The soil slide initiated since 2015 and since then reactivated every year. Vertical slope coupled with incessant rainfall increased the pore pressure, toe cut and weak slope forming material in the steep slope are the main causes for the slide. Removal o
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 Unpublished GSI report.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 construction of channel drain are recommended.
Devaganege
Devaganege
Removal of the debris, easing of the slope and construction of channel drain are recommended.
Slope angle ranges from 25-35 degree and the interface between the overburden and bed rock is very less along the flow direction.