This shallow translational debris slide occured where slope forming material is composed of highly weathered and jointed parent rock mass intermixed with soil combined with removal of slope’s toe support for road construction activities and rainfall de
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
i. Another slide is observed on the right flank of the slide ii.Major drainage observed on the left flank of the slide
Aalo Slide 1
NH-13
i. Construction of retaining wall ii. Removal of slide material to avoid blockage of hill side drain iii. Proper diversion of surface water run off from the affected slope.
i. Slope forming material is composed of highly weathered and jointed parent rock mass intermixed with soil ii. Affected slope is dissected by drainages and rill erosion is observed.