Aerial view of Sichelchamm mountain, Switzerland, showing a large syncline fold. The layers of Cretaceous rock, originally deposited in horizontal beds on the seafloor, have folded as a result of the collision between the African and European tectonic plates. In a syncline fold the younger layers are on the inside of the fold. | |
Licence : | Droits gérés |
Crédit: | Science Photo Library / Edmaier, Bernhard |
Taille de l’image : | 3308 px × 3859 px |
Model Release : | Non requis |
Property Release : | Non requis |
Restrictions : | - |