It is a shallow rotational debris slide triggered by incessant rainfall. Infiltration of surface water runoff due to rainfall along the weak slope forming material attributed to the slope failure
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
800 m S of Bonia
Longding-Konsa road
1. Construction of hill side road drains.  2. Modification of slope angle.
Weak slope forming material predominantly composed of intercalation of siltstone and shale of Disang Group intermixed with soil.