This landslide which occurred about 150 m from slide no.18 is also situated near the intersection of the Jatinga fault and Bandarkhal fault  characterized by highly deformed sandstone, friable shale, siltstone which are highly porous in nature. Oversatur
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
This landslide occurred near slide no.18.
Bandarkhal4
NH54
Toe support for the affected slope through construction of strong RCC retaining wall with sufficient weep holes founded on sound substratum. Construction and proper maintenance of concrete road side drain.
Oversaturation of slope forming material and increase in local pore water pressure. Loose of toe support due to extensive slope cut along NH4. Weak lithology comprised of fragmented and highly jointed sandstone and friable shale.