The debris slide occurred due to unstable slope forming material along the slope extensive slope cut.
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
500m Swof Rangran
Changlang-New Changalang road
1. Removal of slided debris material 2. Construction of hill side drainage.3.  Modification of slope at crown part of the slide
Debris fall/slide occur on steep slope due to weathered shale triggered by intense rainfall.