The landslide has occurred because of Extensive cut slopeting and slope made up of highly weathered sandstone  which under the influence of rainfall got 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
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Lala Chaura Bagan slide
Lala Chaura Bagan
The slope stabilization may be carried out by reducing the slope angle and plantation of small plants.
Destabilization of natural slope comprising highly weathered sandstone due to extensive cutting and and loss of cohesion during incessant rainfall.