Exploring the potential for physically-based models and contemporary slope processes to examine the causes of holocene mass movement

Author:

Brooks S. M.,Anderson M. G.,Ennion T.,Wilkinson P.

Publisher

Springer-Verlag

Reference46 articles.

1. Anderson, M.G., K.S. Richards, and P.E. Kneale (1980): The role of stability analysis in the interpretation of the evolution of threshold slopes. Trans. Inst. Brit. Geog. 5: 101–112.

2. Anderson, M.G., M.J. Kemp, and J.M. Shen (1987): On the use of resistance envelopes to identify the controls on slope stability in the tropics. Earth Surface Processes and Landforms 12: 637–648.

3. Anderson, M.G., K.S. Richards, and P.E. Kneale (1980): The role of stability analysis in the interpretation of the evolution of threshold slopes. Trans. Inst. Brit. Geog. 5: 101–112.

4. Anderson, M.G., M.J. Kemp, and D.M. Lloyd (1988): Refinement of hydrological factors for the design of cut slopes in the tropics. International Society for Soil Mechanics and Foundation Engineering Proceedings: 233–240.

5. Anderson, M.G., A.J.C. Collison, J. Hartshorne, D.M. Lloyd, and A. Park (1986): Developments in slope hydrology-stability modelling for tropical slopes. In: Anderson, M.G., and S.M. Brooks (eds.) Advances in Hillslope Processes, Wiley, Chichester: 799–822.

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