The shallow planar rock slide due to anthropogenic activity. The weathered shale overlain by siltstone is exposed along the slope. The unstable shale is not supporting to siltstone hence, the jointed siltstone with debris material slided during the rainf
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 Longvi
NH-315, Jairampur-Manmao road
1. Removal of slided material. 2. Construction of toe support retaining wall with sufficient weep holes.
1. Toe cutting of the slope for road construction. 2. The weathered shale overlain by siltstone is exposed along the slope.