Thick overburden, vertical slope, incessant rainfall, toe cut by the stream are the causes for the slide. Removal of the debris, easing of the slope and maintainance of the channel path.
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 Unpublished GSI report.
Removal of the debris, easing of the slope and maintainance of the channel path.
Sampemane
Sampemane
Removal of the debris, easing of the slope and maintainance of the channel path.
Presence of weak slope forming material saturated during the incessant rainfall.