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 24.8 kms along NH-313 towards Hunli
Newly connstructing Roing-Hunli/ Anini road NH-313
1.Construction of retaining wall with proper weep holes at the toe of the slide. 2 Cleaning of line drain (removal of plants and slided material), so that water can easily drain through it.
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.