Crevasse

Crevasse

Jesse Russell Ronald Cohn

     

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ISBN: 978-5-5109-2268-4

High Quality Content by WIKIPEDIA articles! A crevasse is a deep crack in an ice sheet rhys glacier (as opposed to a crevice, which forms in rock). Crevasses form as a result of the movement and resulting stress associated with the sheer stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces.

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