The debris slide occurred due to toe cutting of hillslope for widening of agricultural land. The drainage at toe part causes toe erosion and removal of toe support. The prolonged seepage and saturation resulted in hillside collapse due to loss in cohesiv
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 Unpublished GSI report.
Plantation on slope should be encouraged.
North of Dinda village
North of Dinda village
Plantation on slope should be encouraged.
Litho contacts between Metabasalt (competent) and quartz-sericite-schist (highly weathered) facilitating percolation of water, Removal of toe support.