The slope failure occurred on lowly dissected hillslope adjoining agricultural land due to increased infiltration and nala erosion at toe part of hillslope due to over water saturation and increased pore water pressure triggered during heavy rainfall.  T
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 Unpublished GSI report.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 and lined drainage with weep holes are required
South of Hukkalbailu village
South of Hukkalbailu village
Easing of slope and lined drainage with weep holes are required
removal of toe support, Diversion of main stream channel towards hill side accelerated toe erosion.