Slope failure occurred due to weak and unconsolidated slope forming material triggered by incessant rainfall. Loose rock blocks may be removed from slope face.
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
 Mayudia Pass landslide. From Mayudia Pass 0.2 kms along NH-313 towards Hunli
 NH-313 (Roing-Anini road)
Removal of loose rock blocks from the slope face.
Slope failure occurred due to weak and unconsolidated slope forming material triggered by incessant rainfall.