A shallow translational debris slide occurred due to the adverse condition of slope forming material.Saturation of overburden and increase in pore pressure and loss of cohesion during rainfall causes material to slide.
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
i. Slope angle 45°?N310° ii. Extensive slope cut due to road widening
Jomlo-Mongku Slide 2
NH-13
i. Construction of retaining wall is under progress ii. Proper diversion of surface water run off from the upslope
i.SFM composed of weathered parent rock masss intermixed withsoil. ii.Loss of cohesion of parent rock mass during rainfall iii.Affected slope is highly dissected by drainage iv.Ill-planned modification of slope.