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
Retaining wall already constructed.Small slide is observed ata the left flank of the slide.
Pangin Slide 1
NH-13
1.Systematic channeling of surface drainage from the crown part.2.Removal of slide material.
1.SFM is composed of thick institu soil cover intermixed with parent rock mass.2.Loss of cohesion and saturation of overburden during rainfall.3.Steep slope gradient.4.Damp hydrological condition.5.Gully erosion on tha affected slope.