The slide occurred on a moderately dissected hill slope, materially composed of highly weathered and fragmented sandstone, thin clay beds, conglomerates and sandy insitu soil cover underlain by steeply dipping fresh rock (towards the valley) forming a we
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
Though itΓÇÖs a big landslide, the affected area is uninhabited and thus poses no threat to life or property.
Sengya Sambhudhan school slide No.2
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, thin clay and conglomerate beds, with sandy insitu soil (~2 m) cover.
2. Dissection by hill slope draiNGes.
3. Reduction of slope materialΓÇÖs shear