A shallow translational debris slide due to the adverse condition of SFM which is composed of thick in-situ soil cover intermixed with parent rock mass. Saturation of overburden and increase in pore pressure and loss of cohesion during rainfall causes ma
Nair,V,Athira., Jamir, I., 2022, Remote Sensing based Macro-scale (1:50,000) landslide susceptibility mapping in Toposheets82L/16, 82P/1,2,3,4,5,6 ; 83I/13,14 & 83M/01 covering  parts of West Siang East Siang, Upper Siang, Dibang Valley and Lower Dibang
Metalled Road
South of Jeru Slide 1
NH-13
1.Removal of slide material so as to avoid blocking of hill side drain.2.Proper drainage of surface wter run off.3.Modification of already constructed and damaged retaining wall with sufficient weep holes.
1.Adverse condition of rock mass.SFM is composed of highly friable carbonaceous shale intermixed with parent rock mass and soil.2.Loss of cohesion and saturation of overburden during rainfall.