Copper Fox Provides Update ON Geophysical Program at Eaglehead Porphyry Copper Project
COPPER FOX PROVIDES UPDATE ON GEOPHYSICAL PROGRAM AT
EAGLEHEAD PORPHYRY COPPER PROJECT
Calgary, Albert a - August 22, 2025. Copper Fox Metals Inc. (“Copper Fox” or the “Company”)
(TSXV:CUU | OTC:CPFXF | FSE:HPU ), through its wholly owned subsidiary Northern Fox Copper Inc.
(“Northern Fox”), is pleased to announce completion of the planned 3D pole-dipole distributed DCIP survey at
its 100% owned Eaglehead porphyry copper project (see news release dated July 16, 2025).
Highlights of the 2025 survey are:
• A 2,800 meter (m) long zone of anomalous chargeability (>8mv/s contour/~ 17mrads) occurs at surface
in the same northwest trending valley that hosts the four zones of porphyry style mineralization. The
anomaly dips to the north under propylitic altered quartz eye porphyry of the Eaglehead intrusive.
• The surface expression of the anomalous chargeability exhibits a strong correlation to the anomalous
chargeability identified in the 2014 geophysical survey.
• The chargeability anomaly occurs over a horizontal distance of 2,800m and extends down dip
approximately 2,400m to the north (Figure-1).
• Several pipe -like bodies of anomalous chargeability correspond to leached, mineralized hydrothermal
breccia and secondary copper showings mapped on surface (Figure-2).
• The anomalous chargeability occurs within a zone of lower resistivity and extends a significant distance
north (down dip) and a short distance south of the mineral resource area.
Elmer B. Stewart, President and CEO of Copper Fox stated, “ The preliminary results of the 2025 survey
significantly expanded the anomalous chargeability associated with the porphyry copper mineralization. The
strong correlation between chargeability and porphyry mineralization combined with the expanded chargeability
target has significant implications for the potential size of the mineralized envelopes associated with the open-
ended mineralized zones outlined in the 2023 Mineral Resource Estimate (MRE). Going forward merging the
chargeability and resistivity data from the 2014 - 2025 geophysical surveys, is expected to better define the extent
of the biotite granodiorite, the primary host for the porphyry style mineralization, and alteration zones associated
with the porphyry system to optimize future drilling programs.”
Background to 2025 Geophysical Survey
Since 2014, geophysical surveys mapped the chargeability and resistivity signatures of three contiguous areas of
the property. The 2014 survey covered from the East zone to the Camp zone and indicated a linear open-ended
zone of anomalous chargeability that was interpreted to be approximately 6,000m long by 900m wide. The four
open-ended zones of porphyry style mineralization outlined in the 2023 MRE are located along the axis of the
chargeability anomaly. Mapping programs completed after 2014 located a large number of secondary copper
showings and leached mineralized hydrothermal breccias in a previously unexplored area that lies outside of the
2014 geophysical survey area north of the Camp zone. The 2021 geophysical survey (four lines) covered the
mineralized area north of the Camp zone and extended the anomalous chargeability from the 2014 survey down
dip to the north. The 2021 survey results suggested the anomalous chargeability was open to the southeast. The
2025 survey extended the 2021 survey results to the southeast and mapped to the north and down dip of the 2014
survey chargeability and resistivity signatures from the East zone to the Camp zone.
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Figure-1: Shows the distribution of anomalous chargeability at a depth slice of approximately 400m below surface.
Figure-2:Showing a cross section of anomalous chargeability in the Bornite zone (see inset map).
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Preliminary Observations
The preliminary interpretation of the 2025 survey results used the 8mv/s ( ~17mrds) chargeability signature to
define anomalous chargeability. Distances indicated in this news release are approximate. The 2023 MRE
demonstrated mineralization in the East, Bornite, Pass and Camp zones is open-ended in three directions. The
correlation between mineralization and chargeability , the geometry of the anomalous chargeability signature
outlined in 2025, and the depth of drilling in the Bornite zone (average 210m vertical distance) supports the
current interpretation that the mineralization outlined by drilling represents the upper portion of the porphyry
system (Figure-2).
Future Work Plans
Copper Fox has tasked DIAS, to merge the data from the 2014-2025 geophysical surveys to provide updated
chargeability and resistivity plans and sections covering an area measuring approximately 5 ,000m by 4,000m
(Figure-3). Copper Fox plans to use these data sets to better define the distribution of the intrusive phases and
alterations associated with the four deposits of porphyry style copper -gold-molybdenum-silver mineralization
outlined in the 2023 MRE. The focus would be to better define the extent and geometry of the biotite granodiorite,
the primary host for the porphyry style mineralization.
Figure-3:Map showing the locations of the 2014-2025 geophysical surveys to be merged into the compilation.
Survey Specifications
The geophysical survey totaled 19.7-line kilometers and was completed in 14 days (11 days for data acquisition,
and 3 days for equipment layout ) The Ground/Wire Length (“infinity line”) for the survey was 21.2km. DIAS
32 is a distributed array system, comprising single -channel receivers, equipped with battery, time series data
recording, cable-free mesh networking and GPS.
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The Eaglehead Project
The Eaglehead project covers an intrusion hosted calc -alkalic polymetallic (Cu -Mo-Au-Ag) porphyry copper
system (i.e. like the porphyry deposits in the Highland Valley district of BC) located in the prolific Quesnel
Terrain approximately 50 kilometers (km) east of Dease Lake, BC. The property covers 15,713ha centered over
the Late Triassic-Early Jurassic (195Ma) granodioritic/dioritic Eaglehead batholith. The exploration target is an
8km by 3km zone of altered and mineralized rocks located along the southern margin of the batholith referred to
as the “mineralized corridor” that hosts four open-ended deposits and two large zones of porphyry style copper -
molybdenum-gold-silver mineralization and associated alteration located along the apex of an open-ended 6kms
long chargeability anomaly. The spatial relationship between porphyry mineralization and chargeability suggests
continuity of the mineralization between the deposits and down dip along the flanks of the chargeability anomaly.
Qualified Person
Elmer B. Stewart, MSc. P. Geol., President and CEO of Copper Fox, is the Company’s non-independent,
nominated Qualified Person pursuant to National Instrument 43-101, Standards for Disclosure for Mineral
Projects, has reviewed and approved the scientific and technical information disclosed in this news release.
About Copper Fox
Copper Fox is a Canadian resource company focused on copper exploration and development in Canada and the
United States. The principal assets of Copper Fox , and its wholly owned subsidiaries being Desert Fox Copper
Inc. and Northern Fox Copper Inc. are the 100% ownership s of the Van Dyke ISCR project, and the Mineral
Mountain and Sombrero Butte porphyry copper exploration projects all located in Arizona, the 25% interest in
the Schaft Creek Joint Venture with Teck Resources Limited on the Schaft Creek copper -gold-molybdenum-
silver project and the 100% owned Eaglehead polymetallic porphyry copper project each located in northwestern
British Columbia. For more information on Copper Fox’s mineral properties and investments visit the Company’s
website at www.copperfoxmetals.com.
On behalf of the Board of Directors
Elmer B. Stewart
President and Chief Executive Officer
For additional information contact: Lynn Ball at [email protected] or 1-844-464-2820
Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of
the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
Cautionary Note Regarding Forward-Looking Information
This news release contains “forward -looking information” within the meaning of the Canadian securities laws.
Forward-looking information is generally identifiable by use of the words “believes,” “may,” “plans,” “will,”
“anticipates,” “intends,” “budgets ,” “could,” “estimates,” “expects,” “forecasts,” “projects” and similar
expressions, and the negative of such expressions. Forward-looking information in this news release includes
statements regarding: a geophysical survey; updated chargeability and resistivity models ; defining the potential
size of the mineralized envelope ; an indication on the porphyry potential of the Eaglehead project and the
mineralized corridor.
In connection with the forward -looking information contained in this news release, Copper Fox and its
subsidiaries have made numerous assumptions regarding, among other things: that the geological, financial, and
economic advice that Copper Fox has received is reliable and is based upon practices and methodologies which
are consistent with industry standards . While Copper Fox considers these assumptions to be reasonable, these
assumptions are inherently subject to significant uncertainties and contingencies.
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Additionally, there are known and unknown risk factors which could cause Copper Fox’s actual results,
performance or achievements to be materially different from any future results, performance or achievements
expressed or implied by the forward -looking information contained herein. Known risk factors include, among
others: the preliminary interpretation of the chargeability and resistivity data may be erroneous ; the updated
chargeability and resistivity models may not be completed as planned or at all ; the results of the geophysical
survey may not be representative of porphyry mineralization; the chargeability signature may not define the
potential size of the mineralized envelope; the anomalous chargeability may not be an indication on the porphyry
potential of the Eaglehead project ; the mineralized corridor may not host additional porphyry copper style
mineralization; fluctuations in copper prices, demand, commodity prices, and currency exchange rates; conditions
in the financial markets; the overall economy may deteriorate; the need to obtain additional financing to develop
properties and uncertainty as to the availability and ter ms of future financing; the possibility of delay in
exploration or development programs or in construction projects and uncertainty of meeting anticipated program
milestones; and uncertainty as to timely availability of permits and other governmental approvals.
A more complete discussion of the risks and uncertainties facing Copper Fox is disclosed in Copper Fox's
continuous disclosure filings with Canadian securities regulatory authorities at www.sedarplus.ca. All forward-
looking information herein is qualified in its entirety by this cautionary statement, and Copper Fox disclaims any
obligation to revise or update any such forward -looking information or to publicly announce the result of any
revisions to any of the forward -looking information contained herein to reflect future results, events, or
developments, except as required by law.