Crevices near Thingvellir,south-western Iceland,are formed by the extension of the Earth's crust because here the North American and Eurasian tectonic plates are moving apart. The basaltic lava is covered by dense growth of moss. | |
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 : | - |