Salu S and  Senthil Kumar K.,2019: Macro-scale (1:50,000) Landslide Susceptibility Mapping in parts of toposheets nos. 48J12 & 48J16 Uttar Kannada and Shimoga districts, Karnataka. Un pub. GSI report for FS 2018-11
over the slide materaial vegetation growth observed and the slide are retrogressive in nature. At places fresh scars observed.
Naduvaddahalli
Karkikoppa-Naduvaddahalli inter link road
Lining of the stream to be carried and loose debris to be removed from the slide area.
Weak slope forming material (clayey soil) coupled with incessant rainfall may cause for the local increase of pore water pressure leads to failure of the slope. Due to incessant rainfall excess water in the stream which leads to toe cut.