         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 Unpublished GSI report.
Retaining wall to be given. Settlements on upper slope may be shifted
Kansur village
Kansur village
Retaining wall to be given. Settlements on upper slope may be shifted
Toe cutting and toe erosion by stream