A shallow translational rock slide occurred where SFM is composed of jointed, weathered splintery shales. 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
NA
North of Damro-Gingkong Slide 1
Pasighat-yingkiong road
1. Construction of retaining walls.2.Proper mainatainence of hill side drain.3.Construction of retaining wall of appropriate height and width for toe support.
1.SFM is composed of jointed,weathered and splintery shale.2.Regolith thickness is less than 0.5m.3.Loss of cohesion of parent material during rainfall events.