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Image:Crevasses-alpine-glacier.jpg|'''[[Crevasses]]''' cracks in the '''[[glacial]]''' '''[[ice]]'''. The upper 30 meters of glacial ice is somewhat brittle, and as the glacier flows, cracks develop. Crevasses rarely extend to depths below approximately 30 meters because the ice below that too plastic and the cracks close. Image:Crevasses-alpine-glacier.jpg|'''[[Crevasses]]''' cracks in the '''[[glacial]]''' '''[[ice]]'''. The upper 30 meters of glacial ice is somewhat brittle, and as the glacier flows, cracks develop. Crevasses rarely extend to depths below approximately 30 meters because the ice below that too plastic and the cracks close.
Image:Stockhorn Thun Switzerland.jpg|'''[[Horn]]''' a pyramid-shaped mountain '''[[peak]]''' created by several '''[[glaciers]]''' '''[[eroding]]''' away at different sides of the same '''[[mountain]]''' Image:Stockhorn Thun Switzerland.jpg|'''[[Horn]]''' a pyramid-shaped mountain '''[[peak]]''' created by several '''[[glaciers]]''' '''[[eroding]]''' away at different sides of the same '''[[mountain]]'''
 +Image:Glaciers mountain terms.jpg|'''[[Glacier]]''' and '''[[Mountain]]''' terms
</gallery> </gallery>

Revision as of 16:50, 4 July 2010

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