The shallow rotational debris slide has been occurred due to the prolonged percolation of water along the weak planes, leads to the increased stress and pore water pressure resulted the slope failure and road subsidence in downslope direction.
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 23.3 kms along NH-313 towards Hunli
Newly connstructing Roing-Hunli/ Anini road NH-313
1.Removal of protruded overburden from the crown portion.  2. Slope angle to be reduce by benching. 3. Removal of loose material from the slide.
Extensive slope cut for road construction. Weathering and widening of joint planes causing loosening of blocks along the joint planes alonf with super saturation of the SFM