Immature geology, weak slope forming material, regolith thickness of about >5 m thickness, deforestation and heavy downpour are the factors that caused a shallow translational slide.  Notably, Jhum cultivation seemed to have played a significant role in
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
Daoblibdisa market slide No.4
Near Daoblibdisa market
Afforestation with deep rooted trees in order to anchor and strengthen the soil mass.
1. Weak slope forming material comprising sandy insitu soil underlain by weathered sandstone.
2. Overburden thickness of >5 m.
3. Reduction of slope materialΓÇÖs shear strength on over saturation due to rainfall. 
4. Practice of Jhum cultivation at th