Golden Predator Mining Corp. announced the results from the final 16 of 32 reverse circulation drill holes from the 2020 work program at its licensed 100%-owned Brewery Creek mine project located approximately 55 km by road from Dawson City, Yukon. A total of 32 reverse circulation drill holes, totaling 3,706 m, were completed between the Golden and Lucky resource areas in the fall of 2020. The 2020 program was designed to infill within and around two fences of 2019 drilling that encountered mineralization along a 400 m gap where there had been no previous drilling between the Golden and Lucky resource areas. The objective was to establish sufficient drill density in this 400 m gap to be able to incorporate the Lucky resource into the greater Keg pit shell. The gold assays for the remaining 16 drill holes of the program are reported in this release with significant thicknesses of gold mineralization present in 14 of the 16 of the drill holes. The two drill holes not intersecting mineralization were not completed to target depth. The collars of 8 of the drill holes are located outside of the current Golden resource area and the other 8 are located on the southwestern margin of the current Golden resource area. Other significant mineralized intervals include 7.62 m of 2.68 g/t gold from a depth of 102.11 m in drill hole RC20-2700 and multiple intercepts in drill hole RC20-2707 including 9.14 m of 0.58 g/t gold from a depth of 42.67 m and 13.72 m of 0.57 g/t gold from a depth of 70.10 m. Gold mineralization is controlled by fractures oriented sub-parallel to the main thrust fault and a series of high angle conjugate fractures developed within main zone. Composite mineralized intercepts thicknesses range from 6.10 m to 45.72 m with an average composite mineralized thickness of 26.05 m in the 11 drill holes that had full intersections across the mineralized zone. Mineralization encountered in these 16 holes consists of sulfide, transitional and lesser amounts of oxide material. Within the area of this drilling the eastern strike extension of the mineralized zone is not yet defined, and the zone remains open at depth down dip. Three reverse circulation drill holes, totaling 687 m, were completed in 2020 targeting newly defined extensions of the Classic/Lone Star porphyry-style mineralization. The drill holes were widely-spaced step- out holes drilled at significant distances from any existing drilling at the Classic and Lone Star areas. Two of the drill holes (RC20-2710 and RC20-2711) were located approximately 500 m from each other and 650 m southeast of the closest previous drilling within the Classic and Lone Star areas. No significant gold was intersected in either drill hole. The third drill hole (RC20-2712), located approximately 1,330 m to the east of the nearest previous drilling, tested a coincident aeromagnetic and radiometric anomaly indicating a structural zone along the margin of a biotite monzonite intrusive within an area of spotty gold and arsenic in soil geochemistry. This initial test was encouraging with gold intersected in two intervals of monzonite with 0.33 g/t gold over 1.52 m at a depth of 120.40 m and 0.27 g/t gold over 1.52 m at a depth of 131.06 within a 15.29 m zone of anomalous mineralization. Mineralization within the zone consists of pyrite with local arsenopyrite associated with chlorite and calcite alteration minerals. Continuing exploration will develop extensions to the Classic and Lone Star area mineralization, a near surface bulk tonnage target that lies approximately 3 km south of the Brewery Creek Reserve Trend. Together with the Lone Star zone, the Classic zone demonstrates the discovery potential of the entire southern portion of the large Brewery Creek property where a large syenite intrusion hosts gold mineralization primarily in sheeted quartz/carbonate/pyrite veins and as fine-grained disseminations. Initial column leach tests have indicated that this intrusive hosted mineralization is leachable to at least a 200 m depth. This mineralization is clearly a separate younger mineralizing event not associated with the quartz monzonite, thrust fault hosted, mineralization historically exploited in the Reserve Trend which is the subject of the ongoing bankable feasibility study.