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Tuxer Alpen with Patscherkofel

WI_at023_522b.jpg

View from Viggarspitze in NW direction to Patscherkofel (2246 m). The metamorphic rocks forming this part of the Tux Alps, predominantly quartz phyllite, are susceptible to deep-seated gravitational slope deformations, indicated by the numerous back scarps. The central Inn valley with Innsbruck and the Karwendel are shown in the background.

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Created
on Sunday 10 July 2016 by Martin Mergili
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16411 visits, CC BY-NC-SA 4.0 DEED license