The shallow planar debris slide is due to extensive slope cut for road construction and the intensive percolation of the water in the overburden. increase the pore pressure and loss of cohesion during rainfall.
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 16.57 kms along NH-313 towards Mayudia Pass
 NH-313 (Roing-Anini road)
1.Easing of slope/ slope gradation is required.
1.The slope disturbance occurred due to vertical cutting of the hillslope for the road construction without any toe support.