      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 Unpublished GSI report.
High risk as road is present. Proper retaining structure followed by filling. Avoid removal of material at toe region
Kodsinge village
Kodsinge village
High risk as road is present. Proper retaining structure followed by filling. Avoid removal of material at toe region
Saturation of overburden material, cutting of slope for road construction