The slide ois shallow translational rock slide triggered due to slope cut and rainfall during monsoon.The overburden material is predominantly composed of highly fractured sandstone belonging to Gondwana Group of rocks. Moderate dissection of slope by dr
Kikon, A., and Jamir, I., 2021: Remote sensing based macro-scale (1:50,000) landslide susceptibility mapping in Toposheets 78M/9, M/10, M/11, M/13, M/14, M/15, 83A/2, A/3, A/4, A/7, A/8, A/11, A/12, 83B/1, B/5 & B/9 covering  parts of Tawang, West Kameng
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Pinjori-Kimi Road Slide 2
Pinjori-Kimi Road
1. Proper diversion of drainages to systematic drainage system 2. Regrading of slope to gentler angle 3. Removal of detached and loose blocks from the affected slope 4. Construction of retaining wall combined with post plate wire net system to arrest the
1. SFM: Slope material is composed of highly fractured parent rockmass (sandstone) 2. The affected slope has moderate drainage dissections on  both flanks of the slide and within the slide