It is located in the central alpine zone of southern Norway, at approximately 61°-62°N and 7°-9°E, with the water systems of Sognefjorden and Nordfjorden carving a deep U-shaped valley from the west, and the upper reaches of the Gubrandsdalsbrücken to the east. The Jostedalsbrücken is located to the west of this mountain range. This mountain range is composed of Caledonian orogenic thrust metamorphic rocks from about 400 million years ago. It shows a remarkable glacial topography, carved by valley glaciers during the glacial period, and several small glaciers still remain, but these disappeared once during the postglacial period and then formed again. Source: Heibonsha World Encyclopedia, 2nd Edition Information |
南ノルウェー中央高山帯で北緯61゜~62゜,東経7゜~9゜付近にあり,西からソグネフィヨルドSognefjorden,ノールフィヨルドNordfjordenの水系が深いU字谷を刻み,東にはグブランスダールの上流河川が延びる。ヨステダール氷河はこの山塊の西にある。この山地は約4億年前のカレドニア造山衝上変成岩よりなる。氷期の谷氷河に削られ著しい氷食地形を示し,いくつかの小氷河が現存するが,これらは後氷期に一度消失してその後再びできたものである。
出典 株式会社平凡社世界大百科事典 第2版について 情報 |
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