Titlebook: Landslides from Massive Rock Slope Failure; Stephen G. Evans,Gabriele Scarascia Mugnozza,Regin Conference proceedings 20061st edition Spri

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MONITORING AND ASSESSING THE STATE OF ACTIVITY OF SLOPE INSTABILITIES BY THE PERMANENT SCATTERERS TEble data, location and morphology of the area, PS density; and motion of the targets. We present the results of the application of the technique at a regional scale in the Central Italian Alps involving different types of instabilities in different materials. The utility of the technique in landslid

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FORECASTING RUNOUT OF ROCK AND DEBRIS AVALANCHESexcept identification of prospective avalanche source areas and a range of postulated avalanche volumes. Like the physically based model, the statistical method yields maps of predicted runout, but it provides no information on runout dynamics. Although the two methods differ significantly in their

Decibel

CONTINUUM NUMERICAL MODELLING OF FLOW-LIKE LANDSLIDESed flow rules. A series of simulations has been performed. The effects of different morphological conditions have been simulated to understand processes close to obstacles, both deformable and perfectly rigid, or of trough shaped profiles where accumulation is favoured. Mohr-Coulomb, Drucker-Prager,

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ANALYSIS OF POST-FAILURE BEHAVIOURain cause for the unexpectedly high mobility of landslides. Water in the debris also introduces a viscous dissipative stress which can account for the relatively channelled behaviour of landslides over topography. The difference between landslides and debris flows is wholly gradational and related t

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Conference proceedings 20061st editionriggered and both are located in Tajikistan. An additional highlight is a detailed description and analysis of large-scale artificial rock avalanches triggered by underground nuclear explosions during the testing programme of the former Soviet Union. .

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LANDSLIDE MOBILITY AND THE ROLE OF WATER F. LEGROS