The slide is a shallow translational soil slide caused by slope cut and triggered by incessant rainfall. The material comprises of insitu soil (1 to 1.5 m) at the top and weathered sandstonesilt below. The weak material developed pore water pressure due
Kiso, E. and Tariq, Q. A. (2018); MacroScale (1:50,000) Landslide Susceptibility Mapping in Toposheet nos. 83G/5 and 83G/9 in Karbi Anglong, Dima Hasao and NGaon districts in Asam and Kohima District in  NGaland . GSI report of FS 201718.
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Kania Terongaon1
NH36
1. Slope easing in the crown area and removal of heavy vegetation cover. 2. Maintenance of hillside drains along road.
1. Weak overburden material comprising of weathered sandstoneshalesiltstone with insitu soil. 2. Loss of cohesive strength of materials due to increase in pore water pressure during rainfall.