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・ Hardeland hydroelectric power station
・ Hardeman
・ Hardeman (surname)
・ Hardanger
・ Hardanger (disambiguation)
・ Hardanger Arbeiderblad
・ Hardanger Bridge
・ Hardanger District Court
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Hardangervidda
・ Hardangervidda National Park
・ Hardangervidda Natursenter
・ Hardanges
・ Hardap Dam
・ Hardap Region
・ Hardap, Namibia
・ Hardas Pur
・ Hardasipur
・ Hardau (Winterthur)
・ Hardau valley
・ Hardaway
・ Hardaway High School
・ Hardaway Site
・ Hardaway, Alabama


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Hardangervidda : ウィキペディア英語版
Hardangervidda

Hardangervidda is a mountain plateau ("vidde" in Norwegian) in central southern Norway, covering parts of the counties of Buskerud, Hordaland and Telemark. 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. The region is divided administratively between the counties of Buskerud, Hordaland, and Telemark.
==Geography and geology==

The plateau is the largest peneplain (eroded plain) in Europe, covering an area of about at an average elevation of 1,100 m (3,500 ft). 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 1,000 mm per year (39 inches) 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.〔


抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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