  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. Along with the weathered material, vegetation and rock fr
  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 Unpublished GSI report.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 concreate measures. Remove check points, barriers from main stream.
North of Kannur village
North of Kannur village
Toe support by concreate measures. Remove check points, barriers from main stream.
Vertical road cut failure