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・ Wanjia Reeducation Through Labor Camp
・ Wanjiali Square Station
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・ Wanjiku
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Wank (mountain)
・ Wank (surname)
・ Wank Week
・ Wank'ap'iti
・ Wank'ayuq Saywa
・ Wank'uchiri
・ Wanka
・ Wanka Quechua
・ Wankan
・ Wankaner
・ Wankaner (Savli)
・ Wankaner (Vidhan Sabha constituency)
・ Wankaner Junction railway station
・ Wankaner State
・ Wankaner-Surendra Nagar section


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Wank (mountain) : ウィキペディア英語版
Wank (mountain)

The Wank ((:ˈvaŋk)) is a mountain in southern Germany, situated in the Loisach valley close to the Austrian border in the southwestern Ester Mountains range near Garmisch-Partenkirchen. It rises from about above mean sea level up to at the summit.〔Rennenberg, H.; Polle, A.; Reuther, M.: "Role of Ozone in Forest Decline on Wank Mountain (Alps)", in Sandermann, H.; Wellburn, A.; Heath, Robert L.: ''Forest decline and ozone: a comparison of controlled chamber and field experiments'', pp. 136-7. Springer, 1997. ISBN 978-3-540-61321-3〕 The mountain is crowned by a grassy summit which offers spectacular views over Garmisch-Partenkirchen and the surrounding region. The summit can be reached via the eponymous Wankbahn, a cable car system that runs during the summer months, or by an extensive network of footpaths that criss-cross the area. It is possible to both eat and sleep on the Wank at the Wank-Haus, a mountain hut on the summit, and a nearby scientific observatory plays an important role in monitoring atmospheric and climatic conditions. The Wank is a popular destination for hikers, day-trippers from Garmisch-Partenkirchen and paragliders, who are able to take advantage of its strong thermals to make exceptionally long flights.
==Physical characteristics==
The mountain's geology, which is dominated by calcareous rocks, is typical of the Bavarian Alps. Its climate is also typical of the region. Precipitation is high, ranging from about at valley level to at the summit. It peaks in the summer and is lowest in winter. The Wank's mean annual air temperature ranges from in the valley to at the summit. The prevailing wind comes from a westerly direction but for about 30 to 40 days a year the mountain experiences a warm, dry föhn wind. A local wind system also operates in the area giving a daily uphill/downhill circulation. Inversion layers occur for about 30 days per year, predominately in the autumn and winter.〔
The Wank was originally covered by a forest consisting of a mix of spruce, fir and beech trees. A process of man-made deforestation that began in the Roman period, when the trees were cut down and the mountain's slopes were grazed by horses, sheep, goats and cattle, resulted in much of the forest being destroyed by the 15th century. Forestry in the area was taken over by the Bavarian government in 1803 but the former forest cover did not regenerate due in part to the continued use of forest lands as pasture, storms and browsing by game animals. As a result, the current Wank forest is predominately spruce (about 75%) and pine (15%). Forestry programmes are currently underway to improve the arboreal diversity of the mountain.〔

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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