The Conversation (0)
Copper Fox Metals Inc. (TSXV: CUU,OTC:CPFXF) (OTCQX: CPFXF) (FSE: HPU) ("Copper Fox" or the "Company"), 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.
Figure-1: Shows the distribution of anomalous chargeability at a depth slice of approximately 400m below surface.
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/2177/263361_a98cba9c74ee0acd_001full.jpg
Figure-2: Showing a cross section of anomalous chargeability in the Bornite zone (see inset map).
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/2177/263361_a98cba9c74ee0acd_002full.jpg
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.
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/2177/263361_a98cba9c74ee0acd_003full.jpg
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.
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% ownerships 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 investor@copperfoxmetals.com 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.
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 terms 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.
To view the source version of this press release, please visit https://www.newsfilecorp.com/release/263361
View original content to download multimedia: 
Figure 1 – Location of Redstone's West Musgrave Project and the Tollu Cu Deposit relative to the world class Nebo-Babel Cu-Ni-Co Deposit and other deposits and prospects in the area. Information for deposits and prospects from DEMIRS Minedex, Cassini Resources Ltd ASX announcement of 7 December 2015 and Redstone Resources Ltd maiden JORC 2012 resource ASX announcement of 15 June 2016.
