The shallow rotational debris slide occurred due to weathered SFM along the slope. This loose and unconsolidated SFM slided 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
1.7 km SW of Lazu
Khonsa-Lazu road
1.Moderation of slope 2. Provision of lined drainage along the road section.
Weak slope forming material predominantly composed of intercalation of weathered fine grained sandstone, siltstone and shale of Barail Group intermixed with soil.