The rock slide has occurred due to highly jointed nature of country rock, prolonged infiltration of rainwater along the slope surface, dripping hydrological condition leading to development of local hydrostatic pressure
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 18.23 kms along NH-313 towards Hunli
Newly connstructing Roing-Hunli/ Anini road NH-313
1. Removal of loose material occurring at critical angle.
The removal of rock from the toe of the hillslope for road construction disturbance the natural slope. The seepage and infiltration of water along the weaker plane of the county rock resulted in intense weathering and slope saturation.