The slope forming material is predominantly composed of fragmented sandstone and shale intermixed with soil. Rainfall events resulted in saturation of fragile overburden material, increase of pore water pressure and 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
A minor slide is observed on the right flank of the slide at a distance of 10m away
Jengging Slide 1
NH-513
i. Slide materials can be removed further to avoid blocking of road and hill side drain ii. Proper diversion of surface water runoff from the affected slope.
i. Fragile SFM: overburden material comprising fragmented sandstone and shale intermixed with soil (colluvium).
ii. Hillslope moderately dissected by drainages.