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10.1073/pnas.1607009113

http://scihub22266oqcxt.onion/10.1073/pnas.1607009113
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C5027430!5027430!27573836
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suck abstract from ncbi


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pmid27573836      Proc+Natl+Acad+Sci+U+S+A 2016 ; 113 (37): 10281-6
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  • Rate-weakening friction characterizes both slow sliding and catastrophic failure of landslides #MMPMID27573836
  • Handwerger AL; Rempel AW; Skarbek RM; Roering JJ; Hilley GE
  • Proc Natl Acad Sci U S A 2016[Sep]; 113 (37): 10281-6 PMID27573836show ga
  • A predictive understanding of landslide behavior remains elusive, to the extent that once landslide motion is detected the factors that control whether motion will remain slow or accelerate to catastrophic failure remain uncertain. Here, we adapt standard fault mechanics treatments to present a single model that captures both slow and catastrophic landslide motion. We test model predictions using field, laboratory, and remote sensing observations. The failure mode depends on the material properties and the dimensions of the landslide slip surface relative to a critical size. If the slip surface exceeds this size and has rate-weakening frictional properties then catastrophic failure must occur. However, landslides composed of rate-weakening material are characterized by slow sliding when the critical size exceeds landslide dimensions.
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