A shallow rotational debris slide due to the adverse condition of SFM which is composed of thick in-situ soil cover intermixed with parent rock mass. Saturation of overburden and increase in pore 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
1.One more slide is observed in the left flank of the slope.2.No weep holes were given on the reatining wall.3.Cracks were observed in the RCC wall 22m upto damaged wall.
South of Jeru Slide 3
NH-13
1.Proper maintainence of hill side drain all along the affected slope.2.Already constructed retaining structures should be modified withsufficient weep holes.3.Removal of loose detached boulders to avoid further fall.
1.SFM is composed of parent rock fragments (both quartzite and shale) intermixed with soil.2.Drainage direction on the affected slope.3.Saturation of overburden materials during rainfall events.