The deep rotational debris slide has occurred along the vicinity of the river due to toe cutting by river and prolonged infiltration of rain water along the loose younger alluvium leads to the oversaturation 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
350 m NE of slide no. 74
 NH-313 (Roing-Anini road)
No element at risk where the landslide is located therefore no remedial measures can be suggested.
Toe cutting by river. The prolonged infiltration of rain water along the loose younger alluvium leads to the oversaturation during rainfall.