Achan Konyak et al., 2016. Macro-scale (1:50,000) landslide susceptibility Mapping in parts of toposheets no. 83C/2, C/3, East Khasi Hills, West Jaintia Hills and Karbi Anglong, Meghalaya and Assam. Unpub. GSI report of FS 2015-2016.
a first order streams originates in the road turning where slide has initiated.
2 km SW of Jowai
Construction of flexible retaining wall with sufficient height and weep holes. Construction of road side drainage and proper maintenance.
Easing of the slope on both the flanks of the slide.



Highly fractured and jointed rockmass overlain by veneer of soil. Due to incessant rain fall cause the devolvement pore pressure between the interference of soil and rock.