Spanish Mountain Gold Provides 2024 Drill Program Update with Initial Results that Confirm Mineralization Extensions

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Vancouver, British Columbia--(Newsfile Corp. - October 16, 2024) - Spanish Mountain Gold Ltd.  (TSXV: SPA) (FSE: S3Y) (OTC Pink: SPAZF) (the "Company" or "Spanish Mountain Gold") is pleased to provide an update on its 2024 drill program at the Spanish Mountain Gold project located in the Cariboo Gold Corridor, British Columbia, Canada (see Figure 1 - Project Location Map). The Company completed 11 NQ-sized diamond drill holes for a total of 5,590 metres ("m") of drilling, positioned along the northwestern edge of the deposit. Results from the first reported hole in this program, 24-DH-1267, successfully intercepted its intended targets, confirming near surface mineralization and providing valuable information to improve the understanding of mineralization extensions on three horizons and their associated controls.

Highlights:

  • Upper Intercept - Hole 24-DH-1267 intersected 80.00 m grading 0.44 g/t Au (from 53.00 m to 133.00 m), including 22.50 m grading 0.74 g/t Au (from 110.50 m to 133.00 m).

  • Middle Intercept - Hole 24-DH-1267 intersected 91.50 m grading 0.22 g/t Au (from 284.50 m to 376.00 m).

  • Lower Intercept - Hole 24-DH-1267 intersected 8.50 m grading 0.67 g/t Au (from 518.00 m to 526.50 m), and 41.00 m grading 0.19 g/t Au (from 567.50 m to 608.50 m), within sericite-altered rocks bearing pyrite and quartz veins in proximity to a NS- trending fault.

  • Hole 24-DH-1267 ended in mineralization at a depth of 652.50 m, with preliminary results of 14.35 m grading 0.23 g/t Au (from 638.15m to 652.50 m).

  • See Figure 2 - Plan View and Long Section, 2024 Drill Program

Julian Manco, Spanish Mountain Gold's Director, Exploration, commented, "These early results provide valuable insights that help further validate the new geological model of the deposit and its potential for extended mineralization to the northwest. Notably, the presence of gold associated disseminated blebby pyrite in quartz-bearing cataclastic argillite in the upper zone appears to be a promising indicator of newly interpreted mineralization in this upper part of the deposit.

In the middle intervals, the findings align with the new 3D structural interpretation, which highlights a strong spatial relationship between mineralization and west-dipping, north-south-oriented faults (e.g., Fault 1, see Fig. 2). Furthermore, a newly identified mineralized zone at depth shows a similar relationship with another NS-oriented fault (e.g., Fault 2, see Fig. 2), coupled with local intense sericite alteration and quartz veining in the tuffaceous rock. These characteristics have similarity to high-grade gold intervals elsewhere in the deposit, suggesting further mineralization potential within several host lithologies.