The debris slide occurred on lowly dissected hillslope with thick vegetation during rainfall.  The heavy discharge in flowing higher order stream during rainfall resulted in scouring and toe cutting of hillslope by  nala erosion at toe part of hilllslope
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 Unpublished GSI report.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 is required
Gaurigadde Village
Gaurigadde Village
Lined drainage is required
toe erosion by first order stream are the primary causes.