Steep slope coupled with incessant rainfall caused the increase of the pore water pressure and the soil lost it strength. During the rainfall excess water in the stream cut/scoured the adjacent slope. Presence of thick insitu soil also one of the reason.
Reghu, R. and Senthilkumar, K., 2020. Macro-scale (1:50,000) Landslide susceptibility mapping in parts of Toposheet nos.Toposheets nos. 48O01, 48O05 and 48N08, Shimoga and Chikmagalur district, Karnataka. Unpublished GSI report.
Clearing of the fallen slide material from the slide area and easing of the slope.
Dombisara
Dombisara
Clearing of the fallen slide material from the slide area and easing of the slope.
Toe erosion by stream. Anthropogenic activities( unscientific cutting of slope)