The shallow translational debris slide occurred where the SFM material is composed of highly friable and fissile shale, jointed parent rockmass intermixed with soil. Saturation of overburden and loss of cohesion  mainly during  rainfall events has affect
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
NA
West of Kolung Slide 2
NH-513
Construction of retaining structures
i. Slope forming material is composed of friable and fissile shale, jointed parent rockmass intermixed with soil ii. Rill erosion on the affected slope