1. Context
Slope movements are extremely varied in terms of size, morphology and kinematic evolution. Numerous classifications have been proposed, based on different criteria: morphology, kinematics, nature of materials, etc. . Three main families of phenomena can be distinguished, which are responsible for major displacements of materials on slopes and hillsides:
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Bibliography
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(1) - FLAGEOLLET (J.-C.) - Les mouvements de terrain et leur prévention. - 224 p., Masson, Paris (1989).
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(2) - COLAS (G.), PILOT (G.) - Description et classification des glissements de terrain. - Bull. Labo. P. et Ch., spécial, p. 21-30 (mars 1976).
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