Failure of the insitu soil along with the overburden material (tress) in a very steep slope due to toe erosion by a natural stream and triggered by rainfall.
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
The landslide does not pose any threat to settlement or road.
Retzawl4
West of Retzawl
In order to prevent further undercutting by the stream, substantial amount of large boulders/riprap may be placed at the toe portion of slide.  However as the landslide is situated away from settlements and road, no further remedial measures are required
Oversaturation of slope forming material and increase in local pore water pressure. Toe erosion of a very steep hill slope by natural stream. Heavy weight of the overburden (Trees)