Slide recorded along the road cut section along NH 31, slide caused by the presence of joints and weak schistosity planes in the rock that act as releasing plane and oversaturation of the highly weathered and loose material resting on the steep unstable
Chiezou, K. and Kesiezie, K. 2021: Remote sensing based macro scale (1:50,000) landslide susceptibility mapping in toposheets 83A/15, A/16, 83B/13, 83E/02, E/3, E/4, E/6, E/7, E/8, 83F/1, F/5 and F/9 covering  parts of West Kameng, East Kameng, Kurung Ku
Nil
NH-31 slide-3
NH-31
Slope easing and unloading of dead load from the crown area. Clearance of slide debris and construction of proper hillside drains (lined)
Extensive slope cut, Toe cutting of slope during road construction and anthropogenic factors