Geologically, the terrain comprises thick strata of weathered muscovite schist with core stones precariously resting on the slope. Excavated slope exceeding the critical angle along with weak overburden material and drainages on the hillslope played a vi
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
The slide is enlarging in distribution wise. Proper implementation of remedial measures is recommended.
NH 13 Slide 22
NH 13/ NW of Milumkang
1. Removal of unstable blocks of rock from the slope. 2. Systematic channeling and diversion of surface water runoff away from the depleted slope. 3. Proper maintenance of lined hillside drain. 4. Construction of retaining wall for toe support with prope
1. SFM: Slope is predominantly covered by thick strata of overburden material composed of highly weathered rock with blocks/ boulders of muscovite schist within. 2. Hillslope is moderately dissected by drainages. 3. Oversaturation of slope material and l