Glacier crevasses, Canada

Glacier crevasses, Canada

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Credit: DAVID NUNUK/SCIENCE PHOTO LIBRARY

Caption: Glacier crevasses. Crevasses 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.

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Keywords: blue ice, blue sky, british columbia, canada, canadian, coast mountains, cold, crack, cracks, crevasse, crevasses, crevice, crevices, geographical, geography, geological, glacial, glacier, ice, icy, landscape, montane, mountain, mountainous, mountains, national park, national parks, nature reserve, north america, north american, pacific ranges, rockies, rocky, rocky mountains, snow, snowy, tellot glacier, waddington range

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