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Term: Frozen talus slopes Class:  
 vernacular   (0%)
Created 6 June 2017
Last modified 6 June 2017
Contributed by GCW Glossary

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Definition: Slope, formed by rocks and blocks of considerable thickness. Massive or interstitial ice can result in gravity driven creep deformations. These slopes may be associated with other creeping landforms, such as Rock Glaciers or Gelifluction slopes.  TrombottoGeocryology 

 GCW 
Examples: