Titlebook: Low-Dimensional Cooperative Phenomena; The Possibility of H H. J. Keller Book 1975 Springer Science+Business Media New York 1975

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Peter M. Richardss avalanches. This paper compares the foundations, strengths, and limitations of a physically based model and a statistically based forecasting method, both of which were developed to predict runout across three-dimensional topography. The chief advantage of the physically based model results from i

INERT

Gerald F. Kokoszka of the height lost to the horizontal distance travelled (H/L), which is compared to the coefficient of friction, is not computed from the centre of mass of the deposit, as it should be, but from the distal end. Simple spreading of the landslide mass can then explain the excess runout. However, spre

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P. Dayn mountainous regions. This is largely due to the complexity of the processes driving slope failure and our inadequate knowledge of the underlying mechanisms. Ever increasingly, experts are called upon to analyse and predict the stability of a given slope - assessing its risk, potential mode of fail

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H. R. Zellers avalanches. This paper compares the foundations, strengths, and limitations of a physically based model and a statistically based forecasting method, both of which were developed to predict runout across three-dimensional topography. The chief advantage of the physically based model results from i

Cerumen

B. Renker,R. Comèssuitable set of monitoring data is needed. Different types of landslides present different characteristics and are subjected to different spatial and temporal evolution; these become relevant when working at a regional scale or when a catastrophic evolution of the movement is expected. The Permanent

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A. E. Underhilleffect of freeze–thaw cycles on the stability of seasonally-frozen cut slope along Fangzheng-Harbin expressway was studied. A comprehensive study on the silty clay material of the cut slope was carried out by combining results obtained from field monitoring tests, laboratory experiments and numerica

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