Metallic Minerals Corp. announced additional high-grade results from the 2018 exploration programs conducted at its 100% owned McKay Hill Project, located 50 kilometers north of the historic Keno Hill Silver District in the Yukon Territory, and adjacent to ATAC’s Rackla property. Although earlier stage than the Company’s Keno Silver Project to the south, Metallic see’s similar potential for a district scale high-grade silver-lead-zinc-copper system at McKay Hill based on results to date including: Total of 37 vein structures identified on the property to date, with the discovery of 18 new silver-lead-zinc-rich structures in 2018, with 61 samples ranging 1,000 to 4,326 g/t silver equivalent; The outline of six kilometer-scale areas of highly elevated silver, lead, zinc, copper and gold in soils and rock sampling; and Advancement of the Central Zone targets to drill-ready stage along with demonstration of the potential to host bulk-tonnage mineralization. The McKay Hill Project occurs within a belt of silver-lead-zinc related deposits that stretches from the Alaska border to the southern part of the Yukon and includes the famous Keno Hill Silver District. McKay Hill was discovered in the 1920s and had production in the 1940s of high-grade material from the No. 6 Vein Corridor grading 390.8 g/t Ag and 74.1% Pb. With at least 37 vein structures (including the 18 new structures discovered in 2018) which have only seen limited exploration, the area shows potential to host a significant district-scale vein system similar to Keno Hill. The Central Zone was the focus of historic exploration, and production occurred from a small area of the No. 6 Vein within the Central Zone. Exploration work in 2018 has substantially expanded the number of the Central Zone vein exposures, and understanding thereof, resulting in the identification of high-quality targets for drill testing. Importantly, this year’s program has demonstrated that the historically productive No. 6 Vein is part of a much larger system of vein structures than had been previously recognized, now termed the No. 6 Vein Corridor. At least 20 major north-northeast-trending vein structures have been identified in the Central Zone along with northeast-trending stockwork zones in what is now interpreted to be a >1 kilometer-long by 250-metre-wide mineralized corridor that remains open to expansion at both ends. In addition to the work on the Central Zone, exploration on the surrounding areas included the West McKay, Bella, Falls, Red, Independence, Snowdrift, Nash and White Hill targets. Work in these target areas focused on systematic soil grid sampling, along with rock sampling within the identified zones of interest. Results of the 2018 field program have revealed more than a dozen newly discovered vein structures in new areas for follow with seven rock samples returning greater than 500 g/t Ag equivalent values.