The shallow planar debris slide occurred due to weak slope forming material composed of weathered shale of Disang Group with thick (1m) overburden soil.
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
2km NE of Yanman
Changlang-Khimioyng road
Removal of slided debris material on the road side
Weak slope forming material composed of weathered shale of Disang Group with thick (1m) overburden soil.