The soil slide has occurred due to the intensive percolation of the water in loose younger alluvium leads to the oversaturation of slope forming material.
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 5.4 kms along NH-313 towards Mayudia Pass
 NH-313 (Roing-Anini road)
Plantation of deep-rooted species of grass such as vetiver grass may be considered to bind the particles with its fibrous root system.
Seepage of rain water along the loose younger alluvium leads to the oversaturation during rainfall.