The Debris slump occurred on lowly dissected hill slope with sparse vegetation cover. The slope disturbance is observed due to unscientific way of modification of slope & removal of soil for construction. The slope transformation due to vertical opens up
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 Unpublished GSI report.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.
Kampanakodagi
Devangi road
Lined drainage is required.
Removal of toe support after road cutting, high slope gradient and thick overburden are the primary causes.