Aztec Minerals Corp. reported assay results for an additional four holes, TR21-11 to 14, from its now completed 2021, Phase 2, 23-hole, 2,716 metre reverse circulation (RC) drill program on the Tombstone project which covers most of the historic Tombstone silver mining district in southeastern Arizona. The four holes were drilled on two fence patterns to step out to the south from prior drill fences reported previously in the north-central part of the Contention open pit. Every one of the four holes intersected near surface, oxidized gold-silver mineralization, and all four holes bottomed in mineralization. Gold equivalents are calculated using a 70:1 silver: gold ratio. Reported lengths are apparent widths, not true widths. The gold - silver mineralization zones are generally west dipping at around 60-80 degrees, associated with the quartz-feldspar porphyry dikes. However, these dikes also extend at shallow angles out from the Contention fault along fold noses in the Bisbee clastic sediments so the full range of mineralization dips vary from 20 to 80 degrees. True widths for the apparent mineralization intersection widths of the four holes approximately range from 20 to 100% of the apparent widths, with the norm for the mineralized true widths being 60 to 100% of the apparent widths. All 4 holes intersected extensive gold and silver mineralization, see assay intervals in the table below, extending the mineralized zones at depth and along strike, below and west of the Contention open pit. Two of the four holes also intersected old mine workings, likely dating back to the late 1800's, indicating that some of the highest-grade bonanza mineralization in the area drilled was previously mined. The drilled area is on the west side of the Contention Pit, adjacent to the area drilled in 2020 near the centre of the pit (central drill pattern), and measures at least 50 meters north to south along strike by up to 150 meters east-west, perpendicular to the west dip of the Contention mineralized structure, with gold- silver mineralization still open in all directions. The drilled area reported herein demonstrates mineralization over a combined length of 420 meters from the 2020 and current drilling. Holes TR21-17 to 23 have been completed and sampled and each hole intersected similar widespread alteration and mineralization. The total area drilled in 2021 spans 520 m long by over 150 m wide and to maximum depths of 175 m. Final results are pending. The low sulfidation epithermal gold-silver mineralization observed to date is impressive, marked by hydrothermal breccias, quartz veining and silicification associated with quartz-feldspar porphyry dikes and moderate to strong potassic, argillic and advanced argillic alteration and hornfels within the host Bisbee sandstones and siltstones. Areas of intense hematite, goethite and manganese wad are extensive, associated with quartz-calcite veins and localized skarn alteration in limestones. Cerargyrite (silver chloride) is observed in fractures, often with fine-grained visible gold. Most silver and gold mineralized zones intersected in the 2020 and 2021 drill programs are proximal to and in the hanging-walls and footwalls of old underground mine workings.