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 on the far right 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 : | 9630 px × 3629 px |
Model Release : | Non requis |
Property Release : | Non requis |
Restrictions : | - |