High Grade Gold Mineralization with Associated Strong Visible Gold
40.61 g/t Au over 2.6m including 152 g/t Au over 0.6m
Thunder Bay, Ontario--(Newsfile Corp. - June 25, 2026) - Metals Creek Resources Corp. (TSXV: MEK) (FSE: M1C1) (the "Company" or Metals Creek) is pleased to announce diamond drill results for one hole from the recently completed (See News Release: June 11, 2026) three hole diamond drill program at the Ogden Gold Project located in Timmins, Ontario. The Ogden Gold Project (See Fig 1) is a 50/50 Joint Venture with Discovery Mining Ltd. ("Discovery"), with the Company serving as the operator.
This program entailed 3 diamond drill holes totaling 1233 meters(m) targeting the lower portion of the Thomas Ogden Zone (TOG) fold structure which has a shallow easterly plunge. TOG is host to gold bearing flat lying quartz bearing/siliceous secondary structures as well as strongly altered conglomerates and felsites. The altered conglomerates and felsites host pyrite +/- arsenopyrite and local visible gold. High-grade gold mineralization within TOG has a strong preferential association with the TOG fold axis.
Drilling Highlights Include:
40.61 g/t Au over 2.6m including 152 g/t Au over 0.6m (TOG-26-75)
Broad zone of mineralization with 8.43 g/t Au over 13.25m (See Table 1)
Footwall felsic dike returned 0.58 g/t Au over 7.95m
TOG-26-75 returned a downhole intercept (326.60 - 329.20m) of 40.61 grams per tonne (g/t) gold (Au) over 2.60 meters (m) including 0.60m (326.6 - 327.20m) of 152 g/t Au, with strong visible gold (See figure 2). A broad zone of mineralization (See Table 1) including lower grade material returned a downhole intercept of 8.43 g/t Au over 13.25m. This hole (See Schematic Cross Section Fig. 1) was designed to further define the down-plunge extent of the high-grade gold mineralization associated with TOG fold structure as well as test an area of the fold structure with limited data and no documented visible gold. VG was hosted within a highly silicified felsite unit with associated cross-cutting quartz veinlets within hairline fractures. Mineralization consists of finely disseminated pyrite with associated strong silicification and local fuchsite. The Timiskaming conglomerate which hosts the felsite are strongly altered with pervasive albitization, abundant cross cutting quartz-carb veins and associated pyrite. As shown on Fig. 1, the TOG fold axis is conducive to hosting higher grade gold mineralization. Felsic dike at lower ultramafic contact returned a downhole intercept of 0.58 g/t Au over 7.95m with associated pyrite and silicification.