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Tuxer Alpen with Patscherkofel |
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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.
- Location
- View on OpenStreetMap
- Created
- on Sunday 10 July 2016 by Martin Mergili
- Keywords
- alpine vegetation, cityscape, cultural landscape, DSGSD, glacial processes, high-mountain ecosystems, landslide, metamorphic rock, mountainscape, mountaintop, non-tropical montane forest, Zonobiome VI
- Visits and license
- 13838 visits, CC BY-NC-SA 4.0 DEED license