Figure 7 - uploaded by Thomas Bois
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Experiment 3, σ σ σ σc = 4000 Pa. Model with a local planar, circular, shallow (8 mm deep) weak zone parallel to the slope surface (white dashed line in Figure 9a represents projection of the cut contours on the surface). (a) After 80 acceleration steps; (b) after 100 acceleration steps.
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Gravitational slope failures are common phenomena involving all rock slopes, at various scales. It is widely accepted that different factors exert an influence on those gravitational process. Among these, structural heterogeneities (inherited from the geological history of the massif) and alteration/weathering process are of first order. However, t...
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