Article ID Journal Published Year Pages File Type
4684274 Geomorphology 2015 10 Pages PDF
Abstract
A reactivation of the mass movement by frictional sliding of the material half way the run-out track was simulated. It occurred 30 min after the first run-out phase due to an increase in pore pressure. The sliding material changed into a slow flowing mass that reached a newly built up area after about 1 h and moved into Wangong Town over a distance of 80 m.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Authors
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