Immature lithology, weak slope forming material, regolith thickness of about 2ΓÇô5 m thickness, deforestation, and rainfall are the main factors that contributed in causing this shallow translational slide. Notably, Jhum cultivation seemed to have pla
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
The affected area is uninhabited. Deforestation for jhum cultivation made the low mounds prone to landslides.
Daoblibdisa market slide No.2
Near Daoblibdisa market
Afforestation with deep rooted trees in order to anchor and strengthen the soil mass
1. Weak slope forming material comprising of sandy insitu soil underlain by weathered sandstone.
2. Overburden thickness of 2ΓÇô5 m.
3. Reduction of slope materialΓÇÖs shear strength on over saturation due to rainfall. 
