Fig. 15: Deformation model diagram of a large-scale deep landslide in the Guili-Baige section of the Jinsha River. | npj Natural Hazards

Fig. 15: Deformation model diagram of a large-scale deep landslide in the Guili-Baige section of the Jinsha River.

From: Deformation and failure mechanisms of deep-seated landslides: insights from Guili-Baige in Jinsha River tectonic belt

Fig. 15

a Crustal extrusion and uplift process; b Strong earthquakes and faults cause disturbance to the slope; c River erosion causes the front accumulation to become unstable and slide; d Rainfall infiltration causes the slope front to A strong deformation area is formed; e the strong deformation area loses stability and slides and blocks the river channel; f the slope changes before and after instability sliding.

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