The shallow translational debris slide occurred during rainfall due to the thick in-situ soil cover intermixed with rock fragments as SFM. Here regolith thickness is more than 5m. Also damp hydrological condition increases the saturation of overburden he
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
Shops partially damaged/destroyed
NH-13 Slide 6
NH-13
1.Removal of loose debris from the affected slope 2. Proper diversion of surface water runoff. 3.Construction of retaining structure.
1.SFM composed of thick institu soil cover intermixed with rock fragments.2. Damp hydrological condition.3. Drainage on the left flank of the affected slope.