Abstract
Fast slope failures are important because they frequently leave no time available for their remediation or even escape of people. Several types of fast slope failures occur, such as:
• Slides on single or multiple surfaces
• Rock falls and rolls
• Soil and rock avalanches, debris run-outs and fast spreads
• Soil flows
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Srbulov, M. (2011). Fast Sliding of Non-liquefied Soil. In: Practical Soil Dynamics. Geotechnical, Geological, and Earthquake Engineering, vol 20. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-1312-3_5
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DOI: https://doi.org/10.1007/978-94-007-1312-3_5
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