The slide has triggered along Hunli-Anini road section as a result of saturation of highly friable chlorite schist and jointed planes during rainfall and failed along the extensive slope cut.
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 55.8 kms along NH-313 towards Anini
 NH-313 (Roing-Anini road)
1. Removal of protruding and loose rock fragments occurring at critical angle in crown scar. 2. Removal of slided material from road.
1. Highly jointed and weathered friable chlorite schist. 2. Steep extensive slope cut for road construction. 3. Saturation of rock and weak planes due to rainwater.