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Watzmann Glacier : ウィキペディア英語版 | Watzmann Glacier
The Watzmann Glacier is one of the five recognised glaciers in Germany.〔The Watzmann has been recognised as a glacier by the Commission for Glaciology of the Bavarian Academy of Science since 1959〕 It is located below the famous east face of the Watzmann in the Watzmann cirque and is surrounded by the ''Watzmanngrat'' arête, the ''Watzmannkindern'' and the ''Kleiner Watzmann''. The size of the glacier reduced from around in 1820 until it split into a few fields of firn, but between 1965 and 1980 it advanced significantly again〔http://www.lrz.de/~bayerischegletscher/wmg.htm〕 and now has an area of .〔(''Watzmanngletscher - Topographie'' ) at www.lrz.de. Accessed on 24 Dec 2010〕 Its classification as a glacier is not undisputed by scientists, however, due to its size and its low flow velocity. Above and to the west of the icefield lie the remains of a JU 52 transport aircraft than crashed in October 1940. Amongst the other permanent snow and icefields nearby are the ''Eiskapelle'' ("Ice Chapel"), which is well-known due to its easy accessibility from St. Bartholomä and may be the lowest lying permanent snowfield in the Alps, and the ''Schöllhorneis'' on the east face itself. == References ==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Watzmann Glacier」の詳細全文を読む
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