490:, Hardangervidda could again be largely wooded.
337:The area of Hardangervidda was once part of the
249:) in central southern Norway, covering parts of
361:times Hardangervidda and the whole of southern
692:. Oslo: Norsk ReisehĂĄndbok. 1986. p. 93.
403:The whole of the Hardangervidda is above the
375:, a characteristic mountain on Hardangervidda
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644:took place on the Hardangerjøkulen glacier.
678:. London: Macgibon & Kee. p. 206.
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941:Information about the Hardangervidda Trek
365:were uplifted more than thousand meters.
58:2001 view of the Hardangervidda landscape
833:Libell, Henrik Pryser (29 August 2016).
411:enables the presence of many species of
930:The perfect driving route to the fjords
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895:"Bjerknes Centre for Climate Research"
647:The title theme of the Norwegian film
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201:6,500 km (2,500 sq mi)
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986:Protected areas established in 1981
947:The official travel guide to Norway
928:Hardangervidda national park route
725:The Crystal Reference Encyclopedia
703:Gribble, Leonard Reginald (1980).
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781:Journal of the Geological Society
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945:Hardangervidda mountain plateau
613:The final two acts of the play
394:on a rock of the Hardangervidda
269:, and one of Norway's largest
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861:Biodiversity and Conservation
707:. London: Burke. p. 49.
557:Hardangervidda National Park
510:at Skinnarbu, near the lake
430:Norwegian Environment Agency
279:Hardangervidda National Park
217:1,721 m (5,646 ft)
209:1,100 m (3,600 ft)
322:. The bedrock is mainly of
295:The plateau is the largest
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634:Location shooting for the
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500:Hardangervidda Natursenter
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27:Mountain plateau in Norway
545:Norwegian National Road 7
518:and the mountain village
476:Holocene climatic optimum
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653:, by Norwegian composer
383:Hardangervidda landscape
873:10.1023/A:1008990919682
745:Encyclopædia Britannica
641:The Empire Strikes Back
123:Hardangervidda (Norway)
90:Location of the plateau
674:Fodor, Eugene (1964).
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464:Tolypocladium inflatum
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363:Scandinavian Mountains
339:Sub-Cambrian peneplain
214:Highest elevation
1016:Landforms of Telemark
1011:Landforms of Vestland
1006:Landforms of Buskerud
743:"Hardanger Plateau".
723:"Hardanger Plateau".
459:organ transplantation
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289:Further information:
285:Geography and geology
599:cross-country skiing
597:, and in winter for
457:drug widely used in
93:Show map of Vestland
905:on 27 February 2006
899:www.bjerknes.uib.no
801:10.1144/jgs2017-157
793:2018JGSoc.175..721J
616:When We Dead Awaken
547:cross the plateau.
502:(Nature Centre) in
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966:Plateaus of Norway
839:The New York Times
625:Når vi døde vågner
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351:Caledonian orogeny
299:(eroded plain) in
198: • Total
126:Show map of Norway
867:(11): 1521–1541.
705:On Secret Service
601:from hut to hut.
581:in the west. The
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235:Hardanger Plateau
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16:(Redirected from
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907:. Retrieved
903:the original
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443:(especially
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676:Scandinavia
541:Bergen Line
514:, the town
451:Ciclosporin
343:thrust over
324:Precambrian
305:Sandfloegga
221:Sandfloegga
158: /
981:Ullensvang
960:Categories
951:Map hiking
909:13 January
661:References
605:In culture
579:Ullensvang
575:Røvelseggi
392:Map lichen
233:(English:
844:31 August
809:134575021
512:Møsvatnet
480:Stone Age
426:lightning
405:tree line
373:HĂĄrteigen
355:Paleozoic
313:HĂĄrteigen
297:peneplain
243:Norwegian
206:Elevation
971:Eidfjord
881:27371551
650:O'Horten
591:climbing
504:Eidfjord
445:sphagnum
417:reindeer
334:origin.
332:Silurian
320:ice ages
271:glaciers
259:Buskerud
255:Telemark
251:Vestland
183:Buskerud
179:Telemark
175:Vestland
171:Location
146:007°25′E
789:Bibcode
747:. 2007.
727:. 2005.
595:fishing
567:Numedal
520:Rauland
488:warming
474:In the
437:grasses
349:of the
345:by the
239:plateau
143:60°03′N
45:Plateau
879:
807:
621:Danish
587:hiking
539:. The
537:Bergen
516:Rjukan
441:mosses
422:lichen
413:arctic
407:. Its
347:nappes
328:Cambro
301:Europe
263:Europe
257:, and
219: (
187:Norway
181:, and
996:Vinje
877:S2CID
805:S2CID
777:(PDF)
655:Kaada
627:) by
571:Uvdal
453:, an
247:vidde
1001:Tinn
911:2022
846:2016
636:Hoth
593:and
577:and
569:and
535:and
533:Oslo
508:Tinn
484:pine
326:and
193:Area
869:doi
797:doi
785:175
353:in
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