The slide has occurred along Hunli to Anini road section, due steep slope cut and saturation of slope forming material during rainfall.
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 Hunli 52.3 kms along NH-313 towards Anini
 NH-313 (Roing-Anini road)
1. Removal of slided and loose material occurring at critical angle. 2. Easing of slope.
1. Steep slope cut for road construction. 2. Slope forming material is composed of highly jointed and fractured chlorite schist intermixed with loose soil. 3. Loss of cohesion and saturation of SFM during rainfall.