This landslide was due to Extensive cut slopeting and slope made of highly weathered sandstone and shale which failed during incessant rainfall aided with gully formation.
Yadav, S., Mohanty, A., Kandpal, J., 2020. Macro-scale (1:50,000) Landslide Susceptibility Mapping in Toposheet No. 83 D/11 and in parts of Toposheet Nos. 83 D/6, 7 & 10 in Hailakandi and Karimganj districts of Assam, Kolasib and Mamit districts of Mizor
NA
Nishkar slide
Mahapur
Slope angle may be reduced and Vegetation cover may be applied.
Extensive cut slopeting and removal of vegetation, slope made up of weathered shale and sandstone, gully formation and over-saturation during incessant rainfall.