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
NA
South west of Jengging Slide
NH-513
i.Removal of slide material from the affected slope. ii.Proper maintainence of hill side drain.
i. Fragile SFM: overburden material comprising fragmented sandstone and shale intermixed with soil (colluvium).
ii. Hillslope moderately dissected by drainages.
iii. Saturation of slope material during rainfall events.