Debris flow occurred on 19th Aug 2019 in the thick forest where the slopes are moderately dissected. Debris flow initiated due to incessant rainfall. Weak slope forming material and steep slope coupled with continuous rainfall increased the pore pressure
Reghu, R. and Senthilkumar, K., 2020. Macro-scale (1:50,000) Landslide susceptibility mapping in parts of Toposheet nos.Toposheets nos. 48O01, 48O05 and 48N08, Shimoga and Chikmagalur district, Karnataka. Unpublished GSI report.
Maintain the natural stream course
Makeri-2
Makeri-2
Maintain the natural stream course
Toe erosion by stream.