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Provenance Gold Intersects 0.8 g/t Gold over 154.23m from Surface Including 3.02 g/t Gold over 13.72m

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Highlights

  • EC-02 assayed 0.51 g/t Au over 156.4m from surface and EC-03 assayed 0.8 g/t Au over 154.23m from surface including 3.02 g/t Au over 13.72m.

  • Reinforces the NE-SW mineralized structure previously discovered in ED-04 as a significant gold bearing structure in the Tyee Area, confirming the high-grade zone is over 25m in true thickness within a broad mineralized zone, and remains open in all directions.

  • The assay results support the model of the interpreted mineralized structures as coherent and open along strike and at-depth.

Vancouver, British Columbia--(Newsfile Corp. - February 28, 2025) - Provenance Gold Corp. (CSE: PAU) (OTCQB: PVGDF) (the "Company" or "Provenance") is pleased to report assay results for EC-02 and EC-03 at its Eldorado Gold Project in Malheur County, Oregon. EC-02 and EC-03 tested the NE-SW mineralized structure previously discovered in ED-04 in the Tyee Area. (see press release dated July 18, 2023).

  • Hole EC-02 intersected 156 meters that assayed 0.501 g/t gold including 32 meters of 0.94 g/t gold.

  • Hole EC-03 intersected 154 meters of 0.8 g/t gold, including 13.7 meters that assayed 3.02 g/t gold and 12.2 meters containing 2.57 g/t gold, which represent new high-grade zones. This newly recognized higher-grade area is open both down dip and in both directions.

The results from EC-02 and EC-03 are consistent with the presence of the broad mineralized zone found in RC hole ED-04 and support the model that the NE-SW mineralized structure is a significant gold bearing structure, punctuated with multiple higher-grade intervals approximately 25m in true thickness (Figures 1-2). The mineralization remains open in all directions.

As part of its maiden 2024 three-hole core drilling program, the Company drilled holes EC-02 and EC-03 (HQ) to depths of 156.4 meters and 200.6 meters, respectively. Drill equipment issues and difficult drilling conditions through the heavily faulted, fractured, and brecciated zones in this area resulted in significant loss of core and both holes were unable to reach the intended target depth. Given the nature of the core loss, it is suspected that the assay results from EC-02 and EC-03 underrepresent the coarse gold fraction that was seen in ED-04. The strongest gold values are typically associated with gold and pyrite fracture coatings in the heavily fractured and sheared host diorite. Further, around holes ED-04, EC-02 and EC-03, the breakage and core loss were preferentially along the mineralized fractures associated with the weakest and most erodible rock that hosts the majority of the gold mineralization, based on observation and historic studies.