Major Alpine overthrust in the Tschingelhorner in the Grison Alps,Switzerland. The rocks above the prominent thrust fault are conglomerates of Permian age,whereas below is highly deformed limestone of Mesozoic age and flysch of Cenozoic age. The rock window is the famous Martinsloch between the towns of Flims and Elm. | |
Licence : | Droits gérés |
Crédit: | Science Photo Library / Alean, Dr. Juerg |
Taille de l’image : | 6720 px × 4480 px |
Model Release : | Non requis |
Property Release : | Non requis |
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