The shallow rotational debris slide occurred due to increase of pore water pressure man slide37.infall l nt)ionf osed of weathered shale of Disanf Group with d sidle. in weak slope forming material due to oversaturation during heavy 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
500m NE of Yanman
Changlang-Khimioyng road
Removal of slided debris material on the road side.
Weak slope forming material predominantly composed of weathered shale with soil 2.Increase of pore water pressure man slide37.infall l nt)ionf osed of weathered shale of Disanf Group with d sidle. in the slope forming material due to oversaturation durin