This landslide was due to Extensive cut slopeting making the slope unstable and made of weathered sandstone which during incessant rainfall failed.
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
Barthal slide
Bilaipur
Slope angle may be reduced and Vegetation cover may be applied.
Extensive cut slopeting rendered the slope vertical and unstable, loss of cohesion during incessant rainfall.