Tuesday, 4 October 2016

A Multistage Technique to Minimize Overestimations of Slope Susceptibility at Large Spatial Scales

Rainfall induced landslides are one of the most frequent natural hazards on slanted terrains. They usually result in great economic losses and fatalities globally. Worldwide at least 32,322 deaths between 2004 and 2010 have been reported and in the United States alone, landslides cause $1-2 billion in damages and more than 25 fatalities in average each year.

Multistage Technique to Minimize Overestimations
Understanding, mapping, modeling and preventing the aftermath of these devastating events represents an important scientific and operational endeavor.The term “Landslide” describes the downward and outward movement of slope-forming materials that include rock, earth, and debris or a combination of these.

Although landslides are considered to be dependent on the complex interaction of several static and dynamic factors slope angle has great influence on the susceptibility of a slope to sliding. Increased slope angle usually correlates to increased likelihood of failure even if the material distribution on the slope is uniform and isotropic.

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