ose significant geological hazards and risks for communities along mountain fronts and in valleys (Havenith et al., 2006; Strom, 2013; Qiu et al., 2016). Mountain fronts with slow-moving landslide masses are often affected by a sudden acceleration of downhill motion and rapid displacement of material. Deep-seated gravitational slope deformation (DSGSD) is mountain slope deformation of steep, high mountain slopes,

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