Red Canyon Completes Kendal Ridge Targeted Drill Program and Expands Soil Geochemistry Survey
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Red Canyon Completes Kendal Ridge Targeted Drill Program and
Expands Soil Geochemistry Survey
Vancouver, British Columbia, November 13, 202 5: Red Canyon Resources Ltd. (“Red
Canyon” or the “Company”) (CSE: R EDC | OTCQB: REDRF) is pleased to announce it has
completed a Phase 2 targeted diamond drill program and an expanded soil geochemistry
sampling program on its 100% owned Kendal copper project in west-central British Columbia.
The Company controls a portfolio of seven 100%-owned1, internally generated copper and copper
– gold projects in British Columbia and the Western United States.
Company Highlights:
• The Company completed five diamond drill holes totalling 2,548 m, targeting a 500 by 500
m area at the Kendal Ridge zone within the interpreted 4 by 3 km Kendal hydrothermal
system. Kendal Ridge is the Company’s most advance d target area hosting elevated
copper and molybdenum (moly) in altered porphyritic and volcanic rocks with high
porphyry-style vein densities.
• All diamond drill holes intersected porphyry-style B veins with variable pyrite, chalcopyrite,
and moly within propylitic and sericite-chlorite (SC) altered porphyry intrusions and
volcanic rocks. Alteration, vein densities, and increasing copper/moly mineralization are
interpreted to be strongest along the eastern flanks of Kendal Ridge and to the east.
• Importantly, drill hole RCKD-25-006 drilled easterly from Kendal Ridge transected a major
north/south structure beneath the Moly Fork drainage before entering an eastern
continuation of the mineralized porphyry system. The Moly Fork structure is interpreted to
be a significant, long-lived fluid pathway, potentially important in the genesis of the Kendal
system.
• The strongest portion of the resistivity high geophysical feature identified on the Moly Fork
trend remains untested. Furthermore, the area immediately east of Kendal Ridge hosts
breccias with copper/moly mineralization and high-grade hypogene chalcocite veining with
select grades of up to 27.5% copper.
• In H2 2025, to further unveil the expanded potential of the Kendal system, the Company
completed a large-scale soil sample geochemistry program consisting of 252 samples to
target areas with limited or variable rock exposure. Assay results from all Kendal programs
are expected in late 2025 or early 2026.
Wendell Zerb, the Chairman and CEO of the Company, states: "We’ve successfully completed
the 2025 targeted Kendal Ridge drill program , which intersected copper and moly mineralized
porphyry veins throughout all drill holes. This small program was an important test of the Kendal
Ridge zone and dramatically improved our understanding of mineralizing and structural features
driving the large hydrothermal system at Kendal. The Kendal Ridge zone hosts some of the
highest vein densities we’ve encountered to-date at Kendal and our early interpretations suggest
the strongest vector to a possible porphyry centre is east of recent drilling. Importantly, this vector
direction is associated with complex magnetic , conductive and resistive signatures, mapped
copper-bearing breccias and high-grade hypogene chalcocite veining. We recently completed an
expanded soil geochemistry program to improve our vectoring within this large-scale
hydrothermal system that could host multiple copper porphyry centres.”
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Kendal Project
Kendal c omprises five 100%-owned mineral claims tota lling 2,738 hectares located in west -
central British Columbia approximately 25 km northeast of the city of Terrace, a regional
infrastructure hub with a well -serviced airport. Infrastructure is excellent with four intersecting
highways, hydroelectric power, rail corridors and port facilities approximately 120 km to the west
at Prince Rupert. The main project area has direct logging road access, 8 km east from Highway
16. The project area lies within the traditional territory of the Kitselas First Nation.
Figure 1: Kendal project location and infrastructure map with Red Canyon claims.
Kendal Ridge Targeted Drill Program
Red Canyon recently completed five diamond drill holes totalling 2,548 m testing a portion of the
road-accessible Kendal Ridge zone, located within the southwestern portion of the 4 by 3 km
interpreted hydrothermal system at Kendal . Kendal Ridge drilling targeted areas combining
anomalous copper and moly surface lithogeochemistry, high porphyry-style vein densit ies,
thorium/potassium (Th/K) ratio lows, complex magnetic signatures, and conductive and resistive
zones identified by the recent Mobile MT survey conducted at Kendal (Figures 2, 3, 4, and 5).
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Figure 2: Kendal Project topographic orthophoto looking south, with outline of interpreted alteration and
anomalous geochemical footprint (yellow line).
The drill program tested an area of Kendal Ridge spanning approximately 500 by 500 m, from
three drill locations - all were road/trail accessible from the west and south side of Kendal Creek
(Figures 2, and 3).
Drilling predominantly tested the eastern margins of Kendal Ridge (Figure 4), highlighted by high
vein densities, stronger overall alteration, and increasing copper and moly vein abundance. Drill
holes tested along the eastern margin of Kendal Ridge to identify vectoring trends to a possible
porphyry centre.
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Figure 3: Mobile MT resistivity model slice at 300 masl. Kendal project interpreted footprint of hydrothermal
system is defined by an extensive zone of relative high conductivity (resistivity low).
Based on core logging, stronger mineralization appears to be vectoring to the east (Figures 3, 4).
Importantly, drill hole RCKD-25-006, drilled easterly from Kendal Ridge, transected a major north-
south structure at Moly Fork before entering the eastern continuation of the mineralized porphyry
system. The Moly Fork structure is interpreted to be a significant, long -lived fluid pathway,
potentially important in the genesis of the Kendal system. The strongest portion of the resistivity
high identified on the Moly Fork trend remains untested (Figure 4). Furthermore, the area
immediately east of Kendal Ridge hosts known copper -bearing brecci as and high -grade
hypogene chalcocite veining grading up to 27.5% copper (Figures 3, and 7).
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Figure 4: Kendal Ridge Targeted Drill Plan , map background is Mobile MT resistivity model slice at 300
masl.
RCKD-25-007, drilled west across Kendal Ridge (Figure 4), tested a more conductive zone with
a higher overall magnetic response, possibly linked to increased sulphide mineral content in
altered volcanic rocks intruded by porphyry dykes. Overall, alteration is weaker and vein densities
are less robust.
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Figure 5: Mobile MT Inversion modeled resistivity cross section 1220 looking northeast.
Areas with high resistivity and subdued magnetic responses within the Kendal Ridge zone appear
closely associated with altered porphyry intrusions, hosting multiple generations of complex
porphyry-style veins and variable alteration. These porphyry intrusions are important mineralized
hosts based on significant alteration and multiple generations of B -style veining throughout.
Importantly, the porphyry intrusions identified to -date are not interpreted to be the causative
intrusion at Kendal, which has not yet been identified.
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Figure 6: RCKD-25-006 NQ drill hole showing an altered porphyry intrusion and associated B-style veins.
Much of the observed alteration at Kendal is dominantly sericite -chlorite (SC) ; however, the
presence of mineralized B -style veins, which are know n to form in association with potassic
altered fluids, suggests that SC alteration is overprinting earlier potassic alteration. Field work and
recent drilling identified B-style veins continuing into the Kendal Ridge area, extending the known
area of potassic-related fluids west-southwest over a minimum strike length of 1.5 km. The Kendal
system can be considered characterized by a large zone of potassic -related porphyry style
mineralized veining with SC overprinting. Drilling has tested only a small portion of this footprint.
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Expanded Soil Geochemistry Program
In H2 2025, the Company completed a large-scale soil sample geochemistry program consisting
of 252 samples to target areas with limited or variable rock exposure at Kendal (Figures 2, 7).
Figure 7: 2025 Expanded soil sample locations underlain by Mobile MT resistivity raster at 300 masl.
Soil samples were preferentially collected from lowermost B-horizon soils using a soil auger to
penetrate through the organic rich upper layers. Red Canyon’s program is designed to produce a
project scale overview using a consistent sampling approach and robust modern multi-element
ICP analyses.
Assay results from all Kendal programs are expected in late 2025 or early 2026.
About Red Canyon Resources
Red Canyon Resources Ltd. (CSE: REDC | OTCQB: REDRF) is a geoscience-driven, discovery-
focused mineral exploration company exploring North America’s top copper jurisdictions. Red
Canyon has a portfolio of 100% owned 1 copper and copper-gold porphyry exploration projects.
The Company’s technical team consists of experienced geoscientists with diverse capital market,
small cap and major mining company backgrounds, and a track record of success.
For more information, please visit the Company's website at www.redcanyonresources.com.