1 Introduction
Causes and Triggers of Mass-Movements: Overloading Short title: Causes and Triggers of Mass-Movements: Overloading Causes and Triggers of Mass-Movements: Overloading Alain Demoulina, b Hans-Balder Havenithc aFRS-FNRS, Brussels, Belgium bUnit of Physical Geography and Quaternary, Département de GéographieDepartment of Geography, University of Liege, Liege, Belgium cDepartment of Geology, University of Liege, Liege, Belgium 1 Introduction Any review of the literature on landslides rapidly comes to the obvious conclusion that heavy rainfall and earthquakes, occasionally also volcanic eruptions, are the most cited triggers of landsliding in natural conditions. By contrast, slope overloading is more frequently considered a major direct cause of human-induced mass movements, as evidenced by the dominant use of the term to refer to anthropogenic loading in the engineering literature. However, there may actually be natural seismic and non-seismic landslides whose main trigger is overloading, whereas overloading is but one of several concurrent factors in many anthropogenic landslides. Strictly speaking, slope overloading is defined as the addition of a load that increases the existing stress applied to a slope, more specifically to a weaker shear surface within the slope material, so that the latter’s ultimate shear strength is exceeded and failure occurs. But we shall also consider many more cases hereafter, where a moderate surcharge load, though not able to initiate slope failure by itself, is nevertheless a potent cofactor of triggering. The added load is either static (e.g., accumulation of fill or waste on top of a slope) or dynamic, inducing transient instantaneous excess shear stresses (seismic loading, wave loading).
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