This landslide was due to quarry activity for sand mining. The slope composed of weathered sandstone and quarry activity without taking proper slope stabilisation measures the slope 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
Dwarbond- Bilaipur slide
Dwarbond- Bilaipur road
Slope trimming may be done to reduce the slope angle and plantation of small grasses.
Excessive slope cutting for local mining of sand lead to slope instability. Due to negative slope formation and exposure, it failed during incessant rainfall.