The shallow translational rock slide occurred due to the ill planned modification of slope where the SFM composed of highly jointed and fractured quartzite. During heavy precipitation seepage water flows along these joints causes loss of cohesion.
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
Pasi-Tinali Slide 2
NH 513
1.Removal of slide materials to avoid boulders falling on the road side.2.Construction of retaining structures.
1.SFM is composed of loose detached boulders of parent rock mass intermixed with soil.2.Damp hydrological condition.3.Loss of cohesion on the affected slope.