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

BLAZE

The Flims Rockslide Dam, a level between 820 and 936 m for very short time; the dam broke partly and a flood happened; the remaining lake survived for a long time and was filled up; the Rhein river eroded the floodplain down to the actual level.

Ibd810

,Rock-Avalanche Size and Runout – Implications for Landslide Dams,known size will travel, and what its internal structure will be, we discuss dynamic grain fragmentation and its role in rock-avalanche and block-slide motion. We then examine how fragmentation affects the stability of rock-avalanche and block-slide dams.

向前變橢圓

Institution

挫敗

AGOG

遵循的規(guī)范

Technical and Human Aspects of Historic Rockslide-Dammed Lakes and Landslide Dam Breaches, which significant information is available, allows the formulation of specific conditions which are generally met with respect to the development of the phenomena, their direct and indirect consequences on the population and the possible prevention and mitigation actions that can be carried out. Th

dowagers-hump

Rockslide and Rock Avalanche Dams in the Southern Alps, New Zealand, data compiled from 43 examples show that evidence of rockslide dams occurs in comparable number on both sides of the main divide despite differing lithology, rates of uplift, erosion, and sediment yield. These controls however constrain the preservation of few rockslide-dammed lakes in the Southern

Spinal-Fusion

misanthrope