Canada One Provides Review of Exploration at Haul ROAD Zone, Copper Dome Project
#250 – 750 West Pender St. Vancouver, British Columbia, V6C 2T7
CANADA ONE PROVIDES REVIEW OF EXPLORATION AT HAUL ROAD ZONE, COPPER DOME
PROJECT
Vancouver, B.C., September 23, 202 5 - Canada One Mining Corp. (“Canada One ” or the
“Company”) (TSXV: CONE) (OTC: COMCF) (FSE: AU31) is pleased to provide a review of exploration
at the Haul Road Zone on its 100% owned Copper Dome Project , (“Copper Dome”, “Project” or
“Property”), Princeton B.C.
HAUL ROAD ZONE HIGHLIGHTS
Location, ~1.5 km south of the Copper Mountain Mine
Cohesive corridor: Reco Prospect, St. Louis Prospect, Elk No.1 Showing
Reco Prospect vein: chip sample, 0.5 m @ 0.89% Cu, 4.8 g/t Au
Secondary Reco Prospect vein: chip sample, 1.3% Cu, 4.98 g/t Au
Reco Prospect rock samples: Up to 93.3 g/t Au (select rock samples)
St. Louis Prospect footprint: 600 m sulphide halo (200–300 m wide)
Volcanic embayment trench: chip sample, 10 m @ 0.11% Cu (+ Au–Ag)
Elk No.1 Showing: K-spar pegmatites with bornite/malachite
Excellent camp setting: Intrusive–volcanic contacts beside an operating mine
Deep history: Historical 167 m tunnel; multi-decade work by majors
Peter Berdusco, President and CEO of the Company commented: “As we advance our systematic
work at Copper Dome, the Reco, St. Louis, and Elk No.1 mineral occurrences within the Haul Road
Zone outline a cohesive mineralized corridor along the Copper Mountain intrusive contact. Our strategy
is to progress the highest -confidence areas through focused mapping, sampling, and geophysics,
tightening the geologic model while maintaining disciplined capital allocation.”
Haul Road Zone Summary
The Haul Road Zone is located in the central portion of the Property, approximately 1 km east of the
Similkameen River and just 1.5 km south of the Copper Mountain Mine’s southern boundary. This
strategic location places the zone directly along the same intrusive– volcanic contact that has proven
highly productive at Copper Mountain (See Figure 1: “Location Map of the Copper Dome Project”).
Five historical mineral occurrences have been identified in this area - the Reco Prospect, St. Louis
Prospect, Johnston Showing, Enterprise Showing, and Elk No.1 Showing , outlining a cohesive
mineralized corridor with strong potential for copper-gold systems.
Recent sampling work has confirmed the presence of significant mineralization, particularly around the
Reco Prospect, where eleven rock samples were collected within 150 m of the historic al Adit. These
samples, largely composed of massive pyrrhotite, pyrite, and chalcopyrite (See Figure 2: “Map of Haul
Road Zone with Historical Rock Sample Locations and Results (Cu)”).
The combination of high- grade gold values, consistent copper mineralization, and the presence of
molybdenum credits highlights the Haul Road Zone as an emerging exploration focus within Copper
Dome. With multiple mineralized showings distributed across the corridor and its proximity to existing
mine infrastructure, the zone offers a compelling opportunity to expand on historical work and define
new copper-gold targets for future drilling.
Mineral Occurrences of the Haul Road Zone:
Reco Prospect
The Reco Prospect is cut by a sulphidic calcite vein within a 2–3 m shear zone striking 005° –040° and
dipping 80° northwest. The vein, traced on surface for 120 m and 0.1– 1.8 m wide, hosts lenses and
pods of massive sulphides (pyrrhotite, pyrite, minor chalcopyrite). A 0.5 m chip sample across a
pyrrhotite lens assayed 0.89% Cu, 4.8 g/t Au, and 1.9 g/t Ag 1, while a 1 m chip sample at the north
end assayed 0.40% Cu, 0.88 g/t Au, and 2.9 g/t Ag (1, p.18). Historical sampling from the 1940s reported
up to 17 g/t Au (1, p.18).
The vein is cut by a second less continuous quartz carbonate vein, 0.25 m wide. This structure is hosted
in a 2.5- m-wide shear zone striking north and dipping steeply west. The vein is mineralized with
stringers of pyrite and traces of chalcopyrite. A sample from this vein assayed 1.3 % Cu and 4.98 g/t
Au (1, p.18). Exploration began in 1907, when a 167 m tunnel was driven beneath the outcrops (1907–
1909). Subsequent operators conducted geological, geochemical, and geophysical surveys between
1968 and 1990.
In 2023, 11 rock samples were taken within 150 m of the Reco showing. Most of these samples were
taken from the Adit dump and consisted of massive pyrrhotite with pyrite and chalcopyrite. The samples
contained mainly copper and gold mineralization with values in copper for 10 of the samples varying
from 0.14% to 1.93%, and with values in gold for 7 of the samples varying from 0.14 to 93.3 g /t (1, p.
24).
St. Louis Prospect
The St. Louis Prospect is hosted in volcanic breccia, siltstone, and sandstone with minor andesitic and
cherty tuff of the Nicola Group. The Copper Mountain stock lies 120–250 m north. Mineralization forms
a 200–300 m wide pyrite– pyrrhotite zone extending 600 m east from the Reco Prospect, with >1%
sulphides as disseminations and fracture fillings (1, p.16).
The western portion of the prospect contains up to 10% pyrite in fractures, shears, and mafic breccia
fragments. Eleven historical grab and chip samples assayed 0.003–0.039% Cu and 0.1–0.4 g/t Ag (1,
p.17). The prospect was first assessed by Newmont Mining Corp. in 1970–71.
Johnston Showing
Rock sampling within the Johnston showing was taken in 2023 and consisted of two rock samples with
both being altered diorite and mineralized with malachite, chalcopyrite, and bornite. The assay returns
were 2.7% Cu 0.33 g/t Au for the one sample and 0.71% Cu for the other sample (1, p.25).
Backpack drilling was also done at this location. The rock encountered along one 8-foot (2.4 -m)
intersection was an altered microdiorite with malachite and azurite. The assay returns varied from 0.1%
Cu–0.39% Cu for the four two-foot (0.6-m) sections (1, p.25).
Enterprise Showing
Mineralization occurs within a 70–80 m–wide volcanic embayment (formerly Wolf Creek Fm.) projecting
~70 m NW into diorite of the Copper Mountain stock (Copper Mountain Intrusions). Volcanics show
pervasive to stringer biotite –carbonate alteration with albi tization. Chalcopyrite is disseminated and
along hairline fractures; pyrite is present in trace amounts where Cu is stronger. A 10-m chip sample
from a trench analysed 0.11% Cu, 0.038 g/t Au and 0.4 g/t Ag (1, p.18).
In 2023, two samples were taken at the showing with both described as being an altered diorite and/or
microdiorite mineralized with malachite, chalcopyrite, and/or bornite. One sample assayed 0.8% Cu
and 0.18 g/t Au while the other sample assayed 0.74% Cu and 0.27 g/t Au (1, p.25).
Elk No.1 Showing
In diorite of the Copper Mountain stock, ~80 m north of the Nicola Group contact, a 30 × 60 m area
hosts discontinuous K-feldspar (orthoclase) veinlets up to 12 m long and 8 cm wide, at low density (~1
veinlet/4.6 m). Wider veinlets include smoky quartz. M ineralization: malachite and bornite; analogous
to the stock’s common “red potash feldspar pegmatite” veins carrying bornite and chalcopyrite. Mapped
by Newmont (1970–71) (1, p.19).
Figure 1: Location Map of the Copper Dome Project
Figure 2: Map of Haul Road Zone with Historical Rock Sample Locations and Results (Cu)
About The Copper Dome Project
Copper Dome is located in the lower Quesnel Trough porphyry belt, one of British Columbia’s most
prolific mining districts. The Project directly adjoins Hudbay Minerals Inc.’s (TSX: HBM) producing
Copper Mountain Mine to the north which hosts Proven and Probable Reserves of 702 million tonnes
grading 0.24% Cu, 0.09 g/t Au, and 0.72 g/t Ag. Multiple mineralized zones have been identified across
the Property, with historical drilling confirming high- grade copper associated with northeast -trending
structures similar to those hosting mineralization at Copper Mountain.
The Project benefits from excellent infrastructure, enabling year -round access, cost -efficient
exploration, and a stable, low-risk jurisdiction.
Historical Work Completed
• Geophysics: 51 km of induced polarization (IP); airborne magnetic and electromagnetic (EM)
coverage over ~50% of the Property
• Sampling: 2,253 soils and 378 rocks collected
• Drilling: 8,900+ m of diamond drilling
• Trenching: Over 1 km excavated
With a five -year drill permit in place, the Company is focused on advancing the Project toward drill-
ready target definition.
About Canada One
Canada One Mining Corp. is a Canadian junior exploration company focused on copper —the critical
metal powering the global energy transition. The Company advances projects from discovery through
resource definition with disciplined, data- driven exploration and responsible practices. Its flagship
Copper Dome Project, near Princeton, British Columbia, targets a porphyry copper -gold system in a
Tier-1 jurisdiction. Canada One aims to deliver sustainable growth and long-term value for shareholders
and local communities.
Acknowledgement
Canada One acknowledges that the Copper Dome Project is located within the traditional, ancestral
and unceded territory of the Smelqmix People. We recognize and respect their cultural heritage and
relationship to the land, honoring their past, present and future.
Qualified Person
The technical information contained in this news release has been reviewed and approved by David
Mark, P.Geo., an independent Qualified Person for the purposes of National Instrument 43-101.
Note 1: Mark, (2024), Exploration Report on MMI Soil Sampling, Rock Sampling and Backpack Drilling on the Copper Dome Property
Copper Mountain Mine Area Similkameen Mining Division, British Columbia, AR 41492
Contact Us
For further information, interested parties are encouraged to visit the Company’s website at
www.canadaonemining.com, or contact the Company by email at [email protected], or by
phone at 1.877.844.4661.
On behalf of the Board of Directors of
CANADA ONE MINING CORP.
Peter Berdusco
President
Chief Executive Officer
Interim Chief Financial Officer
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