Kumar S &  Singh G 2018: Macro-scale (1:50,000) Landslide Susceptibility Mapping in parts of Toposheets 78O/4, O/8, O/11, O/12 & O/16, parts of East Khasi Hills, South West Khasi Hills & South Garo Hills districts, Meghalaya.UnPub. GSI report for FS 2017
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Arwa Slide
Along the way (near) to Arwa cave
chanalising of nala flow is the first step to stop the slide but it is very big and complex slide and connecting Arwa cave so a site specific study is suggested by the preliminary assessment
deep gully erosion by nala , friable sandstone get easily saturated and looses its shear stength and unscientific road cutting initiated the slide