A deep translational debris slide (natural slide) has occurred on a slope which is structurally controlled and slope forming material is composed of highly weathered shale. This natural slide is triggered by rainfall along with toe erosion by river and h
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
Highly weathered parent rockmass
Old Deka village Slide 1
Old Deka road
No remedial measures are suggested since there are no elements at risk
. Fragile slope forming material. It is composed of highly weathered parent rockmass (shale and sandstone) intermixed with parent soil cover of about 2-5m ii. Structural control in this area iii. Depleted slope is highly dissected by drainages, hence lea