The shallow rotational debris slide due to anthropogenic activity and weak lithology mainly composed of weathered carbonaceous shale and shale of Barail Group.
Ramesh Guguloth, Neethu Alpho Joseph, 2022, Remote Sensing based Macro-scale (1:50,000) landslide susceptibility mapping in Toposheets 83M/4, 8,12,15,16; 83N/01, 2, 5, 6, 9,13; 92A/03, 4, 6, 7, 11,14,15,16; 92E/02, 3 & 4 covering  parts of Tirap, Changan
NIL
300 SW of Rima
NH-315, Nampong-Rima Road
1. Trimming of crown scar along its length 2. Plantation of fast-growing grass/ shrubs on affected slope.
1. Extensive slope cut without stabilizing the slope. 2. Weathered slope forming material (Shale and Carbonaceous shale, Barail Group) is unstable along the slope.