Northwire Canada EditionThursday, August 13, 2026
Northwire
PHNM 0.390 +0.0% AWE 0.150 +30.4% FTZ 0.420 +0.0% PLY 0.055 +0.0% AZS 0.710 +0.0% RARE 9.05 +0.0% FOXT 0.165 −2.9% UCU 2.89 −1.0% BEM 0.090 +0.0% MANU 0.250 +13.6% FL 0.430 −5.5% ICM 0.055 +0.0% AMCO 0.355 +0.0% MSR 0.440 +0.0% REVX 1.57 +2.6% SLI 3.39 +0.0% PHNM 0.390 +0.0% AWE 0.150 +30.4% FTZ 0.420 +0.0% PLY 0.055 +0.0% AZS 0.710 +0.0% RARE 9.05 +0.0% FOXT 0.165 −2.9% UCU 2.89 −1.0% BEM 0.090 +0.0% MANU 0.250 +13.6% FL 0.430 −5.5% ICM 0.055 +0.0% AMCO 0.355 +0.0% MSR 0.440 +0.0% REVX 1.57 +2.6% SLI 3.39 +0.0%
Drill Results

Kingfisher identifies porphyry copper system at HWY 37

KFR · Price

Executive Summary

  • Kingfisher Metals identified a new porphyry copper system beneath the existing Hank epithermal Au‑Ag deposits at the HWY 37 project.
  • The redrill (hole HW‑25‑011) intercepted 429 m of continuous copper mineralization from 530 m to the bottom of hole at 959 m depth, extending beyond the planned target depth.
  • All 2025 field work at HWY 37 is complete; crews have been demobilized and a comprehensive suite of mapping, sampling, and geophysical surveys has been logged.

Key Details

  • Hole HW‑25‑011 (Lower Hank porphyry target)
  • Planned depth: 650 m; final depth reached: 959 m.
  • Porphyry‑style alteration and mineralization observed from 530 m to 959 m (429 m interval).
  • Core shows widespread multigenerational veins, disseminated pyrite, chalcopyrite ± molybdenite; high‑grade copper mineralization at bottom.
  • Three zones intersected:

    • 0–530 m: distal low‑temperature quartz‑carbonate alteration, elevated Pb/Zn.
    • 530–900 m: proximal porphyry alteration (quartz‑chlorite‑sericite ± epidote‑pyrite) with high pyrite‑to‑chalcopyrite ratios.
    • 890–969 m: increasing chalcopyrite‑to‑pyrite ratios, early K‑feldspar‑magnetite veins indicating vector toward heat source/core.
  • Geophysical Support (2025 IP Survey)

  • High‑chargeability domains of 30–70 mV/V flank a broader 20–30 mV/V zone, interpreted as pyrite‑rich shell surrounding copper‑sulphide core.
  • Resistivity data show a broad resistive feature consistent with a porphyry intrusive core surrounded by conductive clay alteration.
  • Airborne magnetics reveal an ~1,800 m × 900 m magnetic anomaly aligning with the interpreted porphyry system.

  • Hole HW‑25‑009 (Williams root area)

  • Completed to 761 m (short of 800 m target) after encountering continuous flanking alteration; terminated as projected higher‑grade potassic zone was not intersected.

  • 2025 Exploration Program Completion

  • Drilling total: 7,630 m completed on Sept. 7, 2025.
  • All drill cores logged; samples sent to Bureau Veritas (Vancouver) for assay.
  • Mapping: 84 person‑days.
  • Soil sampling: >750 samples; surface rock sampling: >650 samples.
  • IP geophysics: 30.7 km of line‑kilometres surveyed.
  • Airborne mobile magnetotellurics (MMT): 1,750 km covering ~319 km².
  • LiDAR survey: 256 km² covered.

  • Qualified Person

  • Tyler Caswell, P.Geo., Vice‑President Exploration, qualified under NI 43‑101, reviewed and approved all technical information.

Notable Quotes

“This initial drill test below the extensive Hank epithermal Au‑Ag system encountered a new porphyry copper system… This targeting success is a major advancement in confirming our exploration hypothesis that a large porphyry copper‑gold system is responsible for the broad epithermal Au‑Ag mineralization at Hank on surface.” – Dustin Perry, CEO


Materiality Assessment: Material – Positive (the discovery of a sizable porphyry copper system represents a significant advancement in the company’s exploration model and could materially affect future resource potential).

Read the original news release →

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