Glacier crevasse. Crevasse in the surface of the Tellot glacier. Crevasses form in glaciers as the ice cracks when the glacier moves. The stresses put on the ice as it flows down the mountain cause cracks like these to appear and disappear over time. Some crevasses can be extremely deep. The Tellot glacier is located in the Waddington Range of the Coast Mountains,British Columbia,Canada | |
Lizenzart: | Lizenzpflichtig |
Credit: | Science Photo Library / Nunuk, David |
Bildgröße: | 3508 px × 5084 px |
Modell-Rechte: | nicht erforderlich |
Eigentums-Rechte: | nicht erforderlich |
Restrictions: | - |