Surface of the Tellot glacier. View over the surface of part of the Tellot Glacier,showing its rough and cracked texture. Cracks and crevices form in glaciers as the ice splits 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: | 7364 px × 2426 px |
Modell-Rechte: | nicht erforderlich |
Eigentums-Rechte: | nicht erforderlich |
Restrictions: | - |