A shallow translational slide occurred due to the adverse condition of slope forming material 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 durin
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
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Koreng-Aalo road Slide 1
NH-13
i. Removal of slide materials to avoid blockage of road and hill side drain ii. Proper maintainence of hill side drain
i.Slope forming material is composed of loose unconsolidated soil intermixed with weathered parent rockmass ii. Loss of cohesion and saturation of overburden materials during rainfall events.