The debris slide occurred on lowly dissected hillslope due to removal of soil for arecanut plantation that destabilised the slope. The stream/nala erosion and undercutting or scouring at toe part of hillslope destabilizes the slope due to over water satu
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 Unpublished GSI report.
Easing of slope, lined drainage and breast wall with weep holes are required
Ganapatikatte village
1.8km from Ganapatikatte village
Easing of slope, lined drainage and breast wall with weep holes are required
saturation of overburden material.