The shallow rotational debris slide is due to the intensive percolation of the water in the overburden. 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 27.2 kms along NH-313 towards Hunli
Newly connstructing Roing-Hunli/ Anini road NH-313
1.Removal of uprooted plants from the slide.
Extensive slpe cut leads to the slope transformation opened up new pathway for water infiltration & slope saturation.