Kingfisher Metals Confirms Early Jurassic Porphyry Mineralization Across Hank-Mary District, a Fertile Window Between Mitchell Cu-Au and Brucejack Au-Ag Deposits

Multiple U-Pb and Re-Os dates between 190–186 Ma establish that the Hank-Mary district formed within a minimum 4-million-year period during a key regional gold-rich mineralization window.  The closest age porphyry deposit is Mitchell (KSM), the largest Cu-Au porphyry deposit in Canada and the closest age epithermal deposit is Brucejack Au-Ag.

Kingfisher Metals Corp. (TSX-V: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher” or the “Company”) is pleased to announce new U-Pb zircon and Re-Os molybdenum geochronology results from the Hank-Mary district on its 933 km² HWY 37 Project, Golden Triangle, British Columbia. The initial results demonstrate that magmatic-hydrothermal activity across the Hank-Mary district is part of highly fertile and gold-rich mineralizing time in the region. These dates overlap with established ages for the Mitchell porphyry deposit at the nearby KSM project, the largest undeveloped Cu-Au porphyry deposit in Canada and is close to the age of the Brucejack epithermal Au-Ag deposit (Table 1 & Figure 1 – 3).

Key Highlights:

  • Similar age as Mitchell Cu-Au porphyry deposit:  Porphyry mineralization at Hank, Williams & Mary (~190–186 Ma) overlaps with the Mitchell deposit (~196–189 Ma).
  • Similar timing to Brucejack Au-Ag epithermal deposit: Epithermal gold mineralization at Hank (~188-184 Ma) ties closely with the Brucejack deposit (~184–183 Ma).
  • One large system: Ages from Hank, Mary, and Williams all fall within the same range, suggesting a single, large mineralizing system that defines the district.
  • Geological age as a fertility indicator: These ages match the Early Jurassic Texas Creek intrusive suite of rocks, known for hosting major porphyry deposits in the Golden Triangle. 

Dustin Perry, CEO and President of Kingfisher, states, “These initial geochronology results validate our exploration model and confirm our belief that the Hank–Mary district represents a large, fertile porphyry system. The confirmation that mineralization across Hank, Mary, and Williams falls within the same Early Jurassic window as the Mitchell and Brucejack deposits highlights strong parallels to two of the most significant gold-rich systems in Canada.”

Figure 1: Regional map of the Golden Triangle showing the location of Kingfisher’s HWY 37 Project (Hank district) relative to Seabridge Gold’s KSM Project (Mitchell deposit) within the Sulphurets District.[1]

Geochronology Results

Two complementary dating methods applied across the Hank district from three studies:

U-Pb zircon geochronology constrains the crystallization age of host intrusions, the timing of magma emplacement, and is performed on zircon mineral separates from intrusive rock samples.

Re-Os molybdenite geochronology directly dates ore-forming hydrothermal events by measuring the radioactive decay of rhenium to osmium in molybdenite (MoS₂), a common porphyry mineral. Molybdenite often precipitates from later-stage hydrothermal fluids during mineralization, Re-Os ages are interpreted to reflect the youngest ages of porphyry mineralization. The results in Table 1 present new data from the British Columbia Geological Survey research by Roddy Campbell presented at Rock Talk 2026[2], new data from Kingfisher Metals and includes one previous result from the Williams deposit.

Table 1: Geochronology results from the Hank porphyry district, HWY 37 Project. Ma = million years ago.

AreaDrillholeMethodAge (Ma)Error (Ma)Source
Mary PorphyryBC07-10U-Pb zircon*190.1±0.024*Preliminary Result; Campbell, 2026
Mary PorphyryBC07-10Re-Os Mo186.3±0.76Campbell, 2026
Hank PorphyryHW-25-011Re-Os Mo187.7±1.1Kingfisher Metals, 2026
Hank PorphyryHW-25-006Re-Os Mo188.0±1.1Kingfisher Metals, 2026
Williams Porphyry188Friesen, 2020[3]

Figure 2: Hank district map showing porphyry centres (Hank, Mary, Williams) with geochronology sample locations and dates.

Interpretation: District and timing relative to the Mitchell and Brucejack deposits

District Scale

The similar-age results across Hank, Mary, and Williams (~190–186 Ma) are consistent with a district-scale magmatic centre capable of generating multiple porphyry deposits, analogous to the multi-phase, multi-centre architecture of the world’s largest porphyry districts.

Figure 3: Major magmatic and mineralization age groups in the Golden Triangle region (after Campbell, 2026, British Columbia Geological Survey). Hank-Mary and KSM data shown for comparison.

Mitchell

The Mitchell deposit (KSM project) has an interpreted span of mineralization ~192 to 190 Ma with youngest magmatism ending around 189 Ma[4]. Early results from the Hank district indicate porphyry mineralization is between 190 and 186 Ma, with overlap in age with the Mitchell porphyry. Mitchell is the closest in age porphyry system in the region, located approximately 75 km from Hank, and is Canada’s largest undeveloped Cu–Au deposit. This time window is considered highly prospective.

Brucejack

Epithermal gold at Hank emplaced after ~188 and before 184 Ma[5].  This timing ties closely with the nearby Brucejack deposit, where epithermal Au – veins are formed between 184-183 Ma[6]. Brucejack is the only known system in the region with this timing, making it a strong analogue for Hank. However, more work is needed to better define the exact age of gold mineralization at Hank.

Background: Geological Age and Porphyry Fertility

New and recently published geochronology places the Hank district in one of the most fertile periods in BC, between Mitchell porphyry (KSM) and Brucejack epithermal Au-Ag deposits. Within these prospective time windows in the region, multiple deposits can be mineralized simultaneously across a large district that is fed by a common district-scale magmatic hydrothermal system.

Geological age is a powerful predictor of porphyry copper-gold and epithermal Au-Ag fertility. In the Golden Triangle of northwestern British Columbia, some of the most significant Cu-Au porphyry deposits and epithermal Au-Ag deposits which include the world-class KSM system and nearby Brucejack deposit are genetically linked to Early Jurassic (~196–185 Ma) Texas Creek magmatism (Figure 3).

Qualified Person

Technical aspects of this news release have been reviewed, verified, and approved by Tyler Caswell, P.Geo., Vice President Exploration of Kingfisher, who is a qualified person as defined by National Instrument 43-101 – Standards of Disclosure for Minerals Projects.

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 136,727,344 shares outstanding.

For further information, please contact:

Dustin Perry, P.Geo.
CEO and Director
Phone: +1 778 606 2507
E-Mail: info@kingfishermetals.com    

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

Mineralization hosted on adjacent and/or nearby properties is not necessarily indicative of mineralization hosted on the Company’s property. This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur.

Forward-looking statements in this news release include, among others, statements relating to  the interpretation that geochronology results from the Hank-Mary district indicate a district-scale magmatic-hydrothermal system with porphyry mineralization ages (~190–186 Ma) overlapping those of the Mitchell Cu-Au and Brucejack Au-Ag deposits, suggestive of a similarly fertile mineralizing environment capable of hosting multiple porphyry deposits; and statements regarding planned exploration on the HWY 37 Project. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; domestic and foreign laws and regulations could adversely affect the Company’s business and results of operations; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance.

The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.


[1] KSM (Seabridge Gold) Seabridge Gold Inc., News Release dated March 31, 2026: “Seabridge Gold Provides Updated Mineral Resource Estimates for KSM Project.” Effective date of estimate: March 30, 2026. The MRE was prepared by independent qualified persons in accordance with NI 43-101.

Treaty Creek (Tudor Gold / Teuton) Tudor Gold Corp., News Release dated January 22, 2026: “Tudor Gold Announces Updated Mineral Resource Estimate for Treaty Creek Project.” Effective date of estimate: November 30, 2025.

Brucejack (Newmont) Newmont Corporation, News Release dated February 2026: “Newmont Announces 2025 Year-End Mineral Reserve and Resource Estimates.” Note: Newmont does not separately disclose deposit-level M+I+Inferred resource tables by category in their press release — the full technical disclosure is in Newmont’s Annual Information Form (AIF) and the supporting NI 43-101 Technical Report on file with SEDAR+.

Snip (Skeena Resources) Skeena Resources Ltd., News Release dated September 5, 2023: “Skeena Resources Delivers Updated Mineral Resource Estimate for the Snip Gold Project.” Effective date of estimate: September 5, 2023.

Bronson Slope (Seabridge Gold) Seabridge Gold Inc., News Release dated June 27, 2024: “Seabridge Gold Reports Mineral Resource Estimate for Bronson Slope.” Effective date on estimate: June 25, 2024.

Snip North (Seabridge Gold) Seabridge Gold Inc., News Release dated April 15, 2026: “Seabridge Gold Announces Maiden Mineral Resource Estimate for Snip North.” Effective date of estimate: April 15, 2026.

[2] Campbell, R.W., Gibson, K., Horvath, O., and van Straaten, B.I. (2026, February 17-19th). A framework for Late Triassic to Early Jurassic plutonism in the central Golden Triangle [Conference presentation]. Smithers Exploration Group ‘Rock Talk’ 2026 Smithers, BC, Canada.

[3] Friesen, O., 2020. 2019 Drilling and Geochemical Report on the Hank/Ball Creek Property, Located in the Liard Mining division, British Columbia, Assessment Report 38858 for Ministry of Energy and Mines, BC Geological Survey.

[4] Febbo, G. E., Kennedy, L. A., Nelson, J. L., Savell, M. J., Campbell, M. E., Creaser, R. A., Friedman, R. M., van Straaten, B. I., & Stein, H. J. (2019). The evolution and structural modification of the supergiant Mitchell Au-Cu porphyry, northwestern British Columbia. Economic Geology, 114(2), 303–324

[5] Kaip, A. W. (1993). Geology and alteration zonation of the Hank property, northwestern British Columbia (104G/1, 2) (M.Sc. thesis, University of British Columbia). Mineral Deposit Research Unit, University of British Columbia

[6] Board, M. et al. (2020), Geochronology of magmatism and epithermal gold mineralization at the Brucejack deposit, northwestern British Columbia, Economic Geology.

Kingfisher Outlines New Porphyry Target 6 km from Highway and Power, HWY 37 Project, Golden Triangle

Kingfisher Metals Corp. (TSX-V: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher” or the “Company”) is pleased to report the delineation of a new porphyry drill target at the Turquoise target area (Figures 1-3). Interpretation of recently updated geophysical inversion datasets1 highlight a compelling subsurface target within the Company’s 933 km² HWY 37 Project, located in the Golden Triangle, British Columbia.

Key Highlights:

  • New near-surface porphyry copper – gold target identified at the Turquoise target area characterized by a 0.5 by 2.0 km chargeability anomaly. The magnetic vector amplitude inversion (MVI), direct current (DC) resistivity and the Mobile MagnetoTellurics (MMT) resistivity datasets all support the core target domain (Figure 2).
  • Majority of target area is covered by a landslide and glacial till, interpreted to cover the core porphyry alteration target with only discrete lateral alteration expressions at surface (Figure 1).   
  • Porphyry proximal indications include advanced argillic mineralogy (dickite and vuggy silica) on surface and high pyrite abundance near geophysical core target domain (Figure 1).
  • Target is near-surface and drill ready.

Dustin Perry, CEO of Kingfisher, states, “The Turquoise target is a direct result of our systematic exploration approach, which continues to unlock new opportunities across this underexplored yet highly prospective region of the Golden Triangle. The target is located within the emerging Hank–Mary district and only ~6 km from existing infrastructure. Turquoise represents a compelling new drill target that we’re excited to test this summer as we continue to build a strong pipeline of high-quality targets across the HWY 37 Project. “

Figure 1: Plan overview of the Turquoise Porphyry Target and Section A-A’ Location
Figure 2: Cross-section Turquoise Porphyry Target IP-chargeability, MVI amplitude, MMT resistivity, DC-resistivity results, and a compilation summary interpretation.

Turquoise Porphyry Target

A new porphyry target has been identified ~3.4 km east of the Hank Porphyry discovery hole (HW-25-011). The target is centered on a 0.5 by 2.0 km chargeability anomaly (> 12.0 mV/V) and is supported by the recent MMT inversion, and magnetic inversion products1. Geophysical patterns define a possible fluid upwelling or structural root to the anomaly, supported by coincident geophysical signatures and surface geology mapping. The scale of the target area is approximately 1 by 3.4 km, elongated to the northeast.

Geophysical Highlights:

  • IP Chargeability: A large, coherent chargeability anomaly extends to surface and is spatially coincident with mapped pyrite alteration. The anomaly forms a volume approximately 0.5 km wide, 0.5 km deep and 2.0 km long and could define a broad sulphide-rich system.  The peak chargeability values are 25 mV/V.
  • MVI Amplitude: A steep, low- to moderate-amplitude magnetic feature is interpreted to reflect a structural focus or a fluid flow pathway. This feature appears to focus on the core of the chargeability anomaly, refining the primary drill target.
  • Resistivity (MMT and DC): Integrated resistivity datasets define classic porphyry-style architecture:
    • A mushroom-shaped, low-resistivity (conductive) cap with values ranging between 25-100 ohm * m and dimensions of approximately 1.0 km deep, 4.0 km wide and 6.0 km long, coincident with mapped clay-rich alteration.  
    • Underlying low- to moderate-resistivity domains are interpreted as potential porphyry stockwork zones, with the central “stem” representing a central fluid upwelling within a broad alteration system.
    • Moderate resistivity at surface correlates with mapped siliceous advanced argillic alteration.

Surface Geology Highlights:

  • Mapping indicates a vector toward higher temperature alteration toward the core target. Advanced argillic mineralogy, including dickite and vuggy silica, has been identified above the chargeability anomaly and may indicate a porphyry-top position.
  • Sericite–chlorite-pyrite-quartz alteration observed at surface within the core target area is consistent with porphyry-style alteration observed at the Hank porphyry.
  • The projected surface expression of the core target is largely obscured by landslide and moraine cover. However, proximal outcrops report elevated pyrite contents (>5%), supporting the geophysical interpretation.
  • Representative prospecting and rock sampling in the valley remain limited due to extensive till and landslide cover.
Figure 3: Photograph of Turquoise Porphyry Target Area.

Qualified Person

Technical aspects of this news release have been reviewed, verified, and approved by Tyler Caswell, P.Geo., Vice President Exploration of Kingfisher, who is a qualified person as defined by National Instrument 43-101 – Standards of Disclosure for Minerals Projects.

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 134,898,973 shares outstanding.

For further information, please contact:

Dustin Perry, P.Geo.
CEO, President, and Director
Phone: +1 778 606 2507
E-Mail: info@kingfishermetals.com    

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

Mineralization hosted on adjacent and/or nearby properties is not necessarily indicative of mineralization hosted on the Company’s property. This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur.

Forward-looking statements in this news release include, among others, statements relating to expectations regarding the projects, and other statements that are not historical facts. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; domestic and foreign laws and regulations could adversely affect the Company’s business and results of operations; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance.

The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.

(1) See news release dated April 2, 2026, available at www.kingfishermetals.com and the Company’s profile at www.sedarplus.ca

Kingfisher Appoints Sharon G.K. Singh to Board of Directors

Kingfisher Metals Corp. (TSX-V: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher” or the “Company”) is pleased to announce the appointment of Sharon G.K. Singh as an independent director of the Company.

Ms. Singh is a highly regarded lawyer with deep expertise in environmental, Indigenous, regulatory and governance matters, particularly in the mining and natural resource sectors. Her appointment further strengthens Kingfisher’s commitment to responsible exploration, strong Indigenous, community and stakeholder engagement, and robust ESG practices.

“Sharon brings an exceptional combination of legal, policy, and practical mining experience at a time when strong Indigenous partnerships, environmental stewardship, and regulatory clarity are critical to advancing projects in British Columbia,” said Dustin Perry, CEO and President of Kingfisher. “Her perspective will be invaluable as we continue to advance our unrivaled land position in the Golden Triangle.”

About Sharon G.K. Singh

Ms. Singh is a Partner and Co-Head of the Indigenous and Environment practices at McMillan LLP, where she advises leading companies on complex matters spanning environmental assessment, permitting, regulatory compliance, Indigenous relations, and ESG strategy. She has extensive experience supporting mining, energy, and infrastructure projects through all stages of development, from regulatory approvals and negotiating Indigenous agreements to developing governance frameworks aligned with long-term project success.

Her background includes experience with an international mining company and board service. She is consistently recognized as a leading Canadian lawyer by Lexpert, Chambers Global, and Legal 500 in disciplines including ESG, Indigenous, environmental, and mining law. Ms. Singh holds a Master of Laws, a Bachelor of Laws, and a Bachelor of Business (International Trade) and is called to the bar in multiple jurisdictions.

Ms. Singh commented, “I am pleased to be joining Kingfisher’s board at this important stage of the Company’s growth. I look forward to working with the board and management team to support the Company’s continuous progress towards its strategic objectives and commitment to responsible development.”

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 133,732,098 shares outstanding.

For further information, please contact:

Dustin Perry, P.Geo.
CEO, President, and Director
Phone: +1 778 606 2507
E-Mail: info@kingfishermetals.com    

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

This news release contains “forward-looking statements” identified by words such as “expects,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential,” and similar expressions, or that events or conditions “will,” “would,” “may,” “could,” or “should” occur. Forward-looking statements involve known and unknown risks and uncertainties that may cause actual results to differ materially from those anticipated, including: the need for additional financing on acceptable terms; compliance with government regulation; changes in domestic and foreign laws that could adversely affect operations; and stock market volatility unrelated to the Company’s performance. These statements reflect the Company’s expectations as of the date of this release and are subject to change. The Company undertakes no obligation to update forward-looking statements should management’s beliefs, estimates, or other factors change.

Multiple Geophysical Datasets Support Increased Target Dimensions at Hank Copper-Gold Discovery, HWY 37 Project, Golden Triangle

Kingfisher Metals Corp. (TSX-V: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher” or the “Company”) is pleased to announce that new and updated geophysical inversion datasets support a robust porphyry copper-gold target within the Hank Cu-Au discovery area. Results include a new Mobile MagnetoTellurics (MMT) and magnetic survey with inversions, newly compiled, leveled and merged airborne magnetic data, updated IP chargeability and direct current (DC) resistivity 3D inversions, along with new petrographic data from geological thin sections. These new and improved datasets provide Kingfisher with five additional data-layers integrated into a 3-dimensional targeting framework. Analysis of these datasets supports the scale and prospectivity of the porphyry Cu-Au discovery at Hank. The Hank discovery is within the 933 km2 HWY 37 Project located within the Golden Triangle, British Columbia.

Key Highlights:

  • The magnetic vector inversion (MVI) model outlines a large alteration footprint, interpreted as magnetite destruction and remanent magnetization, consistent with surface and drill core observations.
  • Expanded IP-resistivity surveys reveal a >2 km wide anomaly coinciding with the interpreted potassic altered core.
  • MMT and DC-resistivity results highlight a significant low resistivity anomaly (below 50 ohmm) over an area of approximately 3.5 by 4.4 km, interpreted as hydrothermal clay alteration related to the Hank system.
  • Petrographic analysis of thin sections from hole HW-25-011 show that hydrothermal alteration has destroyed magnetite and reveals high fertility indicators, including bornite and tennantite.

Dustin Perry, CEO and President of Kingfisher, states, “Over the past three years we have systematically explored the Hank area with multiple geophysical, geological, geochemical, and spectral surveys. These updated datasets provide even more confidence going into the 2026 field program where we seek to aggressively expand upon the newest Cu-Au porphyry discovery in BC’s Golden Triangle.”

Figure 1: Plan view of the Hank-Williams area with reduced to pole magnetics (RTP) in the background. Grey lines show IP-resistivity lines. Inset map on the right presents the HWY 37 tenure outline with compiled, leveled and merged RTP data in the background.
Figure 2: Cross section A-A’ illustrating IP-chargeability, magnetic vector inversion amplitude, MMT resistivity, DC-resistivity results, and a compilation summary interpretation.
Figure 3: Cross section B-B’ illustrating IP chargeability, magnetic vector inversion amplitude, MMT resistivity, DC-resistivity results, and a compilation summary interpretation.
Figure 4: Long section C-C’ illustrating IP chargeability, magnetic vector inversion amplitude, MMT resistivity, DC-resistivity results, and a compilation summary interpretation.
Figure 5: A) early potassic alteration near syn-mineral dyke overprinted by magnetite-destructive alteration; B) electrum grain ~10 microns enclosed by pyrite, replaced to chalcopyrite; C) ~10 micron electrum grain enclosed by chalcopyrite; D) bornite-chalcopyrite emulsion texture near syn-mineral dyke; and E) quartz vein with chalcopyrite-tennantite-electrum.

Summary & Discussion

In 2025, Expert Geophysics Ltd. conducted an 1825.0 line-km MMT survey, with data provided to Moombarriga Geoscience for 3D inversion. Peter E. Walcott & Associates Ltd. completed 22.3 line-km of IP-resistivity surveying. The resulting IP-resistivity data, combined with historical and 2024 data, produced a unified 3D inversion model of resistivity and chargeability for much of the Hank-Williams target area. Hardrock Geophysics Inc. compiled, leveled, and merged all historical airborne magnetic datasets within the HWY 37 tenure, which were then used for 3D magnetic susceptibility and magnetic vector (MVI) inversions.

Integrating geophysical products with diamond drilling, surface geochemistry, geological mapping, and petrography enables new targeting insights. By combining and interpreting these datasets within a porphyry-epithermal framework, a cohesive core porphyry target area has been identified. This integration has led to several significant observations:

  • A large area of possible porphyry-related magnetite destruction is inferred from magnetic data and surface geology.
    • RTP magnetics show a broad, moderate magnetic response in the Hank area (Figure 1). This zone also appears in other magnetic inversion products and aligns with mapped surface alteration.
    • Other datasets confirm a large volume of altered rock marked by magnetite loss and potential remanent magnetization. Cross sections (Figures 2–4) show the extent of the alteration, with high chargeability highlighting a core target. Drillhole HW-25-011 confirmed significant mineralization matching magnetic, chargeability, and resistivity anomalies.
    • Abundant pyrite and sericite at surface and in HW-25-011 support magnetite destruction, including high pyrite-to-chalcopyrite ratios. These features match flanking phyllic alteration.
    • Petrographic and drill core analysis further confirm magnetite destructive sericite-quartz-pyrite alteration assemblages in HW-25-011 (Figure 5).
  • Figures 2-4 show that resistivity sections from the MMT and DC-resistivity surveys outline a broad, low-angle blanket of low-resistivity (conductive) rock. This blanket lies above and to the side of the core target area, which is defined by coincident chargeability and magnetic anomalies.
    • This low-resistivity (conductive) anomaly, clearly mapped in the sections, is interpreted as an area of widespread clay alteration associated with the porphyry-epithermal mineral system.
    • A pronounced, mushroom-shaped conductivity zone marks a fluid pathway in the porphyry-epithermal system.
  • Volumes of moderate resistivity lie beneath the low resistivity anomaly in the DC-resistivity sections (Figures 2-4). These areas are near or overlap the chargeability anomalies. They may be intrusive porphyry stocks that are more resistant than the surrounding clay-altered wall rock.

Hank Porphyry Petrographic Study

Petrographic analysis of the Hank porphyry confirmed complex mineralogy near syn-mineral intrusions and widespread magnetite-destructive alteration (Figure 5). Narrow, syn-mineral intrusions host bornite and tennantite along with chalcopyrite, indicating a fertile system.  Electrum is also identified as 5-10 micron-sized grains near these intrusions, closely associated with copper minerals including bornite, chalcopyrite and tennantite.

Investor Relations Engagements

The Company entered into an investor relations consulting agreement with Adelaide Capital Markets Inc. (“Adelaide“) dated March 1, 2026, for various investor relations services at an aggregate cost of C$8,000 per month, payable monthly, subject to acceptance by the TSX Venture Exchange (the “TSXV”).

The agreement has an initial term commencing March 1, 2026, and ending April 30, 2027, and will automatically renew on a month-to-month basis thereafter unless terminated in accordance with its terms. Adelaide is an arm’s length consultant and was previously granted 35,000 stock options that have fully vested. To the knowledge of the Company, both Adelaide and Deborah Honig, President of Adelaide, own shares of Kingfisher. Neither the Company nor any of its directors, officers or employees have any interest, directly or indirectly, in Adelaide, or their securities, or any right or intent to acquire such an interest. Adelaide manages a marketing team headquartered in Toronto, Ontario, and has been successfully providing services for a broad range of companies listed on the TSXV.

Stock Option Grant

The Company announces the grant of 4,375,000 stock options to certain directors, officers, employees, and consultants pursuant to the Company’s stock option plan. This includes 75,000 stock options granted to Adelaide. The stock options are exercisable for a period of five (5) years at an exercise price of C$0.66 per share and will vest over a period of twenty-four (24) months. The stock options were granted as part of Kingfisher’s ongoing efforts to attract and retain key personnel and provide long-term performance incentives.

Qualified Person

Technical aspects of this news release have been reviewed, verified, and approved by Tyler Caswell, P.Geo., Vice President Exploration of Kingfisher, who is a qualified person as defined by National Instrument 43-101 – Standards of Disclosure for Minerals Projects.

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 133,732,098 shares outstanding.

For further information, please contact:

Dustin Perry, P.Geo.
CEO, President, and Director
Phone: +1 778 606 2507
E-Mail: info@kingfishermetals.com    

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

Mineralization hosted on adjacent and/or nearby properties is not necessarily indicative of mineralization hosted on the Company’s property. This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur.

Forward-looking statements in this news release include, among others, statements relating to expectations regarding the projects, and other statements that are not historical facts. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; domestic and foreign laws and regulations could adversely affect the Company’s business and results of operations; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance.

The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.

Kingfisher Announces Closing of C$30 Million Bought Deal Offering

Kingfisher Metals Corp. (TSXV: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher or the Company“) is pleased to announce it has closed the bought deal private placement previously announced on February 5, 2026, and February 6, 2026, for aggregate gross proceeds of C$30,007,000, including proceeds raised from the Underwriters’ option (the “Offering”). 

The Offering was completed by a syndicate of underwriters led by BMO Nesbitt Burns Inc. as lead underwriter and sole bookrunner, AgentisCapital Markets (First Nations Financial Markets Limited Partnership), Haywood Securities Inc., Raymond James Ltd., and Velocity Trade Capital Ltd. (collectively, the “Underwriters”). In consideration for the services provided by the Underwriters in connection with the Offering, the Underwriters received a cash fee in the amount of C$1,449,030.10.

Pursuant to the Offering, the Company issued 5,300,000 non-critical charity flow-through common shares (the “NCCFT Shares”), at a price of C$0.94 per NCCFT Share, 14,500,000 critical charity flow-through common shares (the “CCFT Shares”), at a price of C$1.04 per CCFTShare, and 15,300,000 hard dollar common shares (the “HD Shares”), at a price of C$0.65 per HD Share (collectively, the “Offered Shares”).

Each NCCFT Share and CCFT Share will qualify as a “flow-through share” for the purposes of the Income Tax Act (Canada) (the “Tax Act”).

The gross proceeds raised from the NCCFT Shares and CCFT Shares will be used to incur Qualifying Expenditures (defined below). The net proceeds of the sale of the HD Shares will be used for exploration of the Company’s properties and general corporate purposes.

The Company shall use the gross proceeds raised from the NCCFT Sharesand the CCFT Shares to incur, on or after the closing date and on or prior to December 31, 2027, “Canadian exploration expenses” (as defined in subsection 66.1(6) of the Tax Act) (“CEE”) and, in the case of CCFTShares, such CEE shall also qualify as “flow-through critical mineral mining expenditures” (as defined in subsection 127(9) of the Tax Act), and in the case of the NCCFT Shares,  as “flow-through mining expenditures” within the meaning of the Tax Act and, in each case, for NCCFT Sharesand CCFT Shares purchased by eligible British Columbia purchasers, as “BC flow-through mining expenditures” that meet the criteria set forth in subsection 4.721(1) of the Income Tax Act (British Columbia), in respect of the exploration activities on the Company’s properties in British Columbia (together, the “Qualifying Expenditures”).

The Offered Shares will be subject to a hold period under Canadian securities laws of four months and one day from their date of issue.Closing of the Offering is subject to final approval of the TSX Venture Exchange (the “TSXV”). 

A director of the Company subscribed for 100,000 HD Shares for gross proceeds of $65,000 under the Offering. Participation by this insider of the Company in the Offering constitutes a related-party transaction as defined under Multilateral Instrument 61-101 – Protection of Minority Security Holders in Special Transactions (“MI 61-101”). The issuance of these securities is exempt from the formal valuation requirements of Section 5.4 of MI 61-101 pursuant to Subsection 5.5(b) of MI 61-101 as the common shares of the Company are listed on the TSXV. The issuance of these securities is also exempt from the minority approval requirements of Section 5.6 of MI 61-101 pursuant to Subsection 5.7(1)(b) of MI 61-101 as the fair market value was less than $2,500,000.

The securities to be offered pursuant to the Offering have not been, and will not be, registered under the U.S. Securities Act of 1933, as amended (the “U.S. Securities Act”) or any U.S. state securities laws, and may not be offered or sold in the United States or to, or for the account or benefit of, United States persons absent registration or any applicable exemption from the registration requirements of the U.S. Securities Act and applicable U.S. state securities laws.

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 128,710,907 shares outstanding.

For further Information, please contact:

Dustin Perry, P.Geo.​​​​​​​​​                                    
CEO and Director​​​​​​​​​​              
Phone: +1 778 606 2507​​​​​​​​​​        
E-Mail: info@kingfishermetals.com

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions (including negative and grammatical variations), or that events or conditions “will,” “would,” “may,” “could” or “should” occur.

Forward-looking statements in this news release include, among others, statements relating to expectations regarding the use of proceeds of the Offering and the incurrence and renunciation of Qualifying Expenditures by the Company and the timing thereof, receipt of final approval from the TSXV and other statements that are not historical facts. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; the results of exploration activities are uncertain; domestic and foreign laws and regulations could adversely affect the Company’s business, results of operations and financial condition; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance.

The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements, except as required by applicable securities laws, in the event that management’s beliefs, estimates or opinions, or other factors, should change.

KINGFISHER METALS INCREASES PREVIOUSLY ANNOUNCED BOUGHT DEAL FINANCING TO C$25 MILLION

Kingfisher Metals Corp. (TSXV: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher” or the “Company”) is pleased to announce that due to strong demand, it has increased the size of the previously announced bought deal to 5,300,000 non-critical charity flow-through common shares (the “Non-Critical Charity Flow-Through Shares”), at a price of C$0.94 per Non-Critical Charity Flow-Through Share, 14,500,000 critical charity flow-through common shares (the “Critical Charity Flow-Through Shares”), at a price of C$1.04 per Critical Charity Flow-Through Shares, and 7,600,000 hard dollar common shares (the “HD Shares”), at a price of C$0.65 per HD Share (collectively, the “Offered Securities”), for total gross proceeds of approximately C$25 million (the “Offering”). The Company previously entered into an agreement with BMO Capital Markets as sole bookrunner, on behalf of a syndicate of underwriters (collectively, the “Underwriters”). The Company has granted the Underwriters an option, exercisable at any time up to 48 hours prior to the closing of the Offering, to purchase up to an additional C$5 million of the Offering.

The Offering is expected to close on or about March 3, 2026 and is subject to Kingfisher receiving all customary regulatory approvals.

The gross proceeds raised from the Non-Critical Charity Flow-Through Shares and Critical Charity Flow-Through Shares will be used to incur Qualifying Expenditures (defined below) as set forth below under Charity Flow-Through Income Tax Considerations. The net proceeds of the sale of the HD Shares will be used for exploration of the Company’s properties and general corporate purposes.

The Company shall use the gross proceeds raised from the Non-Critical Charity Flow-Through Shares and the Critical Charity Flow-Through Shares to incur, after the closing date and on or prior to December 31, 2027, “Canadian exploration expenses” (as defined in subsection 66.1(6) of the Income Tax Act (Canada)) (“CEE”) and, in the case of Critical Charity Flow-Through Shares, such CEE shall also qualify as “flow-through critical mineral mining expenditures” (as defined in subsection 127(9) of the Income Tax Act (Canada)) (together, the “Qualifying Expenditures”).

The Offered Securities will be offered for sale on a private placement basis in each of the provinces and territories of Canada. The HD Shares may be offered in the United States pursuant to an exemption from the registration requirements of the United States Securities Act of 1933, as amended, (“U.S. Securities Act”) and internationally as permitted.

The securities offered have not been registered under the U.S. Securities Act of 1933, as amended, and may not be offered or sold in the United States absent registration or an applicable exemption from the registration requirements. This press release shall not constitute an offer to sell or the solicitation of an offer to buy nor shall there be any sale of the securities in any jurisdiction in which such offer, solicitation or sale would be unlawful.

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 91,872,852 shares outstanding.

For further information, please contact:

Dustin Perry, P.Geo.

CEO and Director

Phone: +1 778 606 2507

E-Mail: info@kingfishermetals.com   

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

Mineralization hosted on adjacent and/or nearby properties is not necessarily indicative of mineralization hosted on the Company’s property. This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur.

Forward-looking statements in this news release include, among others, statements relating to the size and amount of the Offering, the expected closing date of the Offering and the expected use of proceeds of the Offering; statements relating to expectations regarding the projects; and other statements that are not historical facts. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the anticipated timing of the Offering, that the Company will raise the anticipated amount of proceeds from the Offering, that the Company will use the proceeds of the Offering as anticipated, that the Offering will close as expected; the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; domestic and foreign laws and regulations could adversely affect the Company’s business and results of operations; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance.

The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.

KINGFISHER METALS ANNOUNCES C$20 MILLION BOUGHT DEAL FINANCING

Kingfisher Metals Corp. (TSXV: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher” or the “Company”) has announced today that it has entered into an agreement with a syndicate of underwriters led by BMO Capital Markets, as sole bookrunner, under which the underwriters have agreed to purchase, on a bought deal basis, 5,300,000 non-critical charity flow-through common shares (the “Non-Critical Charity Flow-Through Shares”), at a price of C$0.94 per Non-Critical Charity Flow-Through Share, 9,700,000 critical charity flow-through common shares (the “Critical Charity Flow-Through Shares”), at a price of C$1.04 per Critical Charity Flow-Through Shares, and 7,600,000 hard dollar common shares (the “HD Shares”), at a price of C$0.65 per HD Share (collectively, the “Offered Securities”), for total gross proceeds of approximately C$20 million (the “Offering”). The Company has granted the Underwriters an option, exercisable at any time up to 48 hours prior to the closing of the Offering, to purchase up to an additional 25% of the Offering (approximately C$5 million).

The Offering is expected to close on or about March 3, 2026 and is subject to Kingfisher receiving all customary regulatory approvals.

The gross proceeds raised from the Non-Critical Charity Flow-Through Shares and Critical Charity Flow-Through Shares will be used to incur Qualifying Expenditures (defined below) as set forth below under Charity Flow-Through Income Tax Considerations. The net proceeds of the sale of the HD Shares will be used for exploration of the Company’s properties and general corporate purposes.

The Company shall use the gross proceeds raised from the Non-Critical Charity Flow-Through Shares and the Critical Charity Flow-Through Shares to incur, after the closing date and on or prior to December 31, 2026, “Canadian exploration expenses” (as defined in subsection 66.1(6) of the Income Tax Act (Canada)) (“CEE”) and, in the case of Critical Charity Flow-Through Shares, such CEE shall also qualify as “flow-through critical mineral mining expenditures” (as defined in subsection 127(9) of the Income Tax Act (Canada)) (together, the “Qualifying Expenditures”).

The Offered Securities will be offered for sale on a private placement basis in each of the provinces and territories of Canada. The HD Shares may be offered in the United States pursuant to an exemption from the registration requirements of the United States Securities Act of 1933, as amended, (“U.S. Securities Act”) and internationally as permitted.

The securities offered have not been registered under the U.S. Securities Act of 1933, as amended, and may not be offered or sold in the United States absent registration or an applicable exemption from the registration requirements. This press release shall not constitute an offer to sell or the solicitation of an offer to buy nor shall there be any sale of the securities in any jurisdiction in which such offer, solicitation or sale would be unlawful.

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 91,872,852 shares outstanding.

For further information, please contact:

Dustin Perry, P.Geo.

CEO and Director

Phone: +1 778 606 2507

E-Mail: info@kingfishermetals.com   

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

Mineralization hosted on adjacent and/or nearby properties is not necessarily indicative of mineralization hosted on the Company’s property. This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur.

Forward-looking statements in this news release include, among others, statements relating to the size and amount of the Offering, the expected closing date of the Offering and the expected use of proceeds of the Offering; statements relating to expectations regarding the projects; and other statements that are not historical facts. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the anticipated timing of the Offering, that the Company will raise the anticipated amount of proceeds from the Offering, that the Company will use the proceeds of the Offering as anticipated, that the Offering will close as expected; the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; domestic and foreign laws and regulations could adversely affect the Company’s business and results of operations; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance.

The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.

Kingfisher Confirms Blind Copper-Gold Porphyry Discovery at Hank, HWY 37 Project, Golden Triangle, British Columbia

Kingfisher Metals Corp. (TSX-V: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher” or the “Company”) is pleased to announce final assay results from the 2025 drilling program at the HWY 37 Project. The 933 km2 HWY 37 Project is located within the Golden Triangle, British Columbia.

Drillhole HW-25-011 confirms discovery of a new copper – gold (Cu-Au) porphyry system below the Hank epithermal gold-silver (Au-Ag) mineralized system. Assays from HW-25-011 returned 425.0 meters[1] (m) of 0.40% CuEq[2] (0.15% Cu, 0.21 g/t Au and 2.2 g/t Ag) (Figure 1 – 5). This newly identified zone represents a blind discovery, as porphyry Cu-Au mineralization had not previously been recognized or reported at Hank. These results validate Kingfisher’s exploration model and demonstrate the potential for the Hank area to host one or more large-scale porphyry Cu-Au systems. 

Highlights from this release include:

  • Discovery of a blind porphyry Cu-Au system with 425.0 m of 0.40% CuEq (Figure 1 – 5).
  • Potential for a large-tonnage porphyry Cu-Au system nested below the Hank epithermal Au-Ag system (Figure 1 – 5).
  • Zonation observed in drillhole HW-25-011 progresses from low to higher temperature alteration demonstrating a vector towards a porphyry heat source to the southeast. This is indicated by:  
    • Increasing Cu:Au ratios downhole toward the southeast (Figure 4)
    • Sulfide mineralogy (see summary and discussion below)
    • Alteration and vein zonation (see summary and discussion below)
  • 2026 Target Area to be drill tested, approximately 1.75 km x 0.95 km (Figure 2 –  5), defined by geophysical, geological and exploration inputs[3].
  • Mineralization remains open in all directions, with the drill hole terminating in increasing copper grades at 959.0 m depth (Figure 3). 
  • Induced polarization (IP) surveys lines north and south of HW-25-011 outline broad areas of chargeability possibly indicating the presence of a large, disseminated sulfide body (Figure 4).

Dustin Perry, CEO of Kingfisher, states, “The final hole of the 2025 program validates our long-standing belief that the shallow Hank Au-Ag epithermal mineralization is driven by a large porphyry Cu-Au system. This impressive first intercept of 425.0 metres of 0.40% CuEq is interpreted to be on the margin of the system, with anticipated increases in grade toward the conceptual core. The scale and consistency of this discovery, along with a wide untested area hosting strong geophysical anomalies, highlight the potential for further exploration and support the need for aggressive follow-up drilling in 2026.”

Table 1. Drill Results from this Release.

Hole No.From (m)To (m)Interval (m)1Cu (%)Au (g/t)Ag (g/t)CuEq (%)2AuEq (g/t)2
HW-25-011281.0293.012.00.021.181.61.22
Incl.284.85286.451.60.016.953.56.99
and357.0362.45.40.010.941.50.97
and468.0497.029.00.010.272.10.30
and534.0959.0425.00.150.212.20.400.37
Figure 1: Plan View Historical and 2025 Drillhole Locations
Figure 2: Plan view of HW-25-011 relative to historical drilling and section lines.
Figure 3: Interpreted Cross Section HW-25-011
Figure 4: IP Sections
Figure 5: 3D view looking oblique to the northeast showing the location of HW-25-011 relative to the proposed “2026 target area” at Hank for future drill testing, historical drilling and location of the Williams & Mary Cu-Au Deposits as well as the Hank Epithermal Au-Ag System.  

HW-25-011 Summary & Discussion

Porphyry-style mineralization and alteration was identified through detailed core logging and geochemical analysis in drill hole HW-25-011, which returned 425.0 m grading 0.15% Cu, 0.21 g/t Au, and 2.2 g/t Ag (0.40% CuEq) (Figure 3). The host lithologies intersected are limited to volcanics with the exception of two, meter-scale dykes characterized by an increase in quartz veins and chalcopyrite mineralization locally.

Alteration observed in HW-25-011 is consistent with what is typically developed along the flanks of a porphyry copper–gold system. Visual observations show widespread, multi-generational porphyry-style veins and disseminated sulfide mineralization, characterized by pyrite greater than chalcopyrite throughout much of the hole. Prior to HW-25-011, historical drilling at Hank had not identified porphyry-style mineralization or zoned porphyry alteration.

Three alteration–mineralization domains are interpreted within HW-25-011. These domains are consistent with increasing proximity to a porphyry center:

  1. 0–530 m: Porphyry-distal (low temperature) alteration characterized by quartz–carbonate veins and disseminated pyrite, accompanied by elevated Pb, Zn, Ag and Au concentrations.
  2. 530–890 m: Porphyry-flanking (moderate temperature) alteration assemblage of quartz–chlorite–magnetite–pyrite hosted in volcanics. Pyrite-to-chalcopyrite ratios are high overall, with locally elevated chalcopyrite associated with higher-density quartz stockwork domains.
  3. 890–959 m: Porphyry-proximal (moderate to high temperature) alteration marked by lower pyrite-to-chalcopyrite ratios and the appearance of early K-feldspar–magnetite-chalcopyrite veins within a broad quartz–chlorite-magnetite–pyrite–chalcopyrite ± molybdenite alteration assemblage.

Across the reported interval, an increase in Cu:Au ratio downhole and toward the southeast also supports vectoring toward a higher temperature and possibly more copper-dominant porphyry core to the southeast. This same pattern and vector is also observed in the sulfide mineralogy with the visual estimates showing pyrite >> chalcopyrite transitioning to pyrite > chalcopyrite.  Mineralization remains open in all directions, with the hole terminating in mineralization at 959.0 m depth.

Induced polarization (IP) survey lines completed north and south of HW-25-011 (Figure 4) indicate a broad chargeability body interpreted to represent a large sulfide system. The IP chargeability data indicates a potentially broader zone of disseminated sulfide than what is outlined within the “2026 Target Area” shape in Figures 2 – 5. 

The priority 2026 target area is defined by integrated geological, geochemical, and geophysical datasets and covers approximately 1.75 km × 0.95 km (Figure 2 – 5).  This represents the Company’s top priority for follow-up drilling in 2026.

Other

Dustin Perry – CEO, will be presenting at the Metals Investor Forum in Vancouver, BC, tomorrow (Friday, January 23) at 3:00 pm PST.  Those wishing to attend can visit metalsinvestorforum.com for registration details.

Drill core from Williams as well as the new Hank porphyry discovery (HW-25-011) will be on display for the public to view at the core shack during the AME Round Up in Vancouver, BC, on January 26 and 27. 

Quality Assurance / Quality Control (QAQC)

Drilling on site at the HWY 37 Project was supervised by on-site Kingfisher personnel who implemented a full QAQC program using coarse blanks, pulp blanks, standards, and duplicates inserted into the sample stream to monitor analytical accuracy and precision. The samples were sealed on site using tamper proof seals with unique identifiers. The samples were sent to the Bureau Veritas (BV) lab in Vancouver, British Columbia. BV’s quality control system complies with global certifications for Quality ISO/IEC 17025:2017 – General requirements for the competence of testing and calibration laboratories. Diamond drill core samples were analyzed using a combination of BV’s MA200 process for low level concentrations (4 acid digestion/ICP-ES/MS) and MA 370 process for higher level concentrations (4 acid digestion/ICP-ES). Gold assaying was completed using FA430, a 30-gram fire assay with AAS finish. If applicable, base metal overlimits were finalized with titration, and gold overlimits completed with a gravimetric finish. Technical aspects of this news release have been reviewed, verified, and approved by Tyler Caswell, P.Geo., Vice President Exploration of Kingfisher, who is a qualified person as defined by National Instrument 43-101 – Standards of Disclosure for Minerals Projects.

Table 2. 2025 Drill Results HYW–37 Project

Hole No.From (m)To (m)Interval (m)1Cu (%)Au (g/t)Ag (g/t)CuEq (%)2AuEq (g/t)2
HW-25-001249.0797.1548.10.140.161.80.340.31
incl.426.55550.75124.20.180.233.00.470.43
HW-25-002118.0124.06.00.010.481.10.50
and201.0217.016.00.010.262.30.29
and233.0247.014.00.020.272.00.32
and405.0415.010.00.010.451.40.47
HW-25-003101.7108.06.30.010.505.00.56
and160.0164.04.00.010.778.60.87
and487.5488.40.90.011.6833.92.02
and504.0510.06.00.030.344.20.41
HW-25-004328.1885.9557.80.290.301.60.640.58
incl.328.1562.45234.350.440.492.31.000.91
HW-25-005Hole abandoned – HW-25-006 is the redrill
HW-25-006192.0433.0241.00.010.280.40.29
incl.197.0307.0110.00.010.470.20.49
HW-25-007Hole abandoned – HW-25-011 is the redrill
HW-25-0083.65893.0889.350.210.221.50.470.43
incl.287.95328.1040.150.460.622.51.161.06
HW-25-00949.3322.0272.70.110.154.00.310.29
HW-25-0104.3726.0721.70.220.211.30.460.42
incl.4.383.078.70.430.503.01.010.93
incl.273.0320.5547.550.490.561.91.121.03
HW-25-011281.0293.012.00.021.181.61.22
incl.284.85286.451.60.016.953.56.99
and357.0362.45.40.010.941.50.97
and468.0497.029.00.010.272.10.30
and534.0959.0425.00.150.212.20.400.37

             Table 3. Collar location and orientation of 2025 Drilling

Hole IDEasting (mE)North (mN)Azimuth (o)Dip (o)Final Depth (m)
UTM NAD83 Zone 09
HW-25-0014093956344077119-80803
HW-25-0024097696343628292-85550
HW-25-0034100866343432286-68668
HW-25-0044095106344131169-75886
HW-25-0054104756341586295-76282
HW-25-0064104756341586295-77839
HW-25-0074087906342028110-65192
HW-25-0084094156343882027-73893
HW-25-0094095866343818255-82761
HW-25-0104094196343879075-84797
HW-25-0114087906342028111-65959

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 90,909,852 shares outstanding.

For further information, please contact:

Dustin Perry, P.Geo.
CEO and Director
Phone: +1 778 606 2507
E-Mail: info@kingfishermetals.com    

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

Mineralization hosted on adjacent and/or nearby properties is not necessarily indicative of mineralization hosted on the Company’s property. This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur.

Forward-looking statements in this news release include, among others, statements relating to expectations regarding the projects, and other statements that are not historical facts. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; domestic and foreign laws and regulations could adversely affect the Company’s business and results of operations; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance.

The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.


[1] True widths of the reported mineralized interval have not been determined.

[2] Assumptions used in USD for the metal equivalent calculation were metal prices of $4.00/lb copper, $3,000/oz gold, and $30/oz silver. No current or historical metallurgical work has been completed therefore recoveries are assumed to be 80% for copper, 80% for gold and 80% for silver. The following equations was used to calculate the copper equivalence:  AuEq = gold (g/t) + (copper (%) x 0.9143) + (silver (g/t) x 0.0100). The following equations was used to calculate the copper equivalence:  CuEq = copper (%) + (gold (g/t) x 1.0938) + (silver (g/t) x 0.0109) Differences may occur due to rounding.

[3] Dependent on funding

Kingfisher Metals Reports 889.35 meters of 0.47% CuEq and 721.7 meters of 0.46% CuEq from surface at Williams, HWY 37 Project, Golden Triangle, British Columbia

Kingfisher Metals Corp. (TSX-V: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher” or the “Company”) is pleased to announce further results from the 2025 exploration and drilling program at the HWY 37 Project. The 933 km2 HWY 37 Project is located within the Golden Triangle, British Columbia.

Assay results have been received for an additional three diamond drill holes HW-25-008, -009, and -010.  Diamond drill holes HW-25-008 and -010 returned some of the longest copper intercepts from within the Williams porphyry copper-gold system. HW-25-008 cut 889.35 m[1] of 0.47% CuEq[2] starting at surface below 3.65 m of cover to end of hole at 893 m (Figure 4)Drillhole HW-25-010 returned 721.7 m of 0.46% CuEq starting below 4.3 m of cover which includes 78.7 m of 1.01% CuEq from 4.3 m depth (Figure 7). These drillholes demonstrate continuity of grade with mineralization from surface of bedrock to depth within the Williams deposit. 

Highlights from this release include:

  • HW-25-008 (Williams)889.35 m of 0.47% CuEq from 3.65 m
    • Including 40.15 m at 1.16% CuEq from 287.95 m
  • HW25-010 (Williams): 721.7 m of 0.46% CuEq   from 4.3 m 
    • Including 78.7 m of 1.01% CuEq from 4.3 m
    • Including 47.55 m of 1.12% CuEq from 273.0 m

“The Williams drilling continues to demonstrate a well-mineralized porphyry system with copper-gold mineralization extending from surface over long intervals,” said Dustin Perry, CEO of Kingfisher. “While Williams is interpreted as a satellite to a larger porphyry system at Hank, the presence of bornite and localized higher-grade intervals highlights the fertility of the broader system. These results provide geological context for the Hank porphyry system identified in the final hole of the program (HW-25-011), with results expected to be released in the near term.”

Table 1. Drill Results from this Release.

Hole No.From (m)To (m)Interval (m)1Cu (%)Au (g/t)Ag (g/t)CuEq (%)2AuEq (g/t)2
HW-25-0083.65893.0889.350.210.221.50.470.43
incl.287.95328.1040.150.460.622.51.161.06
HW-25-00949.3322.0272.70.110.154.00.310.29
HW-25-0104.3726.0721.70.220.211.30.460.42
incl.4.383.078.70.430.503.01.010.93
incl.273.0320.5547.550.490.561.91.121.03
Figure 1: Plan View Historical and 2025 Drillhole Locations
Figure 2: Plan view of Williams Drilling

HW-25-008 Summary

This hole was designed to cross quartz stockwork veins with chalcopyrite +/- bornite mineralization observed at surface and test the strike and depth extent of the Williams porphyry to the northeast. Hole HW-25-008 intersected mineralization at surface below cover until end of hole, returning 889.35 m of 0.21% Cu, 0.22 g/t Au and 1.5 g/t Ag (0.47% CuEq). This included a higher-grade interval of 40.15 m with 1.16% CuEq from 287.95 m downhole (Figure 4). The alteration associated with the mineralization observed is:

  • 0–157 m: potassic alteration with varying amounts of chalcopyrite ± bornite
  • 157–253 m: felsic stratigraphy with low sulfide and trace chalcopyrite concentrations
  • 253–810 m: potassic alteration in mixed monzonite and wall rock with variable chalcopyrite ± bornite
  • 810–893 m: flanking alteration of epidote-magnetite-K-feldspar, low relative chalcopyrite and increase in pyrite
Figure 3: HW-25-008 – 315 m downhole – 0.68 % Cu, 0.94 g/t Au, & 4.0 g/t Ag (1.75 % CuEq), (Bn = Bornite, Cpy = Chalcopyrite) Potassic alteration with copper sulfide mineralization
Figure 4: Williams deposit section of HW-25-008.

HW-25-009 Summary

Hole HW-25-009 targeted the root area of the Williams deposit. The drill hole returned 272.7 m of 0.11% Cu, 0.15 g/t Au and 4.0 g/t Ag from 49.3 m.  Mineralization observed is hosted within a flanking alteration assemblage of K-feldspar-epidote-magnetite and high pyrite : chalcopyrite ratios.  This observation shows that this hole was drilled in the southeastern margin of the Williams deposit and Kingfisher believes there is potential for additional mineralization to the west-northwest of this hole, demonstrated by trends of mineralization observed in section view (Figure 5).

Figure 5: Annotated cross-section of drill hole HW-25-009

HW-25-010 Summary

Hole HW-25-010 collared on the same drill pad as HW-25-008. This hole was designed to test the deeper domain boundaries of the porphyry system. Hole HW-25-010 accomplished this goal and defined the eastern domain boundary and returning 721.7 m of 0.22% Cu, 0.21 g/t Au, and 1.3 g/t Ag (0.46% CuEq) which includes 78.7 m of 1.01% CuEq and 47.55 m of 1.12% CuEq from 4.3 and 273.0 m respectively (Figure 7).  The alteration associated with the mineralization observed is:

  • 0–196.5 m: potassic alteration with varying amounts of chalcopyrite +/- bornite in wall rock
  • 196.5–268 m: felsic host rock, less favourable host, low relative chalcopyrite abundance
  • 268–521 m: variable potassic alteration in mixed monzonite and wall rock with chalcopyrite +/- bornite
  • 521–797 m: wall rock overprinted by porphyry flanking-type alteration (K-feldspar-epidote-magnetite-chlorite) and low relative chalcopyrite
Figure 6: HW-25-010 – 44.8 m downhole – 1.19% Cu, 0.62 g/t Au, & 12.2 g/t  Ag (2.00% CuEq), (Bn = Bornite, Cpy = Chalcopyrite). Potassic alteration with copper sulfide mineralization
Figure 7: Annotated cross-section showing drill hole HW-25-010

HW-25-006 Update

Further to the release dated November 10, 2025 (Kingfisher Metals Reports 110 Meters of 0.47 g/t Gold in ~500 m step-out at Hank and Extends Gold in Soil Anomaly at Hank on the HWY 37 Project, Golden Triangle, British Columbia), multielement assay results from HW-25-006 has been received.  The new data updates the intersection to 241.0 m of 0.01% Cu, 0.28 g/t Au, and 0.4 g/t Ag (0.29 g/t AuEq) including 110.0 m of 0.01% Cu, 0.47 g/t Au and 0.2 g/t Ag (0.49 g/t AuEq). The values are summarized in table 2 (below). 

Pending Results

Kingfisher has now received assays for diamond drill hole HW-25-011, which are currently being interpreted by the Company with an update to follow in due course. The Company is also waiting on final IP and airborne EM (MMT) geophysical datasets as well as finalized geological mapping data collected during the 2025 field program. Results of these surveys will be released once received and interpreted.

Kingfisher will be attending the upcoming AME Roundup Core Shack in Vancouver, British Columbia. Drill core from Williams as well as the new Hank porphyry system (HW-25-011) will be on display for the public to view in the Core Shack on January 26 and 27.

Quality Assurance / Quality Control (QAQC)

Drilling on site at the HWY 37 Project was supervised by on-site Kingfisher personnel who implemented a full QAQC program using coarse blanks, pulp blanks, standards, and duplicates inserted into the sample stream to monitor analytical accuracy and precision. The samples were sealed on site using tamper proof seals with unique identifiers. The samples were sent to the BV lab in Vancouver, British Columbia. BV’s quality control system complies with global certifications for Quality ISO/IEC 17025:2017 – General requirements for the competence of testing and calibration laboratories. Diamond drill core samples were analyzed using a combination of BV’s MA200 process for low level concentrations (4 acid digestion/ICP-ES/MS) and MA 370 process for higher level concentrations (4 acid digestion/ICP-ES). Gold assaying was completed using FA430, a 30-gram fire assay with AAS finish. If applicable, base metal overlimits were finalized with titration, and gold overlimits completed with a gravimetric finish. Technical aspects of this release have been reviewed, verified, and approved by Tyler Caswell, P.Geo., Vice President Exploration of Kingfisher, who is a qualified person as defined by National Instrument 43-101 – Standards of Disclosure for Minerals Projects.

Table 2. Drill results to date

Hole No.From (m)To (m)Interval (m)Cu (%)Au (g/t)Ag (g/t)CuEq (%)AuEq (g/t)
HW-25-001249.00797.10548.100.140.161.80.340.31
incl.426.55550.75124.200.180.233.00.470.43
HW-25-002118.00124.006.000.010.481.10.50
and201.00217.0016.000.010.262.30.29
and233.00247.0014.000.020.272.00.32
and405.00415.0010.000.010.451.40.47
HW-25-003101.70108.006.300.010.505.00.56
and160.00164.004.000.010.778.60.87
and487.50488.400.900.011.6833.92.02
and504.00510.006.000.030.344.20.41
HW-25-004328.10885.90557.800.290.301.60.640.58
incl.328.10562.45234.350.440.492.31.000.91
HW-25-005Hole abandoned – HW-25-006 is the redrill
HW-25-006192.00433.00241.000.010.280.40.29
incl.197.00307.00110.000.010.470.20.49
HW-25-007Hole abandoned – HW-25-011 is the redrill
HW-25-0083.65893.0889.350.210.221.50.470.43
incl.287.95328.140.150.460.622.51.161.06
HW-25-00949.3322.0272.70.110.154.00.310.29
HW-25-0104.3726.0721.70.220.211.30.460.42
incl.4.383.078.70.430.503.01.010.93
incl.273.0320.5547.550.490.561.91.121.03
HW-25-011Results Pending

Table 3. Collar location and orientation of 2025 Drilling

Hole IDEasting (mE)North (mN)Azimuth (o)Dip (o)Final Depth (m)
UTM NAD83 Zone 09
HW-25-0014093956344077119-80803
HW-25-0024097696343628292-85550
HW-25-0034100866343432286-68668
HW-25-0044095106344131169-75886
HW-25-0054104756341586295-76282
HW-25-0064104756341586295-77839
HW-25-0074087906342028110-65192
HW-25-0084094156343882027-73893
HW-25-0094095866343818255-82761
HW-25-0104094196343879075-84797
HW-25-0114087906342028111-65959

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 90,814,018 shares outstanding.

For further information, please contact:

Dustin Perry, P.Geo.
CEO and Director
Phone: +1 778 606 2507
E-Mail: info@kingfishermetals.com    

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

Mineralization hosted on adjacent and/or nearby properties is not necessarily indicative of mineralization hosted on the Company’s property. This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur.

Forward-looking statements in this news release include, among others, statements relating to expectations regarding the projects, and other statements that are not historical facts. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; domestic and foreign laws and regulations could adversely affect the Company’s business and results of operations; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance.

The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.


[1] True widths of the reported mineralized interval have not been determined.

[2] Assumptions used in USD for the metal equivalent calculation were metal prices of $4.00/lb copper, $3,000/oz gold, and $30/oz silver. No current or historical metallurgical work has been completed therefore recoveries are assumed to be 80% for copper, 80% for gold and 80% for silver. The following equations was used to calculate the copper equivalence:  AuEq = gold (g/t) + (copper (%) x 0.9143) + (silver (g/t) x 0.0100). The following equations was used to calculate the copper equivalence:  CuEq = copper (%) + (gold (g/t) x 1.0938) + (silver (g/t) x 0.0109) Differences may occur due to rounding.

Kingfisher Reports Annual General Meeting Voting Results

Kingfisher Metals Corp. (TSX-V: KFR) (FSE: 970) (OTCQB: KGFMF) (“Kingfisher” or the “Company”) is pleased to report the voting results for the Company’s annual general meeting of shareholders (the “Meeting”) held on December 12, 2025, in Vancouver, British Columbia.

Fixing the Number and Election of Directors

Shareholders fixed the number of directors at five (5), and all five (5) of the nominees listed in Kingfisher’s management information circular dated November 18, 2025, that were proposed by management for election to the board of directors at the Meeting were duly elected. The directors will remain in office until the next annual meeting of the Company’s shareholders or until their successors are elected or appointed.   

Appointment of Auditors

Shareholders appointed De Visser Gray LLP as auditor of the Company for the upcoming year and authorized the directors of the Company to fix the remuneration of the auditor.

Approval of Stock Option Plan

The Company’s incentive stock option plan, which is a rolling stock option plan that permits the issuance of up to an aggregate of 10% of the issued and outstanding common shares of the Company from time to time, was approved by shareholders.

About Kingfisher Metals Corp.

Kingfisher Metals Corp. (https://kingfishermetals.com/) is a Canadian based exploration company focused on copper-gold exploration in the Golden Triangle, British Columbia. Through outright purchases and option earn in agreements (Orogen Royalties, Golden Ridge Resources, and Aben Gold) the Company has quickly consolidated one of the largest land positions in the Golden Triangle region at with the 933 km2 HWY 37 Project and 202 km2 Forrest Kerr Project. Kingfisher also owns (100%) two district-scale orogenic gold projects in British Columbia that total 641 km2. The Company currently has 88,927,226 shares outstanding.

For further information, please contact:

Dustin Perry, P.Geo.
CEO and Director
Phone: +1 778 606 2507
E-Mail: info@kingfishermetals.com   

Neither the TSX-V nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Statements

Certain of the statements made and information contained herein is considered “forward-looking information” within the meaning of applicable Canadian securities laws, including statements with regard to the results of the Meeting. These statements address future events and conditions and are reliant on assumptions made by the Company’s management, and so involve inherent risks and uncertainties, as disclosed in the Company’s periodic filings with Canadian securities regulators. As a result of these risks and uncertainties, and the assumptions underlying the forward-looking information, actual results could differ from those currently projected. The Company does not assume the obligation to update any forward-looking statement, except as required by applicable law.