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Hardangervidda

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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 311:
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
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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. 640: 424:, to their breeding grounds in the more fertile west of the plateau. On 26 August 2016, 323 were killed by 990: 463: 362: 338: 482:) 9,000–5,000 years ago, the regional climate was warmer, and large parts of Hardangervidda were wooded; 458: 788: 598: 342: 980: 615: 274: 902: 876: 804: 350: 242: 774:"Mountains of southernmost Norway: uplifted Miocene peneplains and re-exposed Mesozoic surfaces" 574: 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 970: 454: 868: 796: 657:, is titled "Across the Hardanger Mountain Plateau" and features a train crossing the area. 620: 486:
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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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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In 1981, much of the Hardangervidda was designated a
261:counties. It is the largest plateau of its kind in 213: 205: 197: 192: 170: 32: 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 8: 644:took place on the Hardangerjøkulen glacier. 678:. London: Macgibon & Kee. p. 206. 29: 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 758: 756: 754: 666: 204: 191: 169: 62: 50: 895:"Bjerknes Centre for Climate Research" 647:The title theme of the Norwegian film 583:Norwegian Mountain Touring Association 110: 77: 718: 716: 714: 212: 201:6,500 km (2,500 sq mi) 196: 7: 738: 736: 734: 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). 25: 781:Journal of the Geological Society 109: 102: 76: 69: 52: 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 1: 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 1032: 634:Location shooting for the 554: 500:Hardangervidda Natursenter 288: 27:Mountain plateau in Norway 545:Norwegian National Road 7 518:and the mountain village 476:Holocene climatic optimum 265:, with a cold year-round 234: 135: 63: 51: 42: 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). 624: 464:Tolypocladium inflatum 395: 384: 376: 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 390: 382: 371: 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 151: /  966:Plateaus of Norway 839:The New York Times 625:NĂĄr vi døde vĂĄgner 396: 385: 377: 351:Caledonian orogeny 299:(eroded plain) in 198: â€˘ Total 126:Show map of Norway 867:(11): 1521–1541. 705:On Secret Service 601:from hut to hut. 581:in the west. The 455:immunosuppressant 235:Hardanger Plateau 228: 227: 37:Hardanger Plateau 16:(Redirected from 1023: 976:Inselberg plains 915: 914: 912: 910: 901:. 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Retrieved 838: 828: 817: 784: 780: 767: 744: 724: 704: 698: 689: 684: 675: 669: 648: 646: 639: 633: 629:Henrik Ibsen 614: 612: 608: 560: 529: 497: 473: 468: 462: 449: 443:(especially 434: 402: 336: 317: 309: 294: 246: 230: 229: 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 962:: 897:. 875:. 863:. 837:. 803:. 795:. 783:. 779:. 753:^ 733:^ 713:^ 623:: 589:, 522:. 439:, 273:, 253:, 245:: 185:, 177:, 913:. 883:. 871:: 865:9 848:. 811:. 799:: 791:: 619:( 478:( 467:( 330:- 241:( 223:) 20:)

Index

Hardangervidden
Plateau
2001 view of the Hardangervidda landscape
Hardangervidda is located in Vestland
Hardangervidda is located in Norway
60°03′N 007°25′E / 60.050°N 7.417°E / 60.050; 7.417
Vestland
Telemark
Buskerud
Norway
Sandfloegga
plateau
Norwegian
Vestland
Telemark
Buskerud
Europe
alpine climate
glaciers
Hardangerjøkulen
Hardangervidda National Park
Paleic surface
peneplain
Europe
Sandfloegga
HĂĄrteigen
ice ages
Precambrian
Cambro
Silurian

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