Debris landslide occurred on lowly dissected slope with moderate vegetation.In present scenario the landslide is active & retrogressive in nature. The slope disturbance resulted due to unscientific way of removal of soil by toe or piedmont cutting of the
Kumari, N. and Muduli, S. D., 2020. Macro-scale (1:50,000) Landslide susceptibility mapping in parts of Toposheet nos. 48O02 and 48O06, Chikmangaluru Shimoga, Dakshin Kannada  district,  Karnataka. Unpublished GSI report.
Lined drainage and culvert is required  to discharge excess water downslope
West of Kankod Village
West of Kankod Village
Lined drainage and culvert is required  to discharge excess water downslope
Removal of toe support, high slope gradient and saturation of overburden.