The shallow planar debris slide occurred due to weathered SFM is unstable along the 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
Yankang slide
Khonsa-Changlang road, NH-215
1. Removal of slided debris material
1. Slope forming material is weathered intercalation of shale and siltstone of Barail Group. This makes the SFM unstable along extensive slope cut during rainfall.