The probability of landslide volume, V <Subscript> L </Subscript>, is a key parameter in the quantitative hazard analysis. Several studies have demonstrated that the non-cumulative probability density, p(V <Subscript> L </Subscript>), of landslide volumes obeys almost invariably a negative power law scaling of p(V <Subscript> L </Subscript>) for landslides...</subscript></subscript></subscript>