Konyak. A., and Senthilkumar. K. 2017,Macro-Scale (1:50,000) Landslide Susceptibility Mapping in parts of Toposheets nos. 83C/4, 83C/7 and 83C/8,East Jaintia hills, West Jaintia hills and East Kjhsai  districts,Meghalaya
Sonapur mandir 2
NH44
Drain the nala course by constructing chute drain and construction of hill side drain.
Nala which is flowing middle part of the slide and the geological formation is very weak which is fragmented shale. Flowing nala, which is the main cause for this slide. Water percolating through weaker planes and supersaturating the weaker geological fo