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Issue:

English

 

Written by:

Jason M

 

Date added:

January 24, 2015

 

Level:

University

 

Grade:

A

 

No of pages / words:

3 / 761

 

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The upthrust nature of these sheets at West Runton suggests that rotation of toe blocks, generating forward movement of the surrounding loose beach sand, is the principal process of toe-thrust sheet formation (fig. 6). Passive pressing of toe blocks into the surrounding sand under gravity is unlikely to result in either brittle failure of the sand or differential movement of the sand away from the toe blocks (i...
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For example, the bigger landslide blocks are associated with more extensive thrust sheets, and sheet width is likely associated with excavation depth. The presence of multiple and overlapping thrust sheets that vary in extent along the front of landslide blocks (figs. 4, 5) also suggests that different parts of the toe are active at different times and therefore that sliding rates and volumes averaged across the entire landslide (Waltham and Dixon 2000) likely conceal wide spatial and temporal variations...
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