This landslide was due to Extensive cut slopeting and slope made of highly weathered sandstone which failed during incessant rainfall.
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
Lalpani slide
NH - 154
Slope angle may be reduced and Vegetation cover may be applied.
Extensive cut slopeting, slope forming material comprises highly weathered sadstone, over-saturation and loss of cohesion of slope material during incessant rainfall.