“…The results of our modelling (Figures 10 and 11) may help explain why the frequency of landslides and the failure and collapse of volcanic slopes and domes increases following heavy rainfall (Kerle and van Wyk de Vries, 2001;Matthews et al, 2002;Matthews and Barclay, 2004;Elsworth et al, 2004;Simmons et al, 2004;Taron et al, 2007;Saucedo et al, 2008;Hicks et al, 2010;Vázquez et al, 2022). Extreme or heavy rainfall has been linked to multiple volcanic hazards (McKee et al, 1981;Matthews et al, 2002;Barclay et al, 2006), with theorised mechanisms that range from deep-seated saturation and stress perturbations (McBirney, 1955;Violette et al, 2001;Farquharson and Amelung, 2020;Sahoo et al, 2022) to shallow-seated processes operating in the dome or upper edifice. Of these, the latter is often explained in terms of volumetric expansion of liquids as a function of fuel-coolant interactions (Elsworth et al, 2004;Simmons et al, 2004;Taron et al, 2007), with dome pressurisation and/or weakening driven by thermal stress mechanisms (i.e.…”