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
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NH-31 slide-1
NH-31
Channeling of water away from the crown area through construction of lined hillside drain on the road. Removal of debris on the slope and construction of breast wall with adequate weep holes at the toe.
Extensive slope cut, Toe cutting of slope during road construction and anthropogenic factors