District Copper Commences Summer Field Program at Copper Keg

Vancouver, May 15, 2025 - District Copper Corp. (TSXV: DCOP) ("District Copper", "District", or the "Company") is pleased to announce that crews have mobilized and field work is underway on its flagship Copper Keg porphyry copper project in the Kamloops mining Division, BC. The project covers 6628 ha and is located at the northern end of the Guichon batholith, approximately 20 kms north of the porphyry copper deposits currently being mined by Teck Resources Ltd..
The 2025 program is planned as a multi-phase program with its initial objective to complete a preliminary reconnaissance of the entire project area collecting detailed data on features that characterize the porphyry copper deposit in the Highland Valley mining district. Phase 1 of the planned program focuses on differentiating various intrusive phases of the Guichon Creek Batholith, contact relations with the older Nicola Volcanics, alteration styles, mineralogical associations and mineralized structures to prioritize areas for additional follow-up exploration. The data collected in the initial phase would also be used to complete a re-interpretation of the results of the airborne and ground geophysical surveys in the context of a porphyry copper model for the project which sets the basis for Phase 2 of the 2025 exploration program.
Jevin Werbes, CEO, commented "District Copper is excited to get the 2025 exploration program underway. We are incorporating the historical exploration data into a pragmatic approach for our exploration effort by establishing an exploration model for Copper Keg based on the porphyry copper deposits in the Highland Valley. We feel this approach provides a results-based approach to guide the planned exploration in 2025."
About the Copper Keg property
The following summary of historical exploration has been derived from the publicly available assessment reports on file with the Ministry of Mines for British Columbia. Historical exploration spans from the late 1800's to 2012. The early-stage exploration is reported to consist of mining high grade copper veins.
The property exhibits the geochemical/alteration/lithologic features typical of the argillic altered portion of a porphyry copper system at/along the potassic/propylitic contact. The property is characterized by a large, pyrite bearing, argillic zone exposed along the surface trace of the Barnes Creek fault, a major NNW trending that crosses the Guichon Creek Batholith. The high-grade copper veins noted above, reflect supergene enrichment of distal base metal veins typically associated with a porphyry copper system.
The project is underlain by an intrusive phase of the Guichon Creek batholith which intrudes the surrounding Nicola Group rocks.
Petrographic work and K/Al: Na/Al ratios indicate an alteration package ranging from argillic-phyllic- potassic (all alteration phases associated with porphyry copper systems) supported by alteration minerals indicative of the inner actinolite subzone of a porphyry system as well as secondary biotite (Potassic alteration) and sericite (phyllic alteration), quartz veinlets with pyrite and chalcopyrite.
A large pyritic zone exhibits spatial association with the argillic altered zone and could be representative of what is commonly referred to in porphyry copper terms as the "pyrite shell". Chalcopyrite, bornite and malachite (secondary copper carbonate) have been observed in outcrop and support the presence of a porphyry system.
Two highly altered gossans have been identified along the interpreted trace of the Barnes Creek fault, a major structure within the Guichon Creek batholith. The first area (800m long by 200m wide); the second area is 600 m south and smaller in extent. These gossans exhibit erratic copper concentrations, weak copper-silver soil anomalies and copper mineralization.
Since the Company acquired the property in 2021, it has completed mapping and prospecting, soil sampling, and ground and airborne geophysical programs. Results from this work are consistent with the presence of a porphyry copper system.
Soil sampling in 2024 located highly anomalous values on the recently acquired northern claims. Of the 520 samples, 8 returned values >100 ppm Cu (102.0, 122.2, 126.7, 132.2, 134.8, 136.9, 269.1 and 1517.4). This area is underlain by the Guichon Batholith, which hosts known copper porphyry deposits in this region, in contact with Nicola volcanics.
Qualified Person
Chris M. Healey, P.Geo., Chief Geologist, and a Director of District Copper Corp., is the qualified person under NI 43-101 guidelines who is responsible for the technical content of this release and approves its release.
About District Copper
District Copper is a Canadian company engaged in the exploration for porphyry copper deposits in south-central British Columbia.
For further information, please visit www.districtcoppercorp.com to view the Company's profile or contact Jevin Werbes at 604-363-2506.
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Jevin Werbes, President & CEO
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Cautionary Statement on Forward Looking Statement
Certain information contained in this news release, including information as to our strategy, projects, plans or future financial or operating performance and other statements that express management's expectations or estimates of future performance, constitute "forward looking statements". Actual results may differ materially from those indicated by such statements. All statements, other than historical fact, included herein, including, without limitations statements regarding future production, are forward-looking statements that involve various risks and uncertainties. There can be no assurance that such statements will prove to be accurate and actual results and future events could differ materially from those anticipated in such statements.
In connection with the forward-looking information contained in this news release, District Copper has made numerous assumptions regarding, among other things: the geological advice that District Copper has received is reliable and is based upon practices and methodologies which are consistent with industry standards and the reliability of historical reports. While District Copper 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 District Copper'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 dimensions and shape of the mineralized areas may not be as estimated; the targets outlined by the MVI study may not be associated with felsic intrusives porphyry style alteration or mineralization; the proposed surface program may eliminate these areas as potential targets for future exploration; the NNW trending structures may not contain indications of magnetite destruction typical of hydrothermal alteration; uncertainties relating to interpretation of the outcrop sampling results; the geology, continuity, and concentration of the mineralization; the financial markets and the overall economy may deteriorate; the need to obtain additional financing 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 District Copper is disclosed in District Copper'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 District Copper 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.
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www.districtcoppercorp.com
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