The slope failure occurs on steep slope due to poor lithology predominantly composed of highly weathered quartzite with thick overburden material, which gets oversaturated during rain leading to reduced the shear strength and resulted to slope failure
Anicia K.S., Arvind Kumar Singh, 2022, Remote Sensing based Macro-scale (1:50,000) landslide susceptibility mapping in TS no. 82 P/12, 15, 16; 91 C/3, 4, 7, 8, 12; 91 D/1, 2, 3, 4, 5, 6, 8, 9 and 10 covering parts of Lower Dibang Valley, Lohit, Anjaw and
NIL
 From Roing 37 kms along NH-313 towards Mayudia Pass
 NH-313 (Roing-Anini road)
1. Removal of loose material occurring at critical angle 2. Slope moderation by trimming at the crown portion.
The slope failure occurs on steep slope due to poor lithology predominantly composed of highly weathered quartzite with thick overburden material, which gets oversaturated during rain leading to reduced the shear strength and resulted to slope failure