The slide originated in the high to moderately dissected steep slope. Initially the slide occurred as a soil slide later graded into debris flow. This debris flow should be monitored during the future rainy season.
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 Unpublished GSI report.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 original nala course. Do not construct any settlement along the flow direction. This landslide to be monitored during the future rainy season.
Hanigeri
Hanigeri
Maintain the original nala course. Do not construct any settlement along the flow direction. This landslide to be monitored during the future rainy season.
Toe erosion by stream. unscientific cutting of slope