The Matterhorn as seen from near Trockener Steg,above Zermatt,Valais,Switzerland. The rocks in the foreground are Ophiolites. Some have been uplifted from depths of at least 100 km within the Earth's crust during the formation of the Alps. Orange-brown colours are due to weathering of iron-bearing minerals. | |
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 |
Restrictions : | - |