A shallow translational debris slide occurred due to the adverse condition of SFM. Saturation of overburden and increase in pore pressure and loss of cohesion during rainfall causes material to slide. Affected slope is highly dissected by drainages.
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
Pasighat-Yingkiong road Slide 14
NH-513
1.Proper diversion of surface water run pff from the affected slope.2.Maintainence of hill side drain.3.Construction of retaining structure of appropriate height and width.
1.SFM composed of weathered parent rock masss intermixed withsoil.2.Loss of cohesion of parent rock mass during rainfall.3.Affected slope is highly dissected by drainage.4.Ill-planned modifiaction of slope.