Extensive cut slope due to expansion of the football ground rendered the slope unsatable and oversaturation of the slope forming material (in-situ sil) during heavy rainfall resulted in the landslide incidence. However the slide is of small dimension and
Tep, Y. and Baitha, A., 2020. Macro-scale (1:50,000) landslide susceptibility mapping in parts of Toposheets nos. 78N/8, 78O/1 and 78O/5, Kamrup and Goalpara districts of Assam, West Khasi Hills, Ri-Bhoi and East Garo Hills districts of MGhalaya. Unpubli
The slide is of small dimension and is non threathening
Belahari slide
Belahari village
As the slide do not poss any threat to infrastructure, a simple slope easing to Improve the stability of the slope should be sufficient.
Over-saturation of weak slope forming material comprising thick in-situ soil leading to lose of cohesion and failure. Vertical slope cut with no retaining wall.