The deep rotational debris slide occurred due to weathered SFM along steep slope. Thick unit of weathered carbonaceous shale occupies the lowermost part of exposed slope cut and makes the overlying rocks unstable. Also, pore pressure of SFM increasing du
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
3.7 km SE of Sanliam
Khonsa-Lazu road
1. Construction of gabion wall 2. Stabilize the slope with bench marks 3. Removal of debris material from the drainage in order to avoid excess infiltration.
1. Slope forming material is intercalation of carbonaceous shale –siltstone of Barail Group. The lower part of the exposed slope cut occupied by thick unit of weathered carbonaceous shale makes the overlying rocks unstable 2. Landslide occurred along t