Abstract
It is suggested that rockslide – rock avalanche dams are more complex than is recognized in existing landslide dam classifications. A classification system is proposed emphasizing the three-dimensional relations of the landslide deposit to valley morphology. This system combines a three-step classification taking account of: (A) the plan view distribution of the deposit in relation to valley morphology and the impounded water bodies, (B) the cross valley profile of the landslide deposit as it relates to the buried valley morphology, and (C) the profile of the rockslide debris and the underlying substrate along the thalweg of the valley. It is argued this serves to better describe the dams with respect to the hazard of outburst floods, impoundment histories and the subsequent morphological evolution of mountain stream valleys.
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Acknowledgement
This paper was partly written at the Geological Survey of Canada and partly at the Norges geologiske undersøkelse. The work described in this paper is therefore partially supported by the Research Council of Norway through the International Centre for Geohazards (ICG). Their support is gratefully acknowledged. This is ICG contribution No. 283.
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Hermanns, R.L., Hewitt, K., Strom, A., Evans, S.G., Dunning, S.A., Scarascia-Mugnozza, G. (2011). The Classification of Rockslide Dams. In: Evans, S., Hermanns, R., Strom, A., Scarascia-Mugnozza, G. (eds) Natural and Artificial Rockslide Dams. Lecture Notes in Earth Sciences, vol 133. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-04764-0_24
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