It is a shallow translational slide caused by a combination of factors like immature geology, weak slope forming material, regolith thickness of about 2ΓÇô5 m thickness, deforestation and sudden increase in pore water pressure due to infiltration of r
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
Deforestation for jhum cultivation makes hill slopes more prone to landslides.
Sengya Sambhudhan school slide No.1
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 and fragmented sandstone, clay, with sandy insitu soil.
2. Overburden thickness of 2ΓÇô5 m.
3. Reduction of slope materialΓÇÖs shear strength on over saturation due to rainfall. 
4. Practice of