The affected area is composed of weak lithology, comprising of weathered shale (fragmented) with conglomerate layer at the top. The beds are horizontal to subhorizontal with beds dipping towards the valley. The slide is a shallow debris slide which is re
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.
NA
Sakhabi
SE of Sakhabi village
1. Trim off the unstable mass from the crown area. 2. Proper maintenance of draiNGe at the toe of the slope cut.
1. Poor slope forming material comprising of highly weathered shalesilty shale. 2. Prominent bedding planes dipping towards the valley. 3. During rainfall the weak material loses its cohesive strength and fails along its weak plane.