           The landslide has occurred by erosion of the toe of the slope by the stream flowing at the base. During rainfall, the water flow tends to become turbulent causing the river to erode its banks.
  Neena Vaman, K. V., and  Bhat, A. A., 2020.Macro-scale (1:50,000) Landslide susceptibility mapping in parts of Toposheet nos. 48I12, 48I16, 48J14 and 48J14, Uttar Kannada and Shimoga i district, Karnataka. Unpublished GSI report.
Toe support by appropriate concrete measures. Proper drainage network to be given. Bench the slope and plantation be provided along the slope.
Onithotta village
Onithotta village
Toe support by appropriate concrete measures. Proper drainage network to be given. Bench the slope and plantation be provided along the slope.
Vertical road cut failure