The slumping is observed on hillslope and is demarcated as meta-stable zone susceptible to slope failure during rainfall. The area is identified as slumping zone. The slope forming material consists of in-situ soil with overburden thickness varies betwee
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 Unpublished GSI report.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 and culvert is required  to discharge excess water downslope
Bhartipura village
Bhartipura/Tudike village
Lined drainage and culvert is required  to discharge excess water downslope
Removal of toe support, high slope gradient and high degree of weathering profile are the primary causes.