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 the 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
Yanman slide
Changlang-Khimioyng road
1. Removal of slided debris material 2. Construction of retaining wall along the affected road stretch. 3. Construction of lined hill side road drainage with proper gradient
1.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 dur