Goliath Resources (TSXV: GOT; OTCQB: GOTRF; FSE: B4IF) has released new assays from its 2025 drill campaign at the Surebet Discovery on the 100%-owned Golddigger Property in British Columbia’s Golden Triangle. Results continue to demonstrate strong widths, grades, and continuity across multiple stacked vein sets, further expanding what the company views as a large, robust high-grade gold system.
Key Results:
The standout hole, GD25-377, cut three mineralized intervals within the Bonanza Zone, including:
- 10.25 g/t Au over 7.02 m, within
- 7.16 g/t Au over 10.84 m, within
- 5.20 g/t Au over 15.00 m (true widths)
Additional intervals from the same hole included:
- 1.06 g/t Au over 30.00 m, and
- 8.73 g/t Au over 3.80 m
Other highlights include:
- GD25-332: 13.38 g/t Au over 5.75 m (Goldzilla Vein)
- GD25-380: 6.61 g/t Au over 5.80 m, within 4.83 g/t Au over 8.00 m
- GD25-374: 4.59 g/t Au over 8.00 m, including 8.89 g/t Au over 3.00 m
Goliath notes that all reported intercepts are approximately true width and reflect gold only; Ag-Cu-Pb-Zn assays remain pending.
Drilling has extended the high-grade core by another 80m to the northwest, defining 580m of strike that remains fully open. The mineralized footprint now covers 1.8 km², with exposure across 2.1km of strike and 800m of vertical relief.
The company reports consistent presence of visible gold (VG-NE):
- 2025: 83 of 110 holes (76%) contain VG; assays pending for 80 holes, 62 of which also contain VG
- 2021–2025: 92% of all 386 holes drilled to date show VG
All holes in 2025 intercepted substantial quartz-sulphide mineralization.
The 2025 campaign totalled 64,364m across nine rigs, targeting:
- The potential magmatic “motherlode” source
- Untested Eocene dykes
- Densifying pierce points within Bonanza and Surebet domains
- Expansion of stacked veins laterally and at depth
To date, Goliath has drilled over 156,000 m and >600 pierce points at Surebet.
Roger Rosmus, Founder & CEO of Goliath commented, “The Surebet high-grade gold discovery continues to consistently deliver good assay results, which clearly shows continuity and predictability. Particularly noted by the vast distribution of VG-NE in drill holes spanning an area for over 1,200 metres from northwest to southeast, over 1,000 meters from northeast to southwest and over 800 meters of vertical relief. Within that area are a series of gently dipping stacked veins that dip to the southwest, and another series of gently dipping stacked veins that dip to the southeast. They remain open in the down dip direction of both, suggesting that both could have separate sources feeding each series of stacked veins that would be over 4,000 metres apart. Or one magmatic event that is feeding from either side of it. Equally as impressive are the vertical RIRG dykes coming up through stacked veins, which suggests that there is a magma chamber below the entire mineralized area. At the intersections of the gently dipping veins and the vertical RIRG dykes (called Goldilocks zones) there are two temperature regimes for the VG-NE enriching the zones. Plus, we have found VG-NE within a third rock package with minimal drilling into those zones. Collectively, it is apparent that we are nowhere near the limits of the system, in fact, there is a good chance that we may only be halfway down the various zones with plenty more room to grow the system. Our team looks forward to receiving the assays from remaining holes so we can update the 3D model.”
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