The shallow rotational debris slide has occurred due to the intensive percolation of the water in the SFM. It increased the pore water pressure and reduced the shear strength of the overburben.
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 24.9 kms along NH-313 towards Hunli
Newly connstructing Roing-Hunli/ Anini road NH-313
1.Removal of uprooted trees and plants from the slide. 2.Cleaning of weep holes of the retaining wall required. 3 Construct the road side drains for discharge of water.
Extensive cuttiong of slope for road construction. As a result of slope saturation cause the increased the pore water pressure and reduced the shear strength of the slope.