Initially Slope angle ranges from 25-35 degree and the interface between the overburden and bed rock is very less along the flow direction. At few places the overburden thickness ranges from 2-3m. Incessant rainfall is also one of the triggering factors
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 Unpublished GSI report.
Original stream flow to be maintained
Hallimangatta
Hallimangatta
Original stream flow to be maintained
unscientific cutting of Slope 