Gully erosion leading to shallow rotational slide. High rainfall in the area leads to percolation of water, with development of local pore water pressure and lose of cohesion.
Tep, Y. and Kumar, A. (2018); MacroScale (1:50,000) Landslide Susceptibility Mapping in Toposheet nos. 83C/16 and 83H/1 in  Dima Hasao and Cachar districts in Asam and East Jaintia hills  District in  Meghalaya and West and Central MNipur district in MNi
As it is situated away from settlement and road, remedial measures not required.
Longrangajao slide.
Longrangajao village
As it is situated away from settlement and road, remedial measures not required. However it is observed that there is Jhum cultivation above the crown of the landslide. Therefore, it is suggested to avoid future jhum fields and plantations near the slide
Reduction of strength of the slope forming material on supersaturation due to heavy rain. Gully erosion