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. | |
Lizenzart: | Lizenzpflichtig |
Credit: | Science Photo Library / Alean, Dr. Juerg |
Bildgröße: | 6720 px × 4480 px |
Modell-Rechte: | nicht erforderlich |
Eigentums-Rechte: | nicht erforderlich |
Restrictions: | - |