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Term: En-echelon crevasses Class:  
 vernacular   (0%)
Created 6 June 2017
Last modified 6 June 2017
Contributed by GCW Glossary

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Definition: Series of crevasses oriented at an angle to the glacier margin. These form as a result of rotational strain within the ice along the glacier's edge.  Swisseduc 

 GCW 
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