It is a shallow translational landslide caused by interplay of various factors like, immature geology, weak slope forming material, regolith thickness of about 2ΓÇô5 m thickness, deforestation, and increase in pore water pressure due to  rainwater inf
Lemdur, K. and Kikon, A. (2018); MacroScale (1:50,000) Landslide Susceptibility Mapping in Toposheet nos. 83G/6 and 83G/7 in Karbi Anglong and Dima Hasao districts in Asam, Kohima District of NGaland and West MNipur distrcit of MNipur. GSI report of FS 2
Sengya Sambhudhan school slide No.3
Approx. 500 m south of sengya Sambhudhan school
Afforestation with deep rooted trees in order to anchor and strengthen the soil mass.
1. Weak slope forming material comprising of weathered, flaggy, ferruginous, medium grained sandstone with sandy insitu soil.
2. Reduction of slope materialΓÇÖs shear strength on over saturation due to rainfall. 
3. Practice of Jhum cultivation at the