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The (Corominas 1996) and (Rickenmann 1999) relations, which produced predicted runout distances of 311 m and 379 m, respectively, underestimate the maximum runout distance of the landslide.
At a given initial expansion, the maximum runout distance scales with the initial bed height h0, the runout duration with (h0/g)1/2 and the maximum velocity with (gh0)1/2.
The Klein Rinderhorn rock avalanche released ~ 37 million m3 of limestone along a dip-slope sliding plane, with a maximum runout distance of 4.3 km and estimated Fahrböschung angle of 14°.
Although multiple PDCs are thought to have occurred at the summit area, only the PDC with the estimated maximum runout distance in each direction in the initial phase is considered.
Two separate lavas flowed from the small summit crater on the cone and a nearby lateral vent on the southeastern cone and reached a maximum runout distance of 3.7 km.
Similar(55)
Figure 14 shows the maximum runout distances obtained from the numerical methods used in this study.
Fig. 13 Comparison between the maximum runout distances obtained from the empirical and numerical methods with the field data (in red).
Table 4 and show some differences between the methods used to evaluate the runout distance.
In addition, dam stability is related to landslide runout distance as well.
A simple rule-based soil redistribution model of runout distance was validated using the experimental results.
However, runout distance and duration both increase with increasing initial expansion.
Related(14)
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