Steep slope and the inter face between the soil and bed rock is very less, incessant rainfall increase the pore water pressure and percolation of water in between the rock and overburden act as weak plane. Maintaining of the natural stream flow.
Reghu, R. and Senthilkumar, K., 2020. Macro-scale (1:50,000) Landslide susceptibility mapping in parts of Toposheet nos.Toposheets nos. 48O01, 48O05 and 48N08, Shimoga and Chikmagalur district, Karnataka. Unpublished GSI report.
Maintaining of the natural stream flow.
Mudalumane
Mudalumane
Maintaining of the natural stream flow.
Steep slope are the major causes for the slide. The interface between the overburden and bed rock is very less.