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- W3043490580 abstract "Runout distance was used here to determine whether the large landslide deposit formed several thousand years ago in northern Tahiti was caused by a single or multiple events. Using modelling to quantify the dynamics of this event suggested that a single event or a small number of events (n < 10) were responsible, and that the maximum slide velocity was high (>125 m/s) under partially submarine conditions. Such submarine propagation favoured a slower dynamic but a longer runout. The effective basal friction under submarine conditions ranged from 0.2 < μ < 0.3." @default.
- W3043490580 created "2020-07-23" @default.
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- W3043490580 date "2020-12-01" @default.
- W3043490580 modified "2023-10-13" @default.
- W3043490580 title "Modelling the mobility and dynamics of a large Tahitian landslide using runout distance" @default.
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- W3043490580 doi "https://doi.org/10.1016/j.geomorph.2020.107354" @default.
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