The 2026 program represented the first systematic deep test of the geological model beneath and surrounding the former Brewer mine.
Three deep holes were completed under Carolina Rush’s earn-in agreement with OceanaGold. The drilling confirmed a kilometer-scale hydrothermal system characterized by strong alteration, locally developed porphyry-style veining and chalcopyrite-bearing copper mineralization.
Importantly, the program provided new geological vectors indicating that the potential centre of the copper-gold system may lie west-northwest of the historic Brewer mine, where drilling remains limited.
Highlights from the 2026 Drill Program
Hole B26C-037
Confirmed a vertically extensive hydrothermal alteration system and encountered copper mineralization, including chalcopyrite, together with locally developed porphyry-style veining.
Hole B26C-038
Provided additional geological information on alteration and mineralization within the broader Brewer hydrothermal system.
Hole B26C-039
Drilled approximately 400 metres southeast of Hole 37 and west of the former Brewer mine, Hole 39 intersected significant gold-copper mineralization and demonstrated that the Brewer epithermal system extends into an area that had not previously been tested by drilling.
Taken together, the three holes strengthened Carolina Rush’s interpretation of a shallow northwest-dipping alteration system and helped focus future exploration toward the west-northwest.