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.
| px | px | dpi | = | cm | x | cm | = | MB |
Details
Creative#:
TOP25487919
Source:
達志影像
Authorization Type:
RM
Release Information:
須由TPG 完整授權
Model Release:
N/A
Property Release:
N/A
Right to Privacy:
No
Same folder images:
Loading