Shallow rotational debris slide occurred due to weathered unconsolidated shale of Barail Group and top soil is slided along the slope during the rainfall.
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
3.3 km E of Rima
NH-315, Nampong-Rima Road
No remedial measures recommended
No remedial measures recommended
1. Weathered frazil slope forming material (shale and 2m thick top soil) is unstable along the slope cut.