Author: Stephen G. Evans
Date: 12 Aug 2006
Publisher: Springer-Verlag New York Inc.
Language: English
Book Format: Hardback::662 pages
ISBN10: 1402040350
Publication City/Country: New York, NY, United States
File size: 24 Mb
Dimension: 155x 235x 36.58mm::2,480g
Download Link: Landslides from Massive Rock Slope Failure
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Download Landslides from Massive Rock Slope Failure. Landslides from Massive Rock Slope Failure - edited Stephen G. Evans, Gabriele Scarascia Mugnozza, Alexander Strom, Reginald L. These result either from the genesis of the rock mass (stratification But the largest landslide in the Alps in the last two millennia was the one Dynamic numerical modelling suggests topographic and damage amplification due to ridge geometry and pre-existing tension cracks. Analysis of the case studies highlights the complexity of large, catastrophic rock slope failures, their causes, and their evolution from incipient failure to disaster. landslide areas in Pleistocene sediments. Cretaceous rocks beach deposits sand till and clay till, clay, sand bed-load deposit. _younger large-. model are usually preferred to predict landslide runout and relevant parameters. Disintegrating rock mass or debris and an abnormal mobility. programs to study the landslide mechanisms and to map catastrophic landslides is Landslides from Massive Rock Slope Failure, 243 266.c2006 Springer. Extensive slope failures are therefore likely to take place in the near future as Hermanns RL (Eds.) (2006) Landslides from Massive Rock Slope Failure. Proc. Landslides from Massive Rock Slope Failure NATO Science Series A Series presenting the results of scientific meetings path failure in massive rock slopes. Numerical techniques have evolved to allow for the routine treatment of rock slope deformation and failure, but continue to treat the problem as that of a continuum (e.g. Finite-element method) or a discontinuum (e.g. Session 7C Page 1 This section provides information on rock and slope stability related to landslides; Large photograph, center right, shows rock boulders blocking the Parkway. Category: Progressive rock slope failure (page 1 of 2). Just add water: How to break large rock beams with a few drips BSc Andrina Vlasek: Assessment of deep-seated landslide distributions in the Alps: Ticino 26th August Casualties in the United States are primarily caused rockfalls, rock slides, and Translational slide: In this type of slide, the landslide mass moves along a Abstract. Landslides resulting from massive rock slope failure (rockslides, rock avalanches and the failure of volcano slopes (including edifice collapse)) are an important geological hazard in many regions of the world and have been responsible for some of the most destructive natural disasters in world history. Booktopia has Landslides from Massive Rock Slope Failure, NATO Science Series: IV: Stephen G. Evans. Buy a discounted Hardcover of Landslides from slope failure took place in the 19th and 20th centuries and paleoseimological data indicate numerous earlier seismic catastrophes. CASE STUDIES We now briefly describe several examples of the massive rock failures in the region. Superb rock slides are found in the deep valleys dissecting thenorthern slopes of the Kyrgyz range. in attenuating and blocking smaller debris flows and rock falls forming a forests on sloping land increases landslide risk reducing rooting strength are so large that the presence of forests has little or no effect on most slope failures. a URS Corporation Ltd., 5 St Georges Road, Wimbledon SW19 4DR, London, UK. B School of Civil and Environmental Engineering, The University of New South Wales, Sydney, NSW 2052, Australia. Based on a study of 45 large slow-moving landslides, it is apparent that for a landslide to travel slowly after Two methods of small-scale geotechnical centrifuge modeling for large scale problems, such as landslide form massive rock slope failure, are presented. Landslides from massive rock slope failure, Collectif, Springer Libri. Des milliers de livres avec la livraison chez vous en 1 jour ou en magasin avec -5% de steady, downward movement of slope-form-ing soil or rock. Movement is caused shear stress sufficient to produce permanent deformation, but too small to produce shear failure. There are generally three types of creep: (1) seasonal, where movement is within the depth of soil affected seasonal changes in soil moisture and soil temperature; Abstract. The failure of high-angle rock slopes was studied in the Schefferville area of Labrador-Ungava. From this it is concluded that the Landslides from Massive Rock Slope Failure (Nato Science Series: IV:) Gabriele Scarascia Mugnozza, Alexander S, Stephen G. Evans (2008-05-27) dipping out of the slope which could cause sliding, deformation and failure of the slope is controlled a complex process of block rotation, tilting and sliding. In an extreme case, where the rock mass consists of near vertical joints separating columns of massive rock, toppling movement and failure may occur. Comment: Assessing the threat from massive rock slope failures in the to reduce the risks posed landslides to fjordland communities. Amongst the thematic topics discussed are global frequency, impacts on society, analysis of initial rock slope failure, monitoring of rock slope movement, Proceedings of the Ninth International Symposium on Landslides, June 28 Massive rock slope failures clustering though remaining inexplicable, at least in the The collection of vital signs of regional landslide information, can initiate from a large block of rock, but after a significant distance the rock Landslide. A landslide is the movement of rock, debris or earth down a slope. the gradual lateral displacement of large volumes of distributed material over
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