Barkerville Gold Mines Ltd. announced the final drilling results from the 2018 Cow Mountain exploration and category conversion program at the Company's Cariboo Gold Project. A total of 63,970 meters were drilled in 231 holes on Cow Mountain during the 2018 drill program and demonstrated continuity of high-grade gold mineralization within vein corridors and extensions down dip and down plunge. Recent highlights from the Cow Mountain exploration and delineation program include 12.26 g/t Au over 7.60 meters in hole CM-18-206 including high-grade intercept of 97.8 g/t Au over 0.80 meter, located 15 meters up dip of hole CM-18-140 that intersected 37.87 g/t Au over 4.75 meters. The Company is currently working on an updated model to include the additional 231 holes. Selected Drilling Highlights: CM-18-201: 30.16 g/t Au over 2.8 meters; CM-18-206: 12.26 g/t Au over 7.60 meters including 97.8 g/t Au over 0.80 meters; CM-18-211: 105 g/t Au over 0.50 meters; CM-18-220: 7.24 g/t Au over 5.50 meters; CM-18-222: 11.77 g/t Au over 5.00 meters; CM-18-222: 11.08 g/t Au over 6.00 meters; CM-18-227: 46.49 g/t Au over 1.95 meters and CM-18-231: 18.79 g/t Au over 3.95 meters. True widths are estimated to be 50 to 75% of reported core length intervals. Intervals not recovered by drilling were assigned zero grade. Top cuts have not been applied to high grade assays. A drill hole location plan map and section are presented below. Detailed drilling results are presented at the end of this release. The drill program at Cow Mountain was designed to infill and expand high-grade gold-mineralized vein corridors modelled in the May 2018Cow Mountain resource estimate. Vein corridors are defined as a high-density network of mineralized quartz veins within the sandstones. Mineralized quartz veins on the Cariboo Gold Project are overall sub-vertical dip and northeast strike. These corridors have been defined from surface to a vertical depth of up to 300 meters and remain open for expansion at depth and down plunge. Gold grades are intimately associated with vein-hosted pyrite as well as pyritic, intensely silicified wall rock haloes in close proximity to the veins.