District Copper Seeks Extension to Private Placement
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Suite 700 - 838 West Hastings St., Vancouver, BC V6C 0A6
Telephone: (604) 363-3506
www.districtcoppercorp.com
NEWS RELEASE
DISTRICT COPPER SEEKS EXTENSION TO PRIVATE PLACEMENT
Vancouver, B.C. June 2, 2025 – District Copper Corp. (“District C opper”, “District”, or t he “Company”)
(TSX-Venture: DCOP) announces that, further to its news releases dated April 23, 2025, April 30, 2025, and
May 30, 2025, it will be seeking a 30- day extension in which it has to closed the balance of its private
placement. To date, the Company has closed on 3,830,000 Units on April 30, 2025, having a hold period
expiring August 31, 2025 and 1,800,000 Units on May 30, 2025, having a hold period expiring on October 1,
2025) raising gross proceeds $281,500.
About the Copper Keg property
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 intrude s 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
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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 mineralogy typical of a l each cap.
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 leach cap to a porphyry system.
Soil sampling in 2024 encountered highly anomalous values located on the newly 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 compa ny engaged in the exploration for porphyry copper deposits in south -
central Br itish Columbia .
For further information, please visit www.districtcoppercorp.com to view the Company’s profile or contact
Jevin Werbes at 604-363-2506.
Jevin Werbes, President & CEO
Nei t her the TSX Ventu re Exchange nor its Regula tion Servi ces Provider (as that term is d efined i n the
policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
This news release does not constitute an offer to sell or a solicitation of an offer to sell any of the securities
described herein in the United States. The securities described in this news release have not been and will
not be registered under the United States Securities Act of 1933, as amended (the "U.S. Securities Act") or
any state securities laws and may not be offered or sold within the United States or to U.S. Persons unless
registered under the U.S. S ecurities Act and applicable state securities laws or an exemption from such
registration is available. This news release is not for distribution in the United States or over United States
newswires.
Cautiona
ry Statement on Forward Looking Statement
Certa in inf ormation 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 perf ormance, const itute “forward l ooking statements”. Actual re sults may diffe r
materially f rom t hose indicated by such statement s. All statement s, other than hist orical fact, include d
herein, incl uding, without limitations statement s r egarding future produc tion, are f orward-looking
statements that in volve various risks and un certainties. There c an 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
c onnection with the forw ard-looking informati on c ontained in this news release, District C opper ha s
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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; unc ertainties 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.