Irka NE Assays Confirm High Grade Copper over 1.1km Strike

Irka NE Assays Confirm High Grade Copper over 1.1km Strike

Altair Minerals (ALR:AU) has announced Irka NE Assays Confirm High Grade Copper over 1.1km Strike

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High-quality and growing exploration portfolio with potential for large copper and gold deposits

ALR March 2025 Quarterly Activities Report & Appendix 5B

ALR March 2025 Quarterly Activities Report & Appendix 5B

Altair Minerals (ALR:AU) has announced ALR March 2025 Quarterly Activities Report & Appendix 5B

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Venatica Assays Confirm High-Grade Copper over 700m Strike

Venatica Assays Confirm High-Grade Copper over 700m Strike

Altair Minerals (ALR:AU) has announced Venatica Assays Confirm High-Grade Copper over 700m Strike

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Fourth Major Copper Porphyry Venatica System Discovered

Fourth Major Copper Porphyry Venatica System Discovered

Altair Minerals (ALR:AU) has announced Fourth Major Copper Porphyry Venatica System Discovered

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Altair Minerals Limited  New Central Porphyry System Identified at Venatica

Altair Minerals Limited New Central Porphyry System Identified at Venatica

Sydney, Australia (ABN Newswire) - Altair Minerals Limited (ASX:ALR) (OTCMKTS:CHKMF) is pleased to announce preliminary findings following a site visit where the Company has identified a significant outcrop of stockwork system at Central Porphyry. Outcropping quartzite, magnetite and secondary biotite veined porphyry stockwork which is part of a new separate Central Porphyry - 3km Southwest of the high-grade Irka NE Porphyry.

Key Highlights:

- Identification of new Central Porphyry | Venatica West a Porphyry Cluster

Site visit has discovered a significant outcrop of leached porphyry stockwork and ultra-potassic vein system which identifies a Central Porphyry intrusive part of a cluster system at Venatica West. Typical alteration and veining present within Bornite-Gold rich Copper Porphyry systems.

- Extremely dense veining and stockwork | Multi-stage Mineralisation

Stockwork of A-type quartz, magnetite and secondary biotite on Central Porphyry is the densest identified to date across Venatica West, suggesting significant hydrothermal activity, overlapping events, fracturing and multi-stage mineralisation at Central Porphyry, ideal for copper enrichment.

- Small portion of a much larger system | Central Porphyry Remains Open

Identification of Central Porphyry is an outstanding outcome, due to only a portion of the potassic stockwork zone outcropping, which could've easily been missed. Ultra-potassic alteration with dense stockwork as seen within this outcrop, generally tends to expand kilometres, with remaining footprint of alteration sitting under soil cover. Further fieldwork can identify full extent of this Central Porphyry.

- Potential for regional Porphyry system | SW - NE Regional Porphyry System

Preliminary fieldwork analysis on-going, with already a new Central Porphyry system being identified within virgin grounds at Venatica West, sitting ~3km Southwest of the high-grade Irka NE Porphyry and ~2km Northeast of the Irka SW Porphyry-Skarn system. Suggestive of a regional SW to NE trending porphyry cluster, filling the intersection of two district faults.

- Community Engagement Commenced | Early Community Approval

Early engagement has commenced with the local community, with multiple local members showing support for on-going exploration works. Altair's exploration team has also met with the President of the Community with very positive preliminary discussions. Altair has received initial community approval for exploration works with intention of putting forward long-term proposal of work programs, community incentive programs, project scheduling and local training.

Discovery of New Central Porphyry at Venatica West

The Central Porphyry is located on the Irka permit, situated ~3km southwest of the high-grade Irka NE Porphyry target and is a new intrusion system identified within Venatica West during initial site visit.

The upper zone of a new Central Porphyry has been identified through outcrop which consists of leached ultra-potassic stockwork of quartz, magnetite and secondary biotite dense veining, and surrounded by phyllic alteration halo and hosted within overprinted argillic alteration.

The ultra-potassic alteration suggests Altair is standing above the core of the Central Porphyry. The overprinting of strong argillic alteration has occurred from later stage hydrothermal fluids which has replaced the feldspars with clay material while maintaining the stockwork veining - suggesting a multistage mineralisation event which can significantly enrich the grades of copper sulphide and hypogene zone below. This leached stockwork from late-stage argillic alteration indicates the copper has been remobilized and disseminated into structurally favourable zones below, with potential to enhance grades within the contacts and breccia's at the core of the Central Porphyry.

The ultra-potassic zone generally sits right above the core of a Porphyry intrusion and in the case of the Central Porphyry, it is the densest set of stockwork, and veinlets discovered so far at Venatica West, with high alteration suggesting this area is the key part of hydrothermal activity and potentially the feeder to multiple other Porphyry systems.

The presence of dense secondary biotite veining on altered ultra-potassic outcrop not only indicates the presence of a new Porphyry system sitting below but also is an essential element for developing a large-scale Porphyry deposit within this particular belt.

Within other billion-tonne deposits proximal to Venatica, the presence of secondary biotite into the plays a key role in developing "scale" as its presence within porphyry stock and outwards into diorite host rock, tends to allow substitution of Fe2+ and Mg2+ with Cu2+, which can extend the copper mineral deposit footprint by a further ~500m radius in each direction from the main Porphyry core.

Key Takeaways

- Identification of new Central Porphyry akin to Bornite-Gold rich Copper Porphyries

- Ultra-potassic stockwork suggests we are standing above the core of the system

- Argillic overprint indicates a later-stage hydrothermal fluid enacted on Central Porphyry, leading to multi-phase mineralisation events.

- Leached outcrop, indicates copper has re-mobilized below into more structurally favourable zones allowing secondary enrichment in the porphyry core - which leads to higher grades.

- Presence of secondary biotite halo zone and veining in porphyry stock & diorite host is critical in developing scale within this belt for a large Cu-Au mineralisation zone beyond just the porphyry core.

- Structural alignment in SW-NE direction hosting a regional copper porphyry cluster. Irka NE Porphyry, the Central Porphyry and the SE Porphyry makes a potential corridor over more than 10km length.

This new Porphyry discovery adds on to the targets at Venatica, with 4x highly prospective undrilled targets for discovery being uncovered in this new district which is an extension of the belt which hosts multiple billion-tonne copper deposits, these targets at Venatica currently include:

- Irka NE Porphyry: Over 3.4km strike, with high-grade samples including:

- 7.0% Copper and 33g/t Silver
- 5.7% Copper and 43g/t Silver

- Irka SE Porphyry-Skarn: Large 6km2 anomalous area, with high-grade samples including:

- 4.8% Copper & 0.40g/t Gold
- 6.5% Copper & 0.52g/t Gold

- Central Porphyry: Newly discovered initial outcrop from field visit, part of a significantly larger system sitting under colluvial and soil cover. Ultra-potassic and advanced argillic alteration with significant stockwork and veining part of a separate porphyry intrusive.

- Venatica East: Over 17km of anomalous strike of copper stream sediments which are 5x background levels. Virgin grounds with potential to identify source of copper mineralisation feeding the streams and new major targets.

The identification of this Central Porphyry is significant and a result of the diligent fieldwork of the exploration team, as the outcrop is exposed over a minimal area and could've easily been missed. The degree of stockwork veining and hydrothermal activity suggests this alteration likely expands kilometres in each direction - with most of it sitting under post-mineral soil cover. Further detailed mapping and fieldwork will look to identify the true extent of this potassic alteration zone.

Venatica West is shaping up to be a regional porphyry system, hosting numerous high-quality targets for discovery. The Central Porphyry sits ~3km southwest of Irka NE and ~2km northeast of Irka SW, which indicates a structurally controlled regional porphyry trend SW - NE at Venatica West.

Community Engagement

Altair has received positive initial feedback from the community regarding its preliminary exploration activities and future plans. The community board has provided their approval and remains supportive with great relations built with local miners in the region who are eager for Altair to continue further exploration work.

Altair has also had an introduction and a very positive initial meeting with the President of the local community. Following from this, Altair representatives attended the initial community meeting and received approval to continue exploration works, with local members ready to assist. Altair continues to build upon existing supportive relationships within the community and will seek to provide a longterm formal proposal of its anticipated work programs, community incentive programs, project scheduling and local training. This proposal will be reviewed by the local community and President and will then be used to form the basis of monthly meetings with the community to build upon existing support.

Altair believes its early approach to engage the community and developing upon relationships which have been built over 10-years by the vendor of Irka will be key in fast-tracking exploration and development programs. Furthermore, this engagement is key to Altair's ESG core values and is expected to pay dividends in the future for both the Company and community. The early engagement with the community will also be critical in ensuring a smooth transition into its discovery programs.

Steps Forward at Venatica

The key anticipated steps forward aim to establish maximum value for shareholders through a scientific, systematic and diligent approach to exploration with the target of making a large-scale and globally significant discovery.

Venatica sits in the right the geological formation with all the key indicators capable of making such discovery. Altair plans to immediately initiate a comprehensive program to further evaluate the full potential of Venatica. The next key steps as part of the Venatica execution program includes:

- Evaluation of regional potential and detailed mapping

- On-going community engagement at Venatica West & Venatica East

- Rock chip and geochemical sampling program at Venatica West

Altair Chief Executive Officer, Faheem Ahmed comments:

"This is an outstanding find by our geological team within the high-grade Venatica Copper Project. This is now our third Porphyry target at Venatica West, and we are treading virgin and unexplored grounds here with potential to discover further mineralised outcrops and Porphyry's.

There is consistent dense veining across the outcrop which is exactly what you would like to see within a porphyry intrusion, suggesting significant magmatic fluid activity. More importantly, it appears the Central Porphyry has gone through multi-stage mineralisation, which not only introduces more copper into the intrusion, but also indicates copper has been leached from the outcrop and has potential to go through secondary enrichment below. These are all key indicators we are onto an exceptional exploration target, both with scale and potential to be high-grade.

We now have three key targets at Venatica West, two of them which has shown exceptional copper grades ranging 4 - 9% at surface across a large area. With the latest addition being this Central Porphyry, which has gone through significant leaching. Due to the leaching, we're looking for anomalous levels of copper at surface within the Central Porphyry, which will confirm to us this stockwork is likely to be significant mineralised at depth from remobilization of copper ions.

Furthermore, we are yet to even touch Venatica East, which hosts 17km strike of anomalous copper stream sediments. I'm incredibly excited to get boots on ground at Venatica East which is a pure greenfield opportunity and has never been systematically treaded or even sampled, and no one has ever followed up these prominent copper anomalies. We'll be the first Company to take an experienced geological team down to Venatica East, so the possibilities and upside is quite endless.

Simultaneously, we continue to progress works at Olympic Domain, our latest announcement on the project, 4 December 2024, has indicated a robust conductive ovoid, with historic drilling narrowly missing the core of the target. We are in intending to complete a follow-up TEM survey which can identify the precise depth of this ovoid, which will be critical for our drill program and targeting."

*To view tables and figures, please visit:
https://abnnewswire.net/lnk/BB53832O



About Altair Minerals Limited:  

Altair Minerals Limited (ASX:ALR) (OTCMKTS:CHKMF) is listed on the Australian Securities Exchange (ASX) with the primary focus of investing in the resource sector through direct tenement acquisition, joint ventures, farm in arrangements and new project generation. The Company has projects located in South Australia, Western Australia and Queensland with a key focus on its Olympic Domain tenements located in South Australia.



Source:
Altair Minerals Limited

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RETRANSMISSION: Group Eleven to be Featured on Radius Research for a Live Company Pitch, Deep Dive and Q&A Webinar

RETRANSMISSION: Group Eleven to be Featured on Radius Research for a Live Company Pitch, Deep Dive and Q&A Webinar

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) ("Group Eleven" or the "Company") is pleased to invite investors and other interested parties to attend the Company's upcoming interview with Radius Research.

CEO Bart Jaworski is providing an update on ZNG's Ballywire high-grade zinc-lead-silver (+/- germanium, +/- copper) discovery in the Republic of Ireland.

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Bold Ventures to Present at Metals Investor Forum in Vancouver on May 9, 2025

Bold Ventures to Present at Metals Investor Forum in Vancouver on May 9, 2025

Bold Ventures Inc. (TSXV: BOL) (the "Company" or "Bold") is pleased to announce that the Company will be presenting at Metals Investor Forum (MIF) on May 9 at The Rosewood Hotel, 801 W Georgia St, Vancouver, BC. The Company's President and COO, Bruce MacLachlan, and the Company's V.P. Exploration, Coleman Robertson, will be present during the conference.

John Kaiser, author of Kaiser Research Online, will be introducing Coleman Robertson at 4:50 p.m. Local Time, who will provide an overview and update on the Company's assets and plans for the upcoming field season. Please see the link to the May 9 Metals Investor Forum web page.

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Los Andes Copper at 121 Mining Investment London

Los Andes Copper at 121 Mining Investment London

Los Andes Copper Ltd. (TSXV: LA) (OTCQX: LSANF) ("Los Andes" or the "Company") is pleased to announce that the Company will be attending and participating in the upcoming 121 Mining Investment London event ("121") on 12-13 May 2025.

The 121 conference is London's largest dedicated mining investment event with over 100 companies and more than 400 sophisticated investors attending for two days of pre-booked 1-2-1 meetings.

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OUTCROP SILVER ANNOUNCES PARTNER FUNDED MAIDEN DRILL PROGRAM AT THE PEARL COPPER PROJECT, ARIZONA

OUTCROP SILVER ANNOUNCES PARTNER FUNDED MAIDEN DRILL PROGRAM AT THE PEARL COPPER PROJECT, ARIZONA

Outcrop Silver & Gold Corporation (TSXV:OCG, OTCQX:OCGSF, DE:MRG) ("Outcrop Silver") is pleased to announce the commencement of the maiden drill program at the Pearl Copper Project located in Arizona United States . The drilling campaign will be fully funded by Golden Mile Resources Limited (ASX: G88), whereby Golden Mile is currently earning a 51% interest through funding this A$2 million maiden drill program. Outcrop Silver retained a 1% net smelter return (NSR) royalty.

Outcrop Silver logo (CNW Group/Outcrop Silver & Gold Corporation)

Highlights

  • Outcrop Silver advances the Pearl Copper project through an earn-in agreement with Golden Mile Resources (ASX:G88). Program fully funded by Golden Mile .
  • The Pearl project is located in the prolific Laramide porphyry copper district, which is responsible for 70% of the United States of America's copper production.
  • All drilling permits secured from the Bureau of Land Management (BLM) and the Arizona State Land Department (ASLD).
  • The maiden drill program to test high-grade copper-silver-gold targets at the Odyssey and Ford prospects has commenced.

" Golden Mile's fully funded drill program moves Pearl forward at no cost to Outcrop Silver and exemplifies our strategy of unlocking value from non-core assets while we focus capital on expanding the high-grade Santa Ana silver project in Colombia ," stated Ian Harris , President & CEO of Outcrop Silver.

The Pearl Copper project is located in the Laramide porphyry copper district, one of the most prolific copper-producing regions globally, accounting for approximately 70% of U.S. copper production. The project sits immediately north of BHP's past-producing San Manuel-Kalamazoo Mine and along the trend with Capstone Copper's active Pinto Valley Mine, benefiting from exceptional infrastructure and a skilled local workforce.

Following the receipt of all required exploration permits, including the Notice of Intent (NOI) from the BLM and the Special Land Use Permit (SLUP) and Geologic Field Operation Plan (GFOP) from the ASLD, drilling has commenced. This maiden drill program consists of 14 to 16 reverse circulation (RC) holes totaling up to 1,800 metres, and will test two priority targets.

Transaction

On September 12, 2024 Golden Mile purchased an option on Pearl for A$100,000 (Australian Dollars) with Outcrop Silver retaining a 1% NSR royalty. Golden Mile has the option to earn-in to 51% by funding A$2,000,000 in exploration expenditures by September 12, 2027 . Golden Mile may also earn an additional 34% by funding an additional A$10,000,000 in exploration expenditures within 5 years. Upon completing the earn-in a joint venture will be formed with both parties funding proportionally. If either party dilutes below 10%, their interest will convert to an additional 1% NSR royalty. At such time that a JORC compliant resource achieves 750,000 tonnes of contained copper at a minimum grade of 0.3%, Golden Mile will pay Outcrop Silver A$2,000,000 .

The Pearl Copper project was acquired through the amalgamation with Zacapa Resources. Zacapa's portfolio also included the Kramer Hills brownfield oxide gold project in San Bernardino, California and the South Bullfrog, gold project in Beatty, Nevada adjacent to Anglo Gold's Silicon project.

Qualified Person

Edwin Naranjo Sierra is the designated Qualified Person within the meaning of the National Instrument 43-101 and has reviewed and verified the technical information in this news release. Mr. Naranjo holds a MSc. in Earth Sciences, and is a Fellow of the Australasian Institute of Mining and Metallurgy (FAusIMM). Mr. Naranjo Sierra is a consultant to the company and is therefore independent for the purposes of NI 43-101.

About Outcrop Silver

Outcrop Silver is a leading explorer and developer focused on advancing its flagship Santa Ana high-grade silver project in Colombia . Leveraging a disciplined and seasoned team of professionals with decades of experience in the region. Outcrop Silver is dedicated to expanding current mineral resources through strategic exploration initiatives.

At the core of our operations is a commitment to responsible mining practices and community engagement, underscoring our approach to sustainable development. Our expertise in navigating complex geological and market conditions enables us to consistently identify and capitalize on opportunities to enhance shareholder value. With a deep understanding of the Colombian mining landscape and a track record of successful exploration, Outcrop Silver is poised to transform the Santa Ana project into a significant silver producer, contributing positively to the local economy and setting new standards in the mining industry.

About Golden Mile

Golden Mile is a project development and mineral exploration company. The primary focus is on growing the Company with a multi-asset and multi-commodity strategy through advancing core projects, acquiring high-quality assets, and tactical alliances with joint venture partners.

ON BEHALF OF THE BOARD OF DIRECTORS

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

Certain information contained herein constitutes "forward-looking information" under Canadian securities legislation. Generally, forward-looking information can be identified by the use of forward-looking terminology such as "potential," "we believe," or variations of such words and phrases or statements that certain actions, events or results "will" occur. Forward-looking statements are based on the opinions and estimates of management as of the date such statements are made and they are subject to known and unknown risks, uncertainties and other factors that may cause the actual results, level of activity, performance or achievements of Outcrop Silver to be materially different from those expressed or implied by such forward-looking statements or forward-looking information, including: the receipt of all necessary regulatory approvals, capital expenditures and other costs, financing and additional capital requirements, completion of due diligence, general economic, market and business conditions, new legislation, uncertainties resulting from potential delays or changes in plans, political uncertainties, and the state of the securities markets generally. Although management of Outcrop Silver have attempted to identify important factors that could cause actual results to differ materially from those contained in forward-looking statements or forward-looking information, there may be other factors that cause results not to be as anticipated, estimated or intended. There can be no assurance that such statements will prove to be accurate, as actual results and future events could differ materially from those anticipated in such statements. Accordingly, readers should not place undue reliance on forward-looking statements and forward-looking information. Outcrop Silver will not update any forward-looking statements or forward-looking information that are incorporated by reference.

SOURCE Outcrop Silver & Gold Corporation

Cision View original content to download multimedia: http://www.newswire.ca/en/releases/archive/May2025/08/c1166.html

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Group Eleven Intersects 12.0m of 2.30% Cu and 560 g/t Ag, Including 6.4m of 3.72% Cu and 838 g/t Ag, Demonstrating High-Grade Copper and Silver Potential at Ballywire

Group Eleven Intersects 12.0m of 2.30% Cu and 560 g/t Ag, Including 6.4m of 3.72% Cu and 838 g/t Ag, Demonstrating High-Grade Copper and Silver Potential at Ballywire

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."

Cannot view this image? Visit: https://images.newsfilecorp.com/files/5685/251260_exhibit1_550.jpg

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

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/251260_exhibit1.jpg

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

Cannot view this image? Visit: https://images.newsfilecorp.com/files/5685/251260_exhibit2_550.jpg

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

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/251260_exhibit2.jpg

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

ItemFrom
(m)
To
(m)
Int
(m)
Zn
(%)
Pb
(%)
Zn+Pb
(%)
Ag
(g/t)
Cu
(%)
25-3552-31155.00155.840.848.411.7010.1193.8-
And188.89192.613.722.340.222.5611.9-
Incl.190.82191.750.934.770.455.2225.2-
And296.95344.0747.123.131.374.5021.6-
Incl.300.76301.700.945.210.725.9313.9-
And309.07334.9625.895.102.277.3735.4-
Incl.310.00322.8812.887.723.2410.9557.4-
Incl.315.49319.203.7115.814.5620.37151.1-
And347.79370.4222.630.470.510.98315.81.30
Incl.348.71368.6019.890.490.571.07356.51.46
Incl.348.71360.7312.020.590.791.38560.12.30
Incl.353.39360.737.340.681.271.95768.03.36
Incl.354.34360.736.390.651.462.11838.03.72
Incl.354.34355.200.860.770.060.831880.05.73
And355.20356.090.890.090.020.11516.01.12
And356.09357.020.930.408.478.87399.01.16
And357.02357.980.960.361.151.51128.01.19
And357.98358.780.802.440.212.651215.010.45
And358.78359.841.060.330.060.38979.03.92
And359.84360.730.890.450.030.48871.03.52

 

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.

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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

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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.

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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.

ON BEHALF OF THE BOARD OF DIRECTORS
Bart Jaworski, P.Geo.
Chief Executive Officer

E: b.jaworski@groupelevenresources.com | T: +353-85-833-2463
E: j.webb@groupelevenresources.com | T: 604-644-9514

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

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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

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

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(3) Close-Up Core Photo

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

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(4) Close-Up Core Photo

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

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(5) Close-Up Core Photo

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

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(6) Close-Up Core Photo

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

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(6a) Close-Up Core Photo

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

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(7) Close-Up Core Photo

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

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(8) Close-Up Core Photo

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

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(9) Close-Up Core Photo

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

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