A view on some hydrological triggering systems in landslides
published at : Temporal stability and activity of landslides in Europe with respect to climatic change (TESLEC). Special issue
In this paper different types of hydrological triggering systems for debris flows, shallow and deeper landslides are described. The generation of surface run-off and high peak discharges in first order alpine catchments is an important triggering mechanism for debris flows. The assessment of meteorological threshold conditions for shallow landslides needs more detailed meteorological information than for deeper landslides. In the analyses of the hydrological triggering systems of deeper landslides the presence of a permeable top layer and fissures has to be taken into consideration
published at : Geomorphology / ISSN 0169-555X
Editor : Elsevier, Amsterdam - PAYS-BAS (1987)
Millesime : 1999, vol. 30, no 1-2 [pp. 25-32]
Bibliographic references : 17 ref.
INIST-CNRS, Cote INIST : 21151