The shallow planar debris slide occurred due weathered unconsolidated SFM is unstable along extensive slope cut during 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
 Yatdam slide
Khonsa-Changlang road, NH-215
1.Moderation of slope by benching in between along the slope. 2. Plantation of fast growing plants.
1.Unplanned cutting of slope without stabilizing the slope. 2. Weak slope forming material i.e. intercalation of weathered mudstone and shale of Disang Group.