The slide is a shallow translational slide caused by extensive slope cut, triggered by incessant rainfall. The other causative measures include poor slope forming material and improper maintenance of draiNGe outlet. During incessant rainfall the weak mat
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 Terongaon2
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 waterpressure during rainfall. 3. Extensive cutting of slope.