         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 Unpublished GSI report.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 to be given. Slope to be benched, along with plantation to be given on the slope. Slided material not to be removed.
Yelugar village
Yelugar village
Toe support to be given. Slope to be benched, along with plantation to be given on the slope. Slided material not to be removed.
Toe cutting and toe erosion by stream