Saga Metals Corp. (‘SAGA’ or the ‘Company’) (TSXV: SAGA) (OTCQB: SAGMF) (FSE: 20H) a North American exploration company specializing in the discovery of critical minerals, is pleased to announce the addition of 97 new claims covering 2,425 hectares, increasing the total area of the Radar Ti-V-Fe Project to 24,175 hectares.

The Company’s 100%-owned Radar Property is strategically located just 10 kilometres from the coastal city of Cartwright, Labrador. The location offers excellent infrastructure advantages, including:

• Road access
• Deep-water port on the Atlantic Ocean
• Cartwright Airport
• Proximity to hydroelectric power

With the recent expansion, the Radar Property now fully encompasses the Dykes River intrusive complex, a recently identified Mesoproterozoic layered mafic intrusion (Gower, 2017). The complex has garnered significant interest due to its geological resemblance to large AMCG-type intrusions and the presence of an extensive titanium-vanadium-iron (Ti-V-Fe) enriched layer containing vanadiferous titanomagnetite (‘VTM’).

Regional airborne magnetic surveys highlighted the mafic oxide layer, revealing an arcuate exploration target extending over 20 kilometers in length.

Michael Garagan, CGO & Director of SAGA commented: ‘To lay claim to the entire Dykes River Intrusion is an important milestone for SAGA and its shareholders. Throughout history, many of these mineralized geological settings have been shared amongst multiple companies vying to advance their projects. It’s a unique and significant opportunity to hold the entire 160 square km intrusion mapped at the surface and benefits from tremendous infrastructure. The claim acquisition consolidates the entire intrusion and allows the company to delegate zones for both additional infrastructure and further exploration. We’ve only just begun uncovering the true potential and extent of the oxide layering hosted within the intrusion.’

Figure 1: Map of the Radar project highlighting the oxide layering, road access, and proximity to the town of Cartwright, Labrador. SAGA’s 2024 field programs now confirm compilation of historical airborne geophysics.

Saga Metals Confirms Geological Success with Drilling:

The Company recently reported assays from the first two of seven holes drilled on the Hawkeye zone of the Radar Ti-V-Fe property. Please click here to review the full press release on drill holes #1 and #4. Highlights are listed below.

Highlights:

• Drilled 2,200m confidently testing targets down to a depth of 200 meters, covering a 500-meter by 350-meter target panel.
• Winter program analytical results have been obtained for the first two diamond drill holes.
• Petrographic analysis and the new assays confirm that the main economic mineral is a vanadiferous titanomagnetite (‘VTM’), which is prospective for simplified metallurgical processing.
• Exceptional intercepts of VTM included 31.5m @ 25.95% Fe + 5.34% TiO ₂ + 0.28% V ₂ O ₅ in HEZ-01 and 50m @ 24.49% Fe + 4.74% TiO ₂ + 0.305 % V ₂ O ₅ in HEZ-04.
• Massive high-grade VTM samples including HEZ-01 with 0.3m @ 39.5% Fe + 9.4% TiO ₂ + 0.339% V ₂ O ₅ and HEZ-01 with 0.5m @ 43.0% Fe + 9% TiO ₂ + 0.512% V ₂ O ₅ .
• Drilling intercepts average 20-40% VTM, and particular massive layers exceed 60% VTM.
• Drilling to vertical depths of 200 meters confirms magnetic anomalies identified by geophysics.
• Initial drilling covers just 1/40th of the identified 20 km strike extent of the oxide layering zone in the Dykes River intrusion.

Drilling also confirmed massive to semi-massive oxide layering, hosting VTM mineralization, with significant widths up to 210 meters within the drill core. The geological context identified by Dr. Al Miller’s petrographic studies substantially advanced the understanding of Radar Property mineralization. These findings indicate that the VTM mineralization system is advantageous for simplified metallurgical processing and potentially improves economic outcomes.

Figure 2: The prospective oxide layering zone on the Radar property extends for an inferred 20km strike length, as shown on a compilation of historical airborne geophysics, which SAGA confirmed in the 2024 field programs.

Figure 3: Hawkeye Zone displays a   500m strike by 350m width magnetic anomaly drilled in the winter 2025 program. (2024 Saga Metals. TMI Magnetic Survey).

Given the success of the maiden drill program within the Hawkeye zone over a 500 m strike and the strong correlation between drill core, rock samples and geophysics (Figure 3), SAGA plans to repeat this model over the five priority targets along the 20 km strike length of the oxide layer. The geophysical anomaly drilled in the Hawkeye zone is potentially one of the lesser anomalies. Early indications from geophysics being conducted over the Trapper zone report an even stronger magnetic response.

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 related to the Radar Ti-V-Fe Project disclosed in this news release.

About Saga Metals Corp.

Saga Metals Corp. is a North American mining company focused on the exploration and discovery of critical minerals that support the global transition to green energy. The company’s flagship asset, the Double Mer Uranium Project, is located in Labrador, Canada, covering 25,600 hectares. This project features uranium radiometrics that highlight an 18km east-west trend, with a confirmed 14km section producing samples as high as 0.428% U ₃ O ₈ and uranium uranophane was identified in several areas of highest radiometric response (2024 Double Mer Technical Report).

In addition to its uranium focus, 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 Lithium.

SAGA also holds additional exploration assets in Labrador, where the company is focused on the discovery of titanium, vanadium, and iron ore. With a portfolio that spans key minerals crucial to the green energy transition, SAGA is strategically positioned to play an essential role in the clean energy future.

On Behalf of the Board of Directors

Mike Stier, Chief Executive Officer

For more information, contact:
Saga Metals Corp.
Investor Relations
Tel: +1 (778) 930-1321
Email: info@SAGAmetals.com
www.SAGAmetals.com

The TSX Venture Exchange has not reviewed and does not accept responsibility for the accuracy or adequacy of this release. 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 Ti-V-Fe 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, risks and uncertainties involved in the mineral exploration and development industry, and the risks detailed in the Company’s final prospectus in Manitoba and amended and restated final prospectus for British Columbia, Alberta and Ontario dated August 30, 2024, filed under its SEDAR+ profile at www.sedarplus.ca, and in the continuous disclosure filings made by the Company with securities regulations from time to time. 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.

Photos accompanying this announcement are available at:
https://www.globenewswire.com/NewsRoom/AttachmentNg/e5fcaa32-0144-4ab1-8675-6311908d44c5

https://www.globenewswire.com/NewsRoom/AttachmentNg/4d825e7b-917e-4d9b-a851-f4e0bb4edee0

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Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) (‘Group Eleven’ or the ‘Company’) is pleased to announce assay results from four new holes from the ongoing drill program at the Company’s 100%-owned Ballywire zinc-lead-silver discovery (‘Ballywire’), PG West Project (‘PG West’), Republic of Ireland.

Highlights:

• 25-3552-31, a 65m step-out hole, intersected two strongly mineralized horizons:
  • Cu-Ag horizon (starting at 348.7m downhole)
    • 19.9m of 1.46% Cu and 356 g/t Ag, including
    • 12.0m of 2.30% Cu and 560 g/t Ag, including
    • 6.4m of 3.72% Cu and 838 g/t Ag
  • Zn-Pb-Ag horizon (starting at 297.0m downhole)
    • 47.1m of 4.5% Zn+Pb (3.1% Zn and 1.4% Pb) and 22 g/t Ag, including
    • 25.9m of 7.4% Zn+Pb (5.1% Zn and 2.3% Pb) and 35 g/t Ag, including
    • 12.9m of 11.0% Zn+Pb (7.7% Zn and 3.2% Pb) and 57 g/t Ag, including
    • 3.7m of 20.4% Zn+Pb (15.8% Zn and 4.6% Pb) and 151 g/t Ag
• Up to 10.45% Cu (over 0.80m) and up to 1,880 g/t Ag (over 0.86m) intersected in the Cu-Ag horizon; to the Company’s knowledge, this represents the highest-grade Ag intercept in Ireland over the last >60 years (by any operator) and similarly, one of the highest-grade Cu intercepts
• Cu-Ag horizon consists of replacement-style mineralization along the base of the Waulsortian Limestone in proximity to a fault structure; mineralization appears to consist mostly of tennantite-tetrahedrite (detailed mineralogy work to be undertaken in due course)
• Noteworthy is the presence of elevated antimony in the Cu-Ag zone, grading 0.27% Sb within the above 6.4m interval (including 0.80m of 10.45% Cu, 1215 g/t Ag and 0.83% Sb)
• This hole expands the footprint of the 2.6km long discovery trend by at least 65m down-dip, to a total of at least 170m down-dip along this section (and remains open further down-dip)
• Drilling continues at Ballywire with two rigs testing (i) the NE extension and (ii) 1.3km ENE of the Ballywire discovery in the vicinity of the prospective ‘D’ gravity-high anomaly; a third rig was added this week, testing the deeper Cu-Ag target (below the Waulsortian Limestone)

‘Intersecting spectacular copper-silver grades over significant thicknesses is a pivotal moment for the Ballywire discovery,’ stated Bart Jaworski, CEO. ‘These results not only strongly point to a stratigraphically deeper Cu-Ag horizon but also represent a proof of concept that substantial grades and thicknesses of copper and silver exist at the discovery, in addition to excellent grades of Zn-Pb. The growing presence of critical minerals at Ballywire, namely, copper, germanium and now potentially antimony, highlights the rising strategic importance of this discovery for Ireland, the EU and our shareholders. With today’s Cu-Ag milestone, continued drilling to the NE and along our prospective 6km trend, plus the start of drilling with our third rig, we are poised to further grow shareholder value as the year progresses.’

Exhibit 1. Cross-Section Showing New Drilling (25-3552-31) at Ballywire Discovery

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Note: True width of mineralized intervals in 25-3552-31, as a percent of down-hole interval, is estimated to be 50-70%

Exhibit 2. Plan Map Showing New Drilling and Intersected High-Grade Cu-Ag Mineralization

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New Step-Out Holes at Ballywire Discovery

The Ballywire prospect at the Company’s 100%-owned PG West Project in Republic of Ireland, represents the most significant mineral discovery in Ireland in over a decade. First announced in Sept-2022, the discovery has 52 holes drilled and reported by Group Eleven to date, including the most recent four holes (25-3552-30, -31, -32, and -33) reported today (see Exhibits 1 to 7).

High-grade Zn-Pb mineralization from 25-3552-31 (see Page 1 and Exhibits 1 to 4) consists predominantly of sphalerite, galena and pyrite. High-grade Cu-Ag mineralization in this hole consists of suspected tennantite/tetrahedrite, chalcopyrite, sphalerite, galena and pyrite along and/or close to the base of the Waulsortian Limestone (see Exhibit 1). Noteworthy is the presence of elevated antimony within the Cu-Ag zone. For example, the 6.39m interval below, grading 3.72% Cu and 838 g/t Ag, also grades 0.27% Sb (including 0.80m of 10.45% Cu, 1215 g/t Ag and 0.83% Sb).

Exhibit 3. Summary of Assays from 25-3552-31 at Ballywire

Note: True width of the mineralized interval in hole 25-3552-31, as a percentage of the down-hole interval, is estimated to be 50-70%; for photographs of Cu-Ag rich core, see Appendix and www.groupelevenresources.com.

Three other holes released today were drilled in a 150m gap to the NE of 25-3552-31 (25-3552-30, -32 and -33; see Exhibit 2). Hole 25-3552-30 returned nil mineralization, 25-3552-32 returned three intervals of mineralization up to 0.94m of 2.4% Zn+Pb (0.9% Zn and 1.5% Pb) and 8 g/t Ag, and 25-3552-33 returned three intervals of mineralization up to 0.82m of 2.9% Zn+Pb (1.1% Zn and 1.8% Pb) and 7 g/t Ag. These zones of mineralization are narrower and weaker than those at the main discovery trend but generally in line with recent holes drilled further to the ENE (see holes G11-3552-24, -26 and 28 in news release dated 25-Mar-2025). Disseminated copper mineralization, as well as, mineralized veins and fractures, is strengthening towards the north, suggesting massive sulphide mineralization may be present further north (see northern-most purple line in Exhibit 4). A second mineralized trend is also emerging to the south where the interpreted Cu-Ag rich ‘feeder’ fault pierced by drilling along the main discovery trend appears to correlate with mineralization approx. 350m along strike to the ENE, intersected in G11-3552-08 (see solid and dashed purple lines in Exhibit 4). Drilling is ongoing in the NE area to test the above targets.

Copper-Silver Target

Today’s results add to a growing body of evidence that support the interpretation of a Cu-Ag ‘feeder’ fault parallel to and spatially associated with the main Zn-Pb-Ag discovery at Ballywire (see Exhibit 4). With up to 10.45% Cu and 1,880 g/t Ag in a mineralized horizon near a steeply dipping structure, mineralizing fluids are interpreted to have emanated from deeper in the sedimentary sequence (see Exhibit 5). Meanwhile, the stratigraphy of the region suggests that the Lower Limestone Shale horizon exists approximately 100-200m below the discovery horizon (base of the Waulsortian Limestone). This horizon hosts four well known Cu-Ag historic occurrences in the surrounding area (see Denison, Oola, Gortdrum and Tullacondra in Exhibit 8, located approx. 5km, 9km, 10km and 45km away from Ballywire, respectively).

These historic Cu-Ag occurrences can be interpreted as the eroded remnants of originally more vertically extensive mineralizing systems, likely representing the roots of stratigraphically higher Zn-Pb-Ag mineralization. At Ballywire, the mineralizing system has the potential to be much larger than its neighbouring occurrences (based on a relatively larger footprint to date); additionally, any Cu-Ag mineralization would notionally be intact below the existing Zn-Pb-Ag mineralization.

Given the compelling nature of this exploration model, Group Eleven added a third rig and began drilling this deeper Cu-Ag target this week.

Exhibit 4. Plan Map Showing Interpreted Cu-Ag ‘Feeder’ at Ballywire

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Exhibit 5. Cross-Section Showing Hypothesized Cu-Ag Mineralization in the Lower Limestone Shale

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Exhibit 6. Oblique 3D View of Cu-Ag Mineralization at Ballywire

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Note: Bodies shown (calcite, Zn-Pb-Ag and Cu-Ag) are not constrained by any grade cut-off and are meant for illustrative purposes only

Exhibit 7. Regional Gravity at Ballywire Showing 6km Long Prospective Trend

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Notes to Exhibit 8: (a) Pallas Green MRE is owned by Glencore (see Glencore’s Resources and Reserves Report dated December 31, 2024); (b) Stonepark MRE: see the ‘NI 43-101 Independent Report on the Zinc-Lead Exploration Project at Stonepark, County Limerick, Ireland’, by Gordon, Kelly and van Lente, with an effective date of April 26, 2018, as found on SEDAR; and (c) the historic estimate at Denison was reported by Westland Exploration Limited in ‘Report on Prospecting Licence 464’ by Dermot Hughes dated May, 1988; the historic estimate at Gortdrum was reported in ‘The Geology and Genesis of the Gortdrum Cu-Ag-Hg Orebody’ by G.M. Steed dated 1986; and the historic estimate at Tullacondra was first reported by Munster Base Metals Ltd in ‘Report on Mallow Property’ by David Wilbur, dated December 1973; and later summarized in ‘Cu-Ag Mineralization at Tullacondra, Mallow, Co. Cork’ by Wilbur and Carter in 1986; the above three historic estimates have not been verified as current mineral resources; none of the key assumptions, parameters and methods used to prepare the historic estimates were reported and no resource categories were used; significant data compilation, re-drilling and data verification may be required by a Qualified Person before the historic estimates can be verified and upgraded to be compliant with current NI 43-101 standards; a Qualified Person has not done sufficient work to classify them as a current mineral resource and the Company is not treating the historic estimates as current mineral resources. ‘Rathdowney Trend’ is the south-westerly projection of the Rathdowney Trend, hosting the historic Lisheen and Galmoy mines.

Exhibit 8. Regional Map of Ballywire Discovery and Surrounding Cu-Ag Historic Occurrences

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Qualified Person

Technical information in this news release has been approved by Professor Garth Earls, Eur Geol, P.Geo, FSEG, geological consultant at IGS (International Geoscience Services) Limited, and independent ‘Qualified Person’ as defined under Canadian National Instrument 43-101.

Sampling and Analytical Procedures

All core drilled at Ballywire is NQ (47.6mm) and is cut using a rock saw. Sample intervals vary between 0.42m to 1.3m with the majority of samples in the 0.79m to 0.99m range. The half-core samples are bagged, labelled and sealed at Group Elevens core store facility in Limerick, Ireland. Selected sample bags are examined by the Qualified Person. Transport is via an accredited courier service and/or by Group Eleven staff to ALS Laboratories in Loughrea Co. Galway, Ireland. Sample preparation at the ALS facility comprises fine crushing 70%

Quality Assurance/Quality Control (QA/QC) Information

Group Eleven inserts certified reference materials (‘CRMs’ or ‘Standards’) as well as blank material, to its sample stream as part of its industry-standard QA/QC programme. The QC results have been reviewed by the Qualified Person, who is satisfied that all the results are within acceptable parameters. The Qualified Person has validated the sampling and chain of custody protocols used by Group Eleven.

About Group Eleven Resources

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) is drilling the most significant mineral discovery in the Republic of Ireland in over a decade. The Company announced the Ballywire discovery in September 2022, demonstrating high grades of zinc, lead, silver, copper, germanium and locally, antimony. Key intercepts to date include:

• 10.8m of 10.0% Zn+Pb and 109 g/t Ag (G11-468-03)
• 10.1m of 8.6% Zn+Pb and 46 g/t Ag (G11-468-06)
• 10.5m of 14.7% Zn+Pb, 399 g/t Ag and 0.31% Cu (G11-468-12)
• 11.2m of 8.9% Zn+Pb and 83 g/t Ag (G11-3552-03)
• 29.6m of 10.6% Zn+Pb, 78 g/t Ag and 0.15% Cu (G11-3552-12) and
• 11.8m of 11.6% Zn+Pb, 48 g/t Ag (G11-3552-18)
• 15.6m of 11.6% Zn+Pb, 122 g/t Ag and 0.19% Cu (G11-3552-27)
• 12.0m of 1.4% Zn+Pb, 560 g/t Ag, 2.30% Cu and 0.17% Sb (25-3552-31), including
• 6.4m of 2.1% Zn+Pb, 838 g/t Ag, 3.72% Cu and 0.27% Sb (25-3552-31)

Ballywire is located 20km from Company’s 77.64%-owned Stonepark zinc-lead deposit¹, which itself is located adjacent to Glencore’s Pallas Green zinc-lead deposit². The Company’s two largest shareholders are Glencore Canada Corp. (16.1% interest) and Michael Gentile (16.0%). Additional information about the Company is available at www.groupelevenresources.com.

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 Information

This press release contains forward-looking statements within the meaning of applicable securities legislation. Such statements include, without limitation, statements regarding the future results of operations, performance and achievements of the Company, including the timing, content, cost and results of proposed work programs, the discovery and delineation of mineral deposits/resources/ reserves and geological interpretations. Although the Company believes that such statements are reasonable, it can give no assurance that such expectations will prove to be correct. Forward-Looking statements are typically identified by words such as: believe, expect, anticipate, intend, estimate, postulate and similar expressions, or are those, which, by their nature, refer to future events. The Company cautions investors that any forward-looking statements by the Company are not guarantees of future results or performance, and that actual results may differ materially from those in forward-looking statements as a result of various factors, including, but not limited to, variations in the nature, quality and quantity of any mineral deposits that may be located. All of the Company’s public disclosure filings may be accessed via www.sedarplus.ca and readers are urged to review these materials, including the technical reports filed with respect to the Company’s mineral properties.

APPENDIX – CORE PHOTOS
COPPER-SILVER ZONE IN HOLE 25-3551-31
(With Key Assay Results and Brief Descriptions of Key Mineralogy)

Core Boxes 103-105

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Core Boxes 106-108

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Core Boxes 109-111

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(1) Close-Up Core Photo

Above: Dolomitized Waulsortian Limestone, cross-cut by sulphide bearing veins (suspected tennatite-tetrahedrite, chalcopyrite and/or pyrite)

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(2) Close-Up Core Photo

Above: Suspected tennantite/tetrahedrite (grey), chalcopyrite and pyrite (yellow) and calcite (white)

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(3) Close-Up Core Photo

Above: Chalcopyrite with some pyrite (yellow) and suspected tennantite/tetrahedrite (grey), calcite (white)

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(4) Close-Up Core Photo

Above: Semi-massive chalcopyrite and pyrite (yellow), galena (reflective grey)

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(5) Close-Up Core Photo

Above: Waulsortian Limestones (grey), calcite (white), pyrite and chalcopyrite (yellow)

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(6) Close-Up Core Photo

Above: Suspected tennantite and tetrahedrite (dark grey), chalcopyrite (yellow), calcite (white)

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(6a) Close-Up Core Photo

Above: Suspected tennantite and tetrahedrite (dark grey), chalcopyrite (yellow), calcite (white)

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(7) Close-Up Core Photo

Above: Suspect tennantite and tetrahedrite (dark grey), chalcopyrite (yellow), calcite (white)

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(8) Close-Up Core Photo

Above: Chalcopyrite (yellow), suspected tennantite/tetrahedrite (grey), calcite (white)

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(9) Close-Up Core Photo

Above: Fault zone (juxtaposing sub-Waulsortian lithologies against Waulsortian Limestone)

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¹ Stonepark MRE is 5.1 million tonnes of 11.3% Zn+Pb (8.7% Zn and 2.6% Pb), Inferred (Apr-17-2018)
² Pallas Green MRE is 45.4 million tonnes of 8.4% Zn+Pb (7.2% Zn + 1.2% Pb), Inferred (Glencore, Dec-31-2024)

To view the source version of this press release, please visit https://www.newsfilecorp.com/release/251260