Kingfisher Provides Update on Drill Program at HWY 37 Project, Golden Triangle

About this update from Kingfisher Metals Corp

Kingfisher Provides Update on Drill Program at HWY 37 Project, Golden TriangleVANCOUVER, BC / ACCESS Newswire / July 31, 2025 / Kingfisher Metals Corp. (TSXV:KFR)(FSE:970)(OTCQB:KGFMF) ("Kingfisher" or the "Company") is pleased to provide an update on the previously announced 7,500-meter ("m") drill program at the HWY 37 Project. Drilling at Williams has extended potassic alteration with chalcopyrite and bornite mineralization by ~150 m below the limits of historical drilling. Bornite is mapped at surface and identified to a vertical depth of approximately 680 m in drill core. HW-25-004 intersected a broad zone of intense potassic alteration over 478 m. The 849 km 2 HWY 37 Project is located within the Golden Triangle, British Columbia.Drilling to date has focused on testing for depth extensions of the Williams porphyry Cu-Au system, porphyry Cu-Au targets across the valley (east) in an area with no historical drilling, and at the Upper and Lower Hank porphyry Cu-Au targets (Fig. 1).Dustin Perry, CEO, states "So far, the 2025 drill program has matched our expectations of vertically extending porphyry mineralization at Williams as well as providing a much clearer understanding of this highly prospective district. Our exploration hypothesis indicates vertical continuity of the gold-rich bornite zone, and these holes demonstrate that bornite continues to depth where it was predicted." Figure 1: Hank-Williams Drill AreaWilliams Area DrillingThe first drill hole of the program, HW-25-001, was completed upslope and west of potassic alteration and drilled steeply to the east. The drill hole was collared at a 110 o azimuth and -80 o dip, designed to test the western limit of the porphyry system and provide important data to define the orientation of the mineralized system at Willams. The drill struggled passing through several fault zones and deviated clockwise significantly more than historical drill holes in the region ending approximately 40 o azimuth from the planned target. Despite this, HW-25-001 intersected potassic alteration, often overprinted by phyllic alteration with chalcopyrite ± bornite mineralization from 390 m726 m (Fig. 2 and 3), end of hole was at 803 m and bottomed in early mineral monzanite. This drill test provided valuable insights to the mineralized system at Williams including identifying two porphyry intrusive phases that were previ...

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