TSXV: DMCU; OTCQB: DMCUF; FSE: 03E) announces the appointment of world-renowned Carbon Replacement Deposit (‘CRD’) expert Dr. Peter Megaw, Ph.D., C.P.G., as a technical advisor to the Company.

Dr. Megaw will be providing strategic and technical advice to senior management and assist Domestic in the ongoing exploration activities on its Smart Creek Copper Porphyry Project in Montana.

Dr. Megaw has a Ph.D. in geology from the University of Arizona and more than 30 years of relevant experience focused on silver and gold exploration in Mexico. He is a certified Professional Geologist by the American Institute of Professional Geologists and an Arizona Registered Geologist. Dr. Megaw has been instrumental in a number of mineral discoveries in Mexico including new ore bodies at existing mines, Excellon Resources’ Platosa Mine, and MAG Silver’s Juanicipio and Cinco de Mayo properties; discoveries for which he was given PDAC’s 2016 Thayer Lindsley Award. Peter is also a Director of Relevant Gold Corp. since 2021.

Gord Neal, CEO of Domestic Metals Corp., commented: ‘We warmly welcome Peter to the Domestic Metals’ team. I have worked closely with Peter before at MAG Silver and New Pacific Metals and admire his insatiable passion for large-scale economical mineral discoveries. Known as a world-renowned CRD expert, we look forward to Peter assisting us with exploration activities at our Smart Creek Copper Project which is proving to be highly indicative of both porphyry and CRD style mineralization.’

Webinar

Following the release of surface sampling results yielding up to 102 g/t Au, up to 23% Cu and up to 3,810 g/t Ag at the Smart Creek Project earlier this month, we have scheduled another webinar for January 22^nd to inform you of our follow up plans for Q1. We look forward to you joining us.

When: Thursday, January 22^nd at 1.15pm PST, 4.15pm ET, 10.15pm CET
Registration link: https://domestic-metals.eventbrite.com

Opportunity to Meet with Management

We appreciate meeting with our supporters and shareholders in person as well to provide a detailed update and as such are looking forward to seeing you at our booth #1101 at the VRIC in Vancouver on January 25-26, 2026 and booth #3139 at the Investors Exchange at the PDAC, March 1-4, 2026, in Toronto.

About Domestic Metals Corp.

Domestic Metals Corp. is a mineral exploration company focused on the discovery of large-scale, copper and gold deposits in exceptional, historical mining project areas in the Americas.

The Company aims to discover new economic mineral deposits in historical mining districts that have seen exploration in geologically attractive mining jurisdictions, where economically favorable grades have been indicated by historic drilling and outcrop sampling.

The Smart Creek Project is strategically located in the mining-friendly state of Montana, containing widespread copper mineralization at surface and hosts 4 attractive porphyry copper, epithermal gold, replacement and exotic copper exploration targets with excellent host rocks for mineral deposition.

Domestic Metals Corp. is led by an experienced management team and an accomplished technical team, with successful track records in mine discovery, mining development and financing.

On behalf of Domestic Metals Corp.

Gord Neal, CEO and Director
(604) 657 7813

Follow us on:
X, LinkedIn, Facebook and Instagram

For more information on Domestic Metals, please contact:
Gord Neal, Phone: 604 657-7813 or Michael Pound, Phone: 604 363-2885

Please visit the Company website at www.domesticmetals.com or contact us at info@domesticmetals.com.

For all investor relations inquiries, please contact:
John Liviakis, Liviakis Financial Communications Inc., Phone: 415-389-4670

Neither 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.

Cautionary Note Regarding Forward-Looking Statements

This news release contains certain statements that may be deemed ‘forward-looking statements’. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words ‘expects’, ‘plans’, ‘anticipates’, ‘believes’, ‘intends’, ‘estimates’, ‘projects’, ‘potential’ and similar expressions, or that events or conditions ‘will’, ‘would’, ‘may’, ‘could’ or ‘should’ occur. Forward-looking statements may include, without limitation, statements relating to the Company’s continued stock exchange listings and the planned exploration activities on properties. Although the Company believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance, are subject to risks and uncertainties, and actual results or realities may differ materially from those in the forward-looking statements. Such material risks and uncertainties include, but are not limited to: competition within the industry; actual results of current exploration activities; environmental risks; changes in project parameters as plans continue to be refined; future price of commodities; failure of equipment or processes to operate as anticipated; accidents, and other risks of the mining industry; delays in obtaining approvals or financing; risks related to indebtedness and the service of such indebtedness; as well as those factors, risks and uncertainties identified and reported in the Company’s public filings under the Company’s SEDAR+ profile at www.sedarplus.ca. Although the Company has attempted to identify important factors that could cause actual actions, events or results to differ materially from those described in forward-looking information, there may be other factors that cause actions, events or results not to be as anticipated, estimated or intended. Accordingly, readers should not place undue reliance on forward-looking statements. There can be no assurance that such information will prove to be accurate as actual results and future events could differ materially from those anticipated in such statements. Forward-looking statements are made as of the date hereof and, accordingly, are subject to change after such date. The Company disclaims any intention or obligation to update or revise any forward-looking information, whether as a result of new information, future events or otherwise unless required by law.

(TheNewswire)

Toronto, Ontario TheNewswire – January 19, 2026 Noble Mineral Exploration Inc. (‘Noble’ or the ‘Company’) (TSX-V:NOB, FRANKFURT: NB7, OTCQB:NLPXF) is pleased to announce the results of the first hole drilled in Carnegie Township near Timmins, Ontario, Canada.  The drill program is part of a 5050 partnership with Canada 11530313 Canada Inc. and will include two 500-meter holes that have been located to follow up on drilling done in 2019.  Recent analysis of downhole geophysics from that program indicated that conductors may have been missed and additional down hole geophysics has been done on the new hole (Figure 1).  Heavy snowfall and extreme low temperatures have hampered the drilling but the first hole is now complete, analyses received and down hole surveying done.

In drill hole CG-25-01, a 6.5m section analyzed 0.64% zinc with associated, anomalous values in copper, silver and lead from 141.0 to 147.5 meters down hole (true width not known at this time).  A 1-meter section within the wider section was found to run 1.90% zinc. The anomalous mineralization was found to occur in a weakly laminated sulphide rich graphitic sediment.  Mineralization consisted of about 5% pyrrhotite, with local concentrations of up to 10-15%.  

A Mise à la masse (MALM) survey was competed down hole in the anomalous section.  Mise-a-la-Masse (MALM survey) is a downhole geophysical technique used in exploration and mining to map conductive ore bodies by injecting current directly into them, revealing continuity and shape at surface.

Click Image To View Full Size

Figure 1: Mise à la masse (MALM) survey results projected to surface.  Red to pink colours represent the conductive horizon where anomalous zinc, copper, silver and lead values were intersected in hole CG-25-01.

A surficial magnetometer survey was conducted on the same grid as the MALM survey and detected a magnetic anomaly coincident with the MALM anomaly indicating that the zone is both magnetic and electromagnetic (Fig 2).  These properties will make it easier to trace the zone on surface with traditional surface geophysical techniques.

Click Image To View Full Size

Figure 2: Surficial magnetic survey over the same zone as the MALM survey.

Hole CG-25-02 is collared about 200m to the northwest to intersect the same zone at about 200-meter vertical depth.

An additional 1000m (2 holes) have been scheduled for Southwest Carnegie Township.

The program is being carried out on lands recently transferred to Canada Nickel but on which Noble retains a 5-year Exploration Right for volcanogenic massive sulphide mineralization and precious metals.

Vance White, President and CEO of Noble, said ‘We are very pleased to get this program started with the support of our partners at 11530313 Canada Inc. The search for mineralization similar to the Kidd Creek Mine continues.’

The technical content of this release has been reviewed and approved by Wayne Holmstead, P.Geo., an independent Qualified Person as defined by National Instrument 43-101 – Standards of Disclosure for Mineral Projects.

About Noble Mineral Exploration Inc.

Noble Mineral Exploration Inc. is a Canadian-based junior exploration company, which has holdings of securities in Canada Nickel Company Inc., Homeland Nickel Inc., East Timmins Nickel Inc. (20%), and its interest in the Holdsworth gold exploration property in the area of Wawa, Ontario.

Noble holds mineral and/or exploration rights in ~70,000ha in Northern Ontario and ~24,000ha elsewhere in Quebec upon which it plans to generate option/joint venture exploration programs.

Noble holds mineral rights and/or exploration rights in ~18,000 hectares in the Timmins-Cochrane areas of Northern Ontario known as Project 81, ~2,215 hectares in Thomas Twp/Timmins, as well as an additional 20% interest in ~38,700 hectares in the Timmins area held by East Timmins Nickel. Project 81 hosts diversified drill-ready gold, nickel-cobalt and base metal exploration targets at various stages of exploration. Noble also holds ~4,600 hectares in the Nagagami Carbonatite Complex and its ~3,200 hectares in the Boulder Project both near Hearst, Ontario.  ~3,700 hectares in the Buckingham Graphite Property, ~10,152 hectares in the Havre St Pierre  Nickel, Copper, PGM property, and ~1,573 hectares in the Cere-Villebon Nickel, Copper, PGM property, ~569 hectare Uranium/Rare Earth property (Chateau), ~461 hectare Uranium/Molybdenum property (Taser North),  ~4,465 hectares REE Mehmet Property, and the ~3300 hectare Gull Lake REE Property all of which are in the Province of Quebec and the ~ 647 hectare Chapiteau REE property in Labrador.

. https://www.noblemineralexploration.com

 Noble’s common shares trade on the TSX Venture Exchange under the symbol ‘NOB’.

 Cautionary Statement

 Neither 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. No stock exchange, securities commission or other regulatory authority has approved or disapproved the information contained herein.

The foregoing information may contain forward-looking statements relating to the future performance of Noble Mineral Exploration Inc. Forward-looking statements, specifically those concerning future performance, are subject to certain risks and uncertainties, and actual results may differ materially from the Company’s plans and expectations. These plans, expectations, risks and uncertainties are detailed herein and from time to time in the filings made by the Company with the TSX Venture Exchange and securities regulators.  Noble Mineral Exploration Inc. does not assume any obligation to update or revise its forward-looking statements, whether as a result of new information, future events or otherwise.

 Contacts: H. Vance White, President

Phone:        416-214-2250

Fax:                416-367-1954

Email:        info@noblemineralexploration.com

Investor Relations: info@noblemineralexploration.com       

Copyright (c) 2026 TheNewswire – All rights reserved.

(TheNewswire)

Vancouver, British Columbia TheNewswire – January 19, 2026 Juggernaut Exploration Ltd. (JUGR.V) (OTCPK: JUGRF) (FSE: 4JE) (the ‘Company’ or ‘Juggernaut’) is pleased to announce the inaugural fully funded 10,000 m drill program within the newly discovered district scale gold, silver, copper rich system on the 100% controlled Big One property (the ‘Property’), Golden Triangle, British Columbia. The Company’s maiden drill program will target several extensive high-grade gold, silver, copper-rich shear-hosted veins confirmed on surface within the district-scale Eldorado System and Gold Swarm discoveries. Widespread strong porphyry-style propylitic alteration and gold-rich polymetallic mineralization on the Big One property are indicated to be related to a Jurassic- to Cretaceous-age intrusive source coeval with the alkalic volcano-magmatic event that is associated with the copper-gold-silver porphyry mineralization as seen in close proximity at the adjacent Galore Creek deposit.

Link to Big One 2026 Video

Dan Stuart, CEO of Juggernaut Exploration, states: ‘With a district-scale discovery of this magnitude, host to >500 gold-rich veins and shears exposed on surface for >1 km that rise above the valley floor for >1 km, we are likely only seeing the tip of the iceberg. The Eldorado Gold system and the Gold Swarm Discovery show the right ingredients to quickly become the next major discovery in the Golden Triangle. Juggernaut Exploration is preparing to embark on its inaugural fully funded ~10,000-meter drill program at the Big One property, and we look forward to testing this high-grade district-scale system to depth and unlocking the full potential of this amazing discovery.’

Manuele (Lele) Lazzarotto, President and COO of Juggernaut Exploration states: ‘Preparations are underway for the 2026 fully funded inaugural drill program on one of the most highly anticipated new discoveries in the Golden Triangle. Recently received data from the detailed and regional mapping, LiDAR survey and UAV survey, in combination with excellent geochemical results and structural information has allowed us to vector in on and better understand the extent and geometry of the mineralization seen on surface where multiple high-grade gold, silver, copper veins are exposed for >1 km. The data indicates that the system driving the high-grade polymetallic mineralization at Big One is a magmatic source coeval with the nearby world class Galore Creek deposit. From an exploration perspective, this opens the door for the presence of a large causative mineralizing source at depth, characterized by major gold, silver, and copper-rich fluid pathways, providing significant additional discovery potential. Intersecting the causative source could greatly increase the value of the project in 2026 and beyond.’

Big One Gold-Rich District-Scale System Highlights:

• The district-scale Eldorado System covers an area of 22 km that remains wide open where grab samples assayed up to 263.70 g/t AuEq or 8.48 oz/t AuEq (256.60 g/t Au, 546.00 g/t Ag, 0.43 % Cu, 0.41 % Pb and 0.01 % Zn) from 400 mineralized veins that remain open and are up to 10 m wide, hosted in shear zones up to 50 m wide, and are exposed on surface for 500 m with 1 km of vertical relief.

Link to Gold Dome Figure

Link to Whopper Zone Figure

• The Gold Swarm Discovery is a 3 km area of strong gold potential with 100 gold-rich polymetallic veins exposed on surface for 200 m and up to 4.5 m wide with up to 700 m of vertical relief, where grab samples assayed up to 231.81 g/t AuEq or 7.45 oz/t AuEq(226.94 g/t Au, 335.00 g/t Ag, 0.00 % Cu, 4.99 % Pb and 0.01 % Zn) that remains open.

Link to Goldswarm Figure

• 41% (219 samples out of 527) collected within the Eldorado System in 2024 and 2025 assayed 1 g/t AuEq; 65% (28 samples out of 43) collected within the Gold Swarm Zone in 2024 and 2025 assayed 1 g/t AuEq.

Link to map with samples > 1 g/t AuEq

Gold samples up to 256.60 g/t or 8.25 oz/t, silver samples up to 2810 g/t or 90.34 oz/t, and copper samples up to 14.40 % were collected on Big One.

• The polymetallic veins, alteration signature, geochemical pathfinder element signature, and geophysical anomalies strongly indicate the presence of a large common buried gold, silver, copper-rich porphyry feeder source or similar magmatic source or sources at depth responsible for the extensive district-scale high-grade gold, silver, copper veining confirmed on surface.

• Detailed mapping has confirmed that mineralization at Eldorado and Gold Swarm is linked to a Jurassic to Cretaceous transpressional system and intrusive sources, coeval with the magmatic events that formed the nearby multi-million-ounce Galore Creek copper, gold, silver porphyry deposit.

• The district scale system shows widespread porphyry-style propylitic alteration, with the final phase of alteration occurring simultaneously with mineralization, which will help vector towards the potential source of the mineralization seen in the gold-rich shear zones and veins on surface that remain open.

• Mineralized veins and shear zones were emplaced through brittle-ductile deformation during and after the Jurassic period, forming a major structural corridor at Big One defined by northeast, east, and northwest trends, confirming common orientations as well as similar geochemical signatures and textures of the gold-mineralized veins along the 15 km Highway of Gold corridor surrounding the snowcap of Deeker Glacier strongly indicating that the gold-rich mineralization found throughout is all part of one district-scale gold system that remains open.

• The recently received 5-year drill permit, valid until March 31, 2031, will allow the Company to define the extent of the mineralization at depth as well as fully understand the geometry of the system and related drivers of the mineralization in preparation for a future resource.

The Eldorado System consists of a 22 Km2 area that remains open where grab samples assayed up to 263.70 g/t AuEq or 8.48 oz/t AuEq (256.60 g/t Au, 546.00 g/t Ag, 0.43 % Cu, 0.41 % Pb and 0.01 % Zn) from >400 mineralized veins that are up to 10 m wide hosted in shear zones up to 50 m wide, and are exposed on surface for >1 km with >1 km of vertical relief. The Eldorado System hosts the Gold Dome Zone where grab samples assayed up to 263.70 g/t AuEq or 8.48 oz/t AuEq (256.60 g/t Au, 546.00 g/t Ag, 0.43 % Cu, 0.41 % Pb and 0.01 % Zn), the Big Mac Zone where grab samples assayed up to 113.92 g/t AuEq or 3.66 oz/t AuEq (111.35 g/t Au, 159.00 g/t Ag, 0.02 % Cu, 3.88 % Pb and 0.01 % Zn), and the Whopper Zone where grab samples assayed up to 43.94 g/t AuEq or 1.41 oz/t AuEq (39.84 g/t Au, 333.00 g/t Ag, 0.02 % Cu, 0.07 % Pb and 0.06 % Zn). See news release from September 8, 2025, and November 10, 2025.

The Gold Swarm discovery is a 3 km2 area of strong gold potential with >100 gold-rich polymetallic veins exposed on surface for >200 m and up to 4.5 m wide with up to 700 m of vertical relief, where grab samples assayed up to 231.81 g/t AuEq or 7.45 oz/t AuEq (226.94 g/t Au, 335.00 g/t Ag, 0.00 % Cu, 4.99 % Pb and 0.01 % Zn) that remains open. See news release from September 8, 2025, and November 10, 2025.

Mineralization at Eldorado and Gold Swarm most likely represents part of a broader Jurassic- to Cretaceous-age transpressional mineralizing system directly related to an intrusive source. These Intrusives are indicated to be time equivalent to the alkalic volcano-magmatic event associated with Cu-Au porphyry mineralization that hosts the adjacent Galore Creek Deposit. Detailed geological mapping of the Eldorado system has revealed that the gold-rich polymetallic quartz veins are mostly hosted within and therefore post-date Early Jurassic quartz diorite and hornblende diorite units and associated compressional deformation events, but pre-date Eocene epithermal events. Widespread strong porphyry-style propylitic alteration has been mapped in outcrop on the eastern and northern slopes of the Eldorado system. Multiple phases of propylitic alteration have been observed, with two phases occurring prior to mineralization and the last phase occurring during mineralization. Syn- to post-Jurassic brittle-ductile deformation is responsible for the emplacement and activation of mineralized veins and shear zones, which consist of steep and low-angle structures and are concentrated in northeast, east, and northwest trends, indicating the presence of a major structural corridor at Big One.

The Big One property is situated in a region that is well known for hosting globally recognized precious metal and porphyry deposits, several of which occur near the property including the multiple porphyry systems at Galore Creek, the world’s largest known gold reserve at KSM and the polymetallic copper project at Shaft Creek, as well as the Brucejack high-grade epithermal gold deposit, and the structurally controlled high-grade hydrothermal gold-silver zones at Trophy and Sphal Creek. The property geology is favorable to host these types of deposits, as confirmed by the presence of extensive areas of propylitic alteration, untested geophysical anomalies, strong silt, soil, and rock geochemistry, including pathfinder elements directly related to porphyry systems, key structures and textures, porphyry-style mineralization, and high-grade polymetallic veins, that have been discovered on the Big One property.

The Big One property can be accessed year-round via helicopter from the Glenora/Telegraph Creek Road at the Barrington Mine (33 km to the north-northeast) as well as the Galore Creek Road (15 km to the southeast). The Canadian government committed $25 M to extend/improve the Galore Creek Road to within 15 km of the Big One property. The property is 2 km west of the Scud River airstrip used in the early days of Galore Creek.

The Big One property exploration qualifies for the Critical Mineral Exploration Tax Credit (CMETC).

About Juggernaut Exploration Ltd.

Juggernaut Exploration Ltd. is an explorer and generator of precious metals projects in the prolific Golden Triangle of northwestern British Columbia. Its projects are located in globally recognized geological settings and in geopolitically stable jurisdictions, making them amenable to mining in Canada. Juggernaut is a member and active supporter of CASERM, a collaborative venture between the Colorado School of Mines and Virginia Tech. Juggernaut’s key strategic cornerstone shareholder is Crescat Capital.

For more information, please contact:

Juggernaut Exploration Ltd.

Dan Stuart

Chief Executive Officer, Director

Tel: (604)-559-8028

www.juggernautexploration.com

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Qualified Person

Rein Turna, P. Geo, is the qualified person as defined by National Instrument 43-101, for Juggernaut Exploration projects, and supervised the preparation of, and has reviewed and approved, the technical information in this release.

Disclaimer

The reader is cautioned that grab samples are spot samples, which are typically, but not exclusively, constrained to mineralization. Grab samples are selective in nature and collected to determine the presence or absence of mineralization and are not intended to be representative of the material sampled.

QA/QC Protocol

Grab, channels, chip and talus samples were collected by foot with helicopter assistance. Prospective areas included, but were not limited to, proximity to MINFile locations, placer creek occurrences, regional soil anomalies, and potential gossans based on high-resolution satellite imagery. The rock grab and chip samples were extracted using a rock hammer, or hammer and chisel to expose fresh surfaces and to liberate a sample of anywhere between 0.5 to 5.0 kilograms. All sample sites were flagged with biodegradable flagging tape and marked with the sample number. All sample sites were recorded using hand-held GPS units (accuracy 3-10 meters) and sample ID, easting, northing, elevation, type of sample (outcrop, subcrop, float, talus, chip, grab, etc.) and a description of the rock were recorded on all-weather paper. Samples are then inserted in a clean plastic bag with a sample tag for transport and shipping to the geochemistry lab. QA/QC samples including blanks, certified reference materials, and duplicate samples are inserted regularly into the sample sequence at a rate of 10%.

All samples are transported in rice bags sealed with numbered security tags. The rice bags are transported from the core shacks to the MSALABS facilities in Terrace, BC. MSALABS is certified with both AC89-IAS and ISO/IEC Standard 17025:2017. The core samples undergo preparation via drying, crushing to ~70% of the material passing a 2 mm sieve and riffle splitting. The sample splits are weighed and transferred into three plastic jars, each containing between 300 g and 500 g of crushed sample material. A 250 g split is pulverized to ensure at least 85% of the material passes through a 75 µm sieve. The crushed samples are transported to the MSALABS PhotonAssayTM facility in Prince George, where gold concentrations are quantified via photon assay analysis (method CPA-Au1). Samples that result in gold concentrations ≥5 ppm are analyzed to extinction. Photon assay uses high-energy X-rays (photons) to excite atomic nuclei within the jarred samples, inducing the emission of secondary gamma rays, which are measured to quantify gold concentrations. The assays from all jars are combined on a weight-averaged basis. Multielement analyses are carried at the MSALABS facilities in Surrey, BC, where 250 g of pulverized splits are analyzed via ICF6xx and IMS-230 methods. The IMS-230 method uses 4-acid digestion (a combination of hydrochloric, nitric, perchloric and hydrofluoric acids) followed by inductively coupled plasma emission spectrometry to quantify concentrations of 48 elements. Samples with over-limit results for Ag, Cu, Pb, and Zn undergo ore-grade analysis via the ICF-6xx method (where ‘xx’ denotes the target metal). This method employs 4-acid digestion followed by inductively coupled plasma emission spectrometry.

Gold Equivalent (AuEq) metal values are calculated using: Au 4004.43 USD/oz, Ag 48.80 USD/oz, Cu 5.09 USD/lbs, Pb 2026.43 USD/ton, and Zn 3054.88 USD/ton on October 31, 2025. There is potential for economic recovery of gold, silver, copper, lead, and zinc from these occurrences based on other mining and exploration projects in the same Golden Triangle Mining Camp with a similar style of high-grade gold mineralization where Juggernaut’s project is located, such as the Brucejack Mine and the Homestake Ridge Gold Project. Here, AuEq values were calculated using multi-year running averages for metal price, and included provisions for metallurgical recoveries, treatment charges, refining costs, and transportation. Recoveries for Au, Ag, Cu, Pb, and Zn on Big One are unknown but are assumed to be similar, with 85% gold recovery, 75% silver recovery, 75% copper recovery, 75% zinc recovery, and 50% Pb recovery. The quoted reference of metallurgical recoveries is not from Juggernaut’s Big One project, and there is no guarantee that such recoveries will ever be achieved, unless detailed metallurgical work, such as in a Feasibility Study, is completed on the Big One project.

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.

FORWARD LOOKING STATEMENT

Certain disclosures in this release may constitute forward-looking statements that are subject to numerous risks and uncertainties relating to Juggernaut’s operations that may cause future results to differ materially from those expressed or implied by those forward-looking statements, including its ability to complete the contemplated private placement. Readers are cautioned not to place undue reliance on these statements.

NOT FOR DISSEMINATION IN THE UNITED STATES OR TO U.S. PERSONS OR FOR DISTRIBUTION TO U.S. NEWSWIRE SERVICES. THIS PRESS RELEASE DOES NOT CONSTITUTE AN OFFER TO SELL OR AN INVITATION TO PURCHASE ANY SECURITIES DESCRIBED IN IT.

Copyright (c) 2026 TheNewswire – All rights reserved.

Saga Metals Corp. (‘SAGA’ or the ‘Company’) (TSXV: SAGA,OTC:SAGMF) (OTCQB: SAGMF) (FSE: 20H), a North American exploration company focused on critical mineral discovery, is pleased to announce the assay results for two (2) additional diamond drill holes (R-0010 and R-0011) from the Company’s Q4 2025 Phase of the Mineral Resource Estimate (MRE) drill program in Trapper North at the Radar Ti-V-Fe Project, located near the port of Cartwright in Labrador, Canada.

Trapper North Assay Highlights

• Analytical results have now been obtained for all four (4) diamond drill holes in Trapper North Zone and constitute four (4) of eight (8) drill holes completed during the Q4 2025 Phase of the MRE drill program.
• Analytical results to-date include numerous oxide-rich intercepts, including:
  • R-0010: 135.50 m grading 50.03% Fe₂O₃, 7.87% TiO₂, and 0.352% V₂O₅.
  • R-0011: 95.15 m grading 39.49% Fe₂O₃, 6.49% TiO₂, and 0.220% V₂O₅.
  • R-0009: 87.20 m grading 50.67% Fe₂O₃, 10.15% TiO₂, 0.339% V₂O₅
  • R-0008: 67.60 m grading 46.15% Fe₂O₃, 9.21% TiO₂, 0.311% V₂O₅
• TiO₂ strength:
  • 42.6% of samples > 7% TiO₂ (700 samples majority of which are 2 m)
• V₂O₅ strength:
  • 53.7% of samples > 0.2% V₂O₅ (700 samples majority of which are 2 m)
• Continued consistency and increase in overall oxide concentration in Trapper Vs Hawkeye.

Assay Results from R-0010 and R-0011

• Hole R-0010 (collared at the same location as R-0009 but oriented at 0° azimuth for true width assessment): Intercepted 135.5 meters (from 1.5 m to 137 m) grading 50.028% Fe₂O₃, 7.872% TiO₂, and 0.352% V₂O₅.
• Hole R-0011 (100-meter step-out along strike from R-0009 and R-0010): Intercepted 95.15 meters (from 58.1 m to 153 m) grading 39.49% Fe₂O₃, 6.49% TiO₂, and 0.22% V₂O₅. Additionally, this hole also encountered a 22-meter interval of rhythmically banded oxide, suggesting more persistent layering occurs away from the concentrated mass in the fold nose.

For comparison with the rest of Trapper North, the following table summarizes key intercepts from all four drill holes completed in Q4 2025.

Table 1: Assay results and composites of R-0008, -0009, -0010 and -0011 from Trapper North.

Michael Garagan, CGO & Director of Saga Metals, commented: ‘The successful assay results from all four drill holes at Trapper North mark a significant milestone for the Radar Project. These latest intercepts from R-0010 and R-0011 confirm the continuity of high-grade mineralization along the northern limb. This structurally related increase in thickness boosts Trapper as a standout zone with tremendous potential for titanium, vanadium, and iron mineral resources, advancing our goal of establishing a strategic North American supply of critical minerals.’

Figure 1-3 below outline all four drill holes in Trapper North with the corresponding intercepts at different viewing angles for a complete, accurate picture of the subsurface geometry:

Figure 1: Cross-Section BB looking West showing R-0008, -0009, and -0010 highlighting high-grade intercepts with the 3D Magnetic Inversion of the 2025 Trapper Zone ground magnetic survey. For the full set of R-0008 & R-0009 assays see Figure 3 cross-section N-11.

Figure 2: Cross-Section AA looking West showing R-0008, -0009, and -0011 highlighting high-grade intercepts with the 3D Magnetic Inversion of the 2025 Trapper Zone ground magnetic survey. For the full set of R-0008 & R-0009 assays see Figure 3 cross-section N-11.

Figure 3: Cross-Section N-11 looking Northwest showing R-0008, -0009, -0010 and -0011 highlighting high-grade intercepts in holes R-0008 & -0009 with the 3D Magnetic Inversion of the 2025 Trapper Zone ground magnetic survey. For the assays of R-0010 & R-0011 see Figures 1 & 2 Sections BB & AA.

Trapper North Drill Hole Details and Geological Insights

Hole R-0010 was collared at the same location as R-0009 but re-oriented to a 0-degree azimuth (compared to the standard 38 degrees) in order to test the northern limb of the Trapper North Fold. Both holes maintained a -45-degree dip. This allowed the team to drill directly through the anomaly and oxide layering at an optimal angle, enabling precise correlation of structural data between R-0009 and R-0010 while clearly defining the northern contact and limits of the oxide layer.

Hole R-0011, drilled as a 100-meter step-out along strike from R-0009 and R-0010, successfully tracked the continuation of the semi-massive oxide layer that is particularly abundant through the nose of the fold. Notably, it also intercepted a 22-meter interval of rhythmically banded oxide. This zone provides an outstanding window into the deposit, featuring exceptionally high VTM content.

Additionally, deeper oxide layering in R-0011, appeared to shallow toward the northeast—an intriguing observation that could indicate a potential at-depth connection between the Trapper and Hawkeye zones, further supporting the theory that this section of the property is one large lopolith. While this remains theoretical at present, the team intends to test the concept with future drilling once additional data increases confidence in its likelihood.

Mineral Resource Estimate Focus

The drilling in Q4 2025 at Trapper North forms part of the Company’s broader strategy to advance toward a maiden Mineral Resource Estimate for the Radar Project. The economic target is the large, continuous sections of oxide mineralization (semi-massive to massive VTM and ilmenite layers) that demonstrate consistent and exceptional grades in titanium, vanadium, and iron—critical minerals for North American supply security needed in defense, aerospace, renewable energy, and steel production.

Drilling these extensive oxide zones provides essential data on grade, thickness, continuity, and geometry, enabling the definition of a robust resource. The exceptional results from Trapper North validate the priority of targeting these enriched structural features. The rhythmic banding seen in drill hole R-0011 and in Trapper South to-date adds to the overall consistency and exceptional mineralization across the entire Trapper Zone. These elements inform the ongoing 2026 drill campaign, designed to systematically grid and delineate these zones across the Trapper Zone for increased resource confidence.

Next Steps at the Radar Ti-V-Fe Project

Personnel are expected to arrive in Cartwright, Labrador, today, and drilling will commence shortly thereafter.

The initial focus for the 2026 Radar Project drill program will be in the southern section of the Trapper Zone, also known as ‘Trapper South.’ SAGA’s geological team and Gladiator’s drill crews will take advantage of the extensive trail network created in the summer of 2025, allowing for an easy traverse for snowmobiles and the excavator used to move the drill. Drilling will begin at the southeastern extent of Trapper South, targeting approximately 30 holes (7,500 m). The program will then advance hole by hole back toward Trapper North, positioning the team to complete the remainder of the MRE drill campaign by spring.

Figure 4: Trapper Zone map outlining location of the initial 2026 focus for remainder of the MRE drill program to be completed in 2026  showing the TMI of the 2025 Trapper Zone ground magnetic survey Drilling will commence in Trapper Zone and move to Trapper North.

About Radar Property

The Radar Property spans 24,175 hectares and hosts the entire Dykes River intrusive complex (~160 km²), a unique position among Western explorers. Geological mapping, geophysics, and trenching have already confirmed oxide layering across more than 20 km of strike length, with mineralization open for expansion.

Figure 5: Radar Property map, depicting magnetic anomalies, oxide layering and the site of the 2025 drill programs. The Property is well serviced by road access and is conveniently located near the town of Cartwright, Labrador. A compilation of historical aeromagnetic anomalies is overlaid by ground-based geophysics, as shown.

Vanadiferous titanomagnetite (‘VTM’) mineralization at Radar is comparable to global Fe–Ti–V systems such as Panzhihua (China), Bushveld (South Africa), and Tellnes (Norway), positioning the Project as a potential strategic future supplier of titanium, vanadium, and iron to North American markets.

Figure 6: Radar Project’s prospective oxide layering zone validated over ~16 km strike length through Fall 2025 drilling, as shown on a compilation of historical airborne geophysics as well as ground-based geophysics in the Hawkeye and Trapper zones completed by SAGA in the 2024/2025 field programs. SAGA has demonstrated the reliability of the regional airborne magnetic surveys after ground-truthing and drilling in the 2024 and 2025 field programs.

Qualified Person

Paul J. McGuigan, P. Geo., is an Independent Qualified Person as defined under National Instrument 43-101 and has reviewed and approved the technical information disclosed in this news release.

Technical Information

Samples were cut by Company personnel at SAGA’s core facility in Cartwright, Labrador. Diamond drill core was sawed and then sampled intervals. The drill hole core diameter utilized was NQ.

Core samples have been prepared and analyzed at the Impact Global Solutions (IGS) laboratory facility in Montreal, Quebec. Blanks, duplicates, and certified reference standards are inserted into the sample stream to monitor laboratory performance. Crush rejects, and pulps are kept and stored in a secure storage facility for future assay verification. The Company utilizes a rigorous, industry-standard QA/QC program.

About Saga Metals Corp.

Saga Metals Corp. is a North American mining company focused on the exploration and discovery of a diversified suite of critical minerals that support the North American transition to supply security. The Radar Ti-V-Fe Project comprises 24,175 hectares and entirely encloses the Dykes River intrusive complex, mapped at 160 km² on the surface near Cartwright, Labrador. Exploration to date, including 4,250 m of drilling, has confirmed a large, mineralized layered mafic intrusion hosting vanadiferous titanomagnetite (VTM) and ilmenite mineralization with strong grades of titanium and vanadium.

The Double Mer Uranium Project, also in Labrador, covers 25,600 hectares and features uranium radiometrics that highlight an 18km east-west trend, with a confirmed 14km section producing samples as high as 0.428% U3O8. Uranium uranophane was identified in several areas of highest radiometric response (2024 Double Mer Technical Report).

Additionally, SAGA owns the Legacy Lithium Property in Quebec’s Eeyou Istchee James Bay region. This project, developed in partnership with Rio Tinto, has been expanded through the acquisition of the Amirault Lithium Project. Together, these properties cover 65,849 hectares and share significant geological continuity with other major players in the area, including Rio Tinto, Winsome Resources, Azimut Exploration, and Loyal Metals.

With a portfolio spanning key commodities critical to the clean energy future, SAGA is strategically positioned to play an essential role in critical mineral security.

On Behalf of the Board of Directors

Mike Stier, Chief Executive Officer

For more information, contact:

Rob Guzman, Investor Relations
Saga Metals Corp.
Tel: +1 (844) 724-2638
Email: rob@sagametals.com
www.sagametals.com

Neither the TSX Venture Exchange nor its Regulation Service Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Disclaimer
This news release contains forward-looking statements within the meaning of applicable securities laws that are not historical facts. Forward-looking statements are often identified by terms such as ‘will’, ‘may’, ‘should’, ‘anticipates’, ‘expects’, ‘believes’, and similar expressions or the negative of these words or other comparable terminology. All statements other than statements of historical fact, included in this release are forward-looking statements that involve risks and uncertainties. In particular, this news release contains forward-looking information pertaining to the Company’s Radar Project. 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. Important factors that could cause actual results to differ materially from the Company’s expectations include, but are not limited to, changes in the state of equity and debt markets, fluctuations in commodity prices, delays in obtaining required regulatory or governmental approvals, environmental risks, limitations on insurance coverage, inherent risks and uncertainties involved in the mineral exploration and development industry, particularly given the early-stage nature of the Company’s assets, and the risks detailed in the Company’s continuous disclosure filings with securities regulations from time to time, available under its SEDAR+ profile at www.sedarplus.ca. The reader is cautioned that assumptions used in the preparation of any forward-looking information may prove to be incorrect. Events or circumstances may cause actual results to differ materially from those predicted, as a result of numerous known and unknown risks, uncertainties, and other factors, many of which are beyond the control of the Company. The reader is cautioned not to place undue reliance on any forward-looking information. Such information, although considered reasonable by management at the time of preparation, may prove to be incorrect and actual results may differ materially from those anticipated. Forward-looking statements contained in this news release are expressly qualified by this cautionary statement. The forward-looking statements contained in this news release are made as of the date of this news release and the Company will update or revise publicly any of the included forward-looking statements only as expressly required by applicable law.

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