The debris flow originated in the thick forest during the rainy season. The slope gradient are high and the slopes are moderately dissected. During the rainy season the slide to be monitored properly.
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 Unpublished GSI report.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
Hanigeri-2
Hanigeri-2
Maintain the natural stream course
Toe erosion by stream