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Titlebook: Natural and Artificial Rockslide Dams; Stephen G. Evans,Reginald L. Hermanns,Gabriele Sca Book 2011 Springer-Verlag Berlin Heidelberg 2011

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G. Bianchi-Fasani,C. Esposito,M. Petitta,G. Scarascia-Mugnozza,M. Barbieri,E. Cardarelli,M. Cercato,
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Rock Avalanche Dams on the Trans Himalayan Upper Indus Streams: A Survey of Late Quaternary Events id dams, the barriers composed of two or more materials due to the interaction of the rock avalanche with substrates, or large uptake of moisture. Most of the newly discovered dams impounded lakes for many years, some for centuries, and the evidence suggests relatively gradual or phased breaching. S
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Rockslide Dams in the Northwest Himalayas (Pakistan, India) and the Adjacent Pamir Mountains (Afghaockslide dams in the northwest Himalayas impounded lakes with volumes in excess of 20 Gm., significantly larger than present-day Lake Sarez. We use SRTM-3 digital terrain data and satellite imagery to analyse four major historical rockslide damming events (1) our analysis of the 1841 Indus rockslide
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Stability and Life Span of Landslide Dams in the Himalayas (India, Nepal) and the Qin Ling Mountainoraine material, size of the catchment area, climatic conditions and rates of sedimentation. Finally a simple diagram, which correlates the grain, boulder and block size of landslide material and the stability of a dam should help in determining whether a lake-damming landslide is stable or not.
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Formation and Treatment of Landslide Dams Emplaced During the 2008 Wenchuan Earthquake, Sichuan, Changjiashan Lake), 7 dams had a high danger, 5 dams medium danger and 8 dams were of low danger. The case of the Tangjiashan rockslide dam that formed the largest landslide-dammed lake, is discussed in detailed. The scenarios analysed were for 20, 25, 33, and 50% of the dam failing, yielding, respect
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