Saturday, September 26, 2026
MiningNewsTerminal
Saturday, September 26, 2026 Admin

XTM.V ·

Transition Metals Further Defines Cu-Au Porphyry Targets at Pike Warden, Yukon ZTEM™ survey highlights prominent conductivity feature under cover within area dubbed Copper Junction Fieldwork highlights prospective porphyry target at Copper Junction, coincident with

Exploration Programs Sampling & Geoscience Results

Transition Metals Further Defines Cu-Au

Porphyry Targets at Pike Warden, Yukon

ZTEM™ survey highlights prominent conductivity feature under cover within area

dubbed Copper Junction

Fieldwork highlights prospective porphyry target at Copper Junction, coincident with

prospective alteration and copper mineralization

Four new polymetallic showings discovered, with samples returning assay values up to

1.04 g/t Au, 3.63% Cu, 1.37% Mo, 2.6% Zn, and 0.12% W

Sudbury, Ontario--(Newsfile Corp. - August 22, 2024) - Transition Metals Corp. (TSXV: XTM)

("Transition" or "the Company") is pleased to provide an update on exploration work completed at its

Pike Warden project ("the Property") located near Whitehorse, Yukon. This summer, the Company's

exploration team focused on areas of the property considered prospective for hosting porphyry Cu-Au

mineralization, including Copper North, Copper Junction, and Olympus (Figure 1). The work involved

collecting samples and data to better characterize the geology, structure, alteration, fracture and vein

density, and vein types in these areas, as well as sampling any prospective-looking mineralization.

Final data from the Z-Axis Tipper Electromagnetic system (ZTEM™) survey, flown by Geotech Ltd. over

Pike Warden (see news release dated

June 22, 2024

), has been received. Notably, the Company's

preliminary interpretation of the ZTEM™ data highlights a large conductivity anomaly located centrally

within one of the more prominent areas of prospective alteration and elevated copper mineralization,

Copper Junction.

Scott McLean, P.Geo., CEO of Transition Metals, commented,

"We are encouraged that our work

continues to highlight some compelling untested Cu-Au porphyry targets. Our geological team is

actively collaborating with our geophysical consultants to prioritize key targets on the property in

preparation for drilling."

Figure 1:

Pike Warden project map, with prominent structural trends, discovered polymetallic

showings, and recent highlight samples.

To view an enhanced version of this graphic, please visit:

https://images.newsfilecorp.com/files/2766/220787_eb389c1644b0da0e_002full.jpg

Sampling Results

In total, 79 samples were submitted for analysis, returning values of up to 1.04 g/t Au, 3.63% Cu, 1.37%

Mo, 2.61% Zn, and 0.12% W from regions of outcropping and scree mineralization. This work has

confirmed four new mineralized showings, named Steam, Whistle, Contrition, and Daedalus (Figure 1).

With the addition of these new zones, the total number of mineralized showings on the property now

stands at twenty-nine.

During the sampling conducted this summer, 92% of the collected samples were found to contain

elevated levels of pathfinder elements, which are used to vector towards centers of mineralization.

Notably, 47% of these samples exhibited anomalous concentrations of key metals, including copper,

gold, silver, molybdenum, zinc, lead, and tungsten. These elevated and anomalous values contribute to

the company's growing database, providing valuable insights for ongoing exploration. Select highlighted

values are presented above to showcase the potential of the area. However, the reader is cautioned that

only select highlight values are reported, that rock samples (bedrock and scree) are selective by nature,

and that values reported may not represent mineralization of the entire project area.

Transition Metals adheres to rigorous sampling and analytical protocols that meet or exceed industry

standards. Samples are securely stored until they are transported in batches to the ALS Geochemistry

facility in Whitehorse, Yukon. Each sample batch includes certified reference materials, blanks, and

duplicates, all processed under the control of ALS. The samples were analyzed in Vancouver by ALS

Chemex, with ALS Laboratories' quality system meeting the requirements of International Standards

ISO/IEC 17025:2005 and ISO 9001:2015. The analysis was conducted using the ME-MS61 method,

which reports 48 elements through four-acid digestion followed by ICP-MS. Gold was analyzed using the

AU-ICP21 method, involving fire assay fusion with an ICP-AES finish. In cases of over-limit results, gold

was determined by fire assay with a gravimetric finish, and base metals were analyzed using ore-grade

(OG62) four-acid digestion with an ICP-AES finish.

Copper Junction

This summer's work highlights the potential of the Copper Junction area to host a large-scale copper

porphyry system. In this region, the Company's preliminary interpretation of the recently completed

ZTEM™ survey identifies a prominent east-west magnetic low trend that crosscuts a northeast-

southwest trend of elevated conductivity. This feature, one of several identified on the Property, is

centrally located within the expanded alteration and copper mineralization footprint in the Copper

Junction area (Figure 2). Condor North Consulting ULC ("Condor") is currently further processing and

refining the ZTEM™ geophysical data.

The conductivity feature identified at Copper Junction occurs at the intersection of two significant

structural trends. The first trend is associated with an east-west striking concentric feature, interpreted as

a collapse structure related to the Bennett Lake caldera complex. The second trend follows a cluster of

northeast-trending features which host the majority of the copper and molybdenum mineralization, as well

as the epithermal-style base and precious metal occurrences identified to date on the property. These

northeast-trending structures appear to also control increased fracture and vein density, enhanced

potassic alteration, and sites of copper mineralization peripheral to the defined ZTEM™ conductivity

feature located under cover within the Copper Junction region.

Figure 2:

A photograph of the Copper Junction area looking west-southwest, illustrating the location of

copper mineralization, including the new Whistle and Steam showings, in relation to the east-west

structure and the ZTEM™ conductivity feature.

To view an enhanced version of this graphic, please visit:

https://images.newsfilecorp.com/files/2766/220787_eb389c1644b0da0e_003full.jpg

Next Steps

The Company plans to use the recently collected geological information, along with the geophysical

interpretations and 3D inversion models, to assist in refining areas prospective for hosting porphyry-style

copper-gold mineralization on the Property. The exploration team will continue to evaluate and prioritize

this data in preparation for drill testing.

The recent field program included detailed geological mapping, particularly around potential porphyry

target centers, with a focus on fracture density, vein styles, dike types, alteration abundance, alteration

intensity, and mineralization associations. These activities have generated a significant amount of new

data, which will be used to refine the Company's geological model of the Property. This includes

analyzing altered, unaltered, and mineralized samples in geological studies to investigate the geological

environment, pressure-temperature fluid evolution, and the broader mineralizing system preserved on the

Property

About the Pike Warden Property

The Pike Warden property (Figure 1) is located in the traditional territory of Carcross/Tagish First Nation

and is situated on the northern rim of the Bennett Lake Caldera Complex, one of the largest extinct

volcanic centers in Canada.

The property is located approximately 65 kilometres southwest of Whitehorse, Yukon, and is composed

of 203 contiguous mining claims totaling approximately 41 km². The property encompasses a

combination of historic and recently discovered high-grade polymetallic gold, copper, and silver

epithermal showings that are indicative of a large epithermal-porphyry system in the vicinity of the

Bennett Lake Volcanic Complex. In June 2022, Transition entered into an option agreement to acquire a

100% interest in the property from the Vendor in exchange for cash, shares, and work expenditures over

a four-year period (see Company news release dated

June 28, 2022

).

Qualified Person

The technical elements of this news release have been approved by Mr. Benjamin Williams, P.Geo.

(PGO), Senior Geologist of Transition Metals Corp. and a Qualified Person under National Instrument

43-101.

About Transition Metals Corp.

Transition Metals Corp. (TSXV: XTM) is a Canadian-based, multi-commodity explorer. Its award-winning

team of geoscientists has extensive exploration experience which actively develops and tests new ideas

for discovering mineralization in places that others have not looked, often allowing the company to

acquire properties inexpensively. Joint venture partners earn an interest in the projects by funding a

portion of higher-risk drilling and exploration, allowing Transition to conserve capital and minimize

shareholder's equity dilution. Further information is available at

www.transitionmetalscorp.com

or by

contacting:

Scott McLean

President and CEO

Transition Metals Corp.

Tel: (705) 669-1777

Cautionary Note on Forward-Looking Information

Except for statements of historical fact contained herein, the information in this news release constitutes

"forward-looking information" within the meaning of Canadian securities law. Such forward-looking

information may be identified by words such as "plans", "proposes", "estimates", "intends", "expects",

"believes", "may", "will" and include without limitation, statements regarding estimated capital and

operating costs, expected production timeline, benefits of updated development plans, foreign exchange

assumptions and regulatory approvals. There can be no assurance that such statements will prove to be

accurate; actual results and future events could differ materially from such statements. Factors that could

cause actual results to differ materially include, among others, metal prices, competition, risks inherent in

the mining industry, and regulatory risks. Most of these factors are outside the control of the Company.

Investors are cautioned not to put undue reliance on forward-looking information. Except as otherwise

required by applicable securities statutes or regulation, the Company expressly disclaims any intent or

obligation to update publicly forward-looking information, whether as a result of new information, future

events or otherwise. Neither the 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.

To view the source version of this press release, please visit

https://www.newsfilecorp.com/release/220787