The shallow planar failure occurred due to the weathered slope forming material along the extensive slope and the beds dipping towards valley side.
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
Deban, Namdapha Natonal Park
Miao-Vijyanagar road
 1.  Removal of slided debris material 2. Trimming of crown scar along its length
Debris slide occurred on steep slope due to highly weathered and jointed mudstone and sandstone rocks.