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. | |
Lizenzart: | Lizenzpflichtig |
Credit: | Science Photo Library / Edmaier, Bernhard |
Bildgröße: | 3308 px × 3859 px |
Modell-Rechte: | nicht erforderlich |
Eigentums-Rechte: | nicht erforderlich |
Restrictions: | - |