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
NA
Northwest of Rotung Slide 1
NH-13
1.Removal of loose debris/slide material.2.Proper maintaenance of hill side and proper diversion of surface water runoff.3.Construction of retaining structures.
i. Steep slope angle ii. Ill planned modification of slope for road construction iii. Slope forming material is composed of weathered parent rockmass intermixed with soil