Hole 23 Delivers! Power Nickel Final Drill Results from the Fall 2022 Drill Program and Initial Drill Results from Winter 2023

Hole 23 Delivers! Power Nickel Final Drill Results from the Fall 2022 Drill Program and Initial Drill Results from Winter 2023

Highlights

Main Zone

  • 0.97% Ni, 0.45% Cu, 0.07% Co, 0.80 g/t Palladium, 0.27 g/t Platinum over 16.4m in Hole PN-23-023
    Including
  • 1.08% Ni, 0.50% Cu, 0.08% Co, 0.91 g/t Palladium, 0.31 g/t Platinum over 13.5m
  • 1.37% Ni, 0.44% Cu, 0.10% Co, 1.11 g/t Palladium, 0.57 g/t Platinum over 5.6m
  • 0.57% Ni, 0.17% Cu, 0.04% Co, 0.47 g/t Palladium, 0.18g/t Platinum over 14.8m in Hole PN-23-024
    Including
  • 0.92% Ni, 0.32% Cu, 0.06% Co, 0.59 g/t Palladium, 0.34g/t Platinum over 4.85m
    And
  • 1.03% Ni, 0.17% Cu, 0.07% Co, 1.13 g/t Palladium, 0.1g/t Platinum over 2.3m in Hole PN-23-024
  • Drilling has completed for the winter season, and will resume in the summer. Holes PN-23-025 to PN-23-035 are awaiting assay results, and several have encountered significant intervals of massive sulfides.

Power Nickel Inc. (the "Company" or "Power Nickel") (TSXV:PNPN)(OTCQB:PNPNF)(Frankfurt:IVVI) continues to confirm the presence of high-grade Ni-Cu-Co-PGE mineralization in the Main Zone of its Nisk project near James Bay, Quebec. In addition, step out exploration drilling 800m east of the Main Zone shows indications of a new Ni-Cu-Co-PGE zone within the same ultramafic sequence of rocks. The Main Zone drill results for holes PN-23-23 and PN-23-24 extend mineralization up dip from previous high-grade holes into an area previously believed to be a low grade zone between two high grade lodes (Figure 1

New Discovery 800m east of Main Zone
0.22% Ni, 0.42% Cu, 0.01% Co, 0.71 g/t Palladium, 0.31 g/t Platinum over 4.9m Hole PN-22-020

Late in the fall 2022 drill program, two holes (PN-22-020 and PN-22-021) tested an exploration target at shallow depths approximately 800m and 600m respectively east of the high-grade Main Zone (Figure 1). Hole PN-22-021 did not intersect sulphide mineralization, but further to the east hole PN-22-020 intersected three (3) zones of sulphides with significant Ni-Cu-Co-PGE mineralization (Table 1). This hole contained low amounts of sulphides but with a high ratio of Ni-Cu-Co-PGE mineralization. The area will require further testing for potential massive sulphide zones, and both holes are good candidates for downhole EM surveying to look for off-hole EM conductors.

In a March 1 news release, hole PN-22-018 was listed as NSR (no significant results), but further analysis of initial assay results from this hole revealed a low-grade Ni/PGE zone over 7.5m and it is reported here (Table 1).

Table 1 below presents the significant results received from the remaining fall 2022 program and the initial holes from the winter 2023 program.

Table 1: Significant results from the 2022 drilling program.

Hole ID

UTM E1

UTM N1

Length (m)

Azimuth (°)

Dip (°)

From (m)

To (m)

Interval Length2 (m)

Au (g/t)

Ni (%)

Cu (%)

Co (%)

Pd (g/t)

Pt (g/t)

PN-22-015

460176

5728829

544.4

157.3

-76

NSR - hole was lost in ultramafic host rocks

PN-22-016

460313

5728831

321

152.9

-58

Hole lost 1m of core in mineralized zone

PN-22-018

459537

5728552

465

180.4

-70

427.00

434.50

7.50

0.01

0.29

0.01

0.02

0.37

0.09

PN-22-019

459802

5728686

262.74

152.2

-66

Hole lost short of target

PN-22-020

460917

5728876

219.07

161.1

-61

85.00

86.50

1.50

0.01

0.81

0.09

0.04

1.00

0.03

And

100.00

102.25

2.25

0.13

0.13

0.35

0.01

0.74

0.30

And

112.60

117.50

4.90

0.05

0.22

0.42

0.01

0.71

0.31

PN-22-021

460722

5728815

178.24

162

-61

NSR

PN-23-022

460238

5728735

315

164.9

-66

208.46

208.96

0.50

3.75

0.33

0.04

2.95

0.04

0.03

Including

238.95

241.15

2.20

0.01

0.40

0.20

0.03

0.55

0.21

PN-23-023

459658

5728641

423.02

158.1

-67

358.65

375.05

16.40

0.02

0.97

0.45

0.07

0.80

0.27

Including

360.65

374.15

13.50

0.03

1.08

0.50

0.08

0.91

0.31

Including

360.65

366.25

5.60

0.03

1.37

0.44

0.10

1.11

0.57

PN-23-024

459746

5728651

433.03

162.9

-70

315.00

316.00

1.00

0.26

0.15

0.33

0.02

1.03

0.29

And

345.00

359.80

14.80

0.01

0.57

0.17

0.04

0.47

0.18

Including

345.00

349.85

4.85

0.02

0.92

0.32

0.06

0.59

0.34

And Including

357.50

359.80

2.30

0.01

1.03

0.17

0.07

1.13

0.01

  1. UTM NAD83, Zone 18N.
  2. True widths are estimated to be 70% of the Interval Length.

Fourteen (14) holes totaling 5370.67 metres were completed in the fall of 2022 for the second phase of drilling at Nisk. At the time of writing, an additional fifteen (15) holes totalling 5210 m have been completed in the winter 2023 drill program.

Power Nickel Inc., Wednesday, April 26, 2023, Press release picture

Figure 1 - Longitudinal view of the Nisk Main presenting the currently available assay results.

Power Nickel Inc., Wednesday, April 26, 2023, Press release picture

Figure 2 - Cross section view presenting current assay results in hole PN-23-023

"We are very pleased with the ongoing success of our exploration drilling at Nisk. Hole PN-23-023 assays were as pretty as its PICTURE (Figures 2 & 3). It was another excellent intersection. The team has done an amazing job piecing together the underground mystery of this deposit and we believe we have learned some invaluable clues both with our East and West exploration away from the main zone on where our next Pod like Nisk main may lie," commented Power Nickel CEO Terry Lynch

Power Nickel Inc., Wednesday, April 26, 2023, Press release picture

Figure 3 - Picture of massive sulphides in drill core from hole PN-23-023

In order to help our investors and interesting parties review the work being done, we have created some images to help with the visualization of our project (Figures 4 & 5). Below is a side view of how Power Nickel conceptualize the River of Nickel flowing within the green outline below to the surface and back down to a depth of about 400 metres over almost a kilometre.

Power Nickel Inc., Wednesday, April 26, 2023, Press release picture

Figure 4 - Conceptual ‘River of Nickel' at Nisk outlined in long section.

Looking at the top view, we can see both the flow of the river of nickel and the width of mineralization we have discovered.

Power Nickel Inc., Wednesday, April 26, 2023, Press release picture

Figure 5 - Conceptual ‘River of Nickel' in plan view at Nisk Main Zone.

Promotion & Communication Expense

Recent changes in guidance on IR and Communication spending require BC Reporting issuers to comment on their program spending in this respect. We have committed to the following programs.

Winning Media - $60,000 USD for digital marketing services in compliance with the Policies and guidelines of the TSX Venture Exchange and other applicable legislation, Virtus Media Group -$50,000 USD for digital marketing services in compliance with the policies and guidelines of the TSX Venture Exchange and other applicable legislation from now until the end of June. Machai Capital Inc - $100,000 CAD for digital marketing services in compliance with the policies and guidelines of the TSX Venture Exchange and other applicable legislation.

About the Nisk Project

The Nisk Project is located in the southern portion of the Eeyo Istchee James Bay territory, Québec, the site of a number of mining projects improving infrastructure (Figure 6).

Power Nickel completed the acquisition of its option to acquire up to 80% of the Nisk Project from Critical Elements Lithium Corp. (CRE:TSXV). The Nisk Project comprises a large land position (20 kilometres of strike length) with numerous high-grade Nickel intercepts.

Power Nickel Inc., Wednesday, April 26, 2023, Press release picture

Figure 6 - Location of the Nisk Project with respect the current infrastructure available in the area.

QAQC and SAMPLING

GeoVector Management Inc is the Consulting Company retained to oversee the drilling program, which includes core logging and sampling of the drill core.

All samples were submitted to and analyzed at ALS Global ("ALS"), an independent commercial laboratory located in Val-d'Or, Québec for both the sample preparation and assaying. ALS is a commercial laboratory independent of Power Nickel with no interest in the Nisk Project. ALS is an ISO 9001 and 17025 certified and accredited laboratory. Samples submitted through ALS are run through standard preparation methods and analysed using ME-ICP61a (33 element Suite; 0.4g sample; Intermediate Level Four Acid Digestion) and PGM-ICP27 (Pt, Pd, and Au; 30g fire assay and ICP-AES Finish) methods. ALS also undertake their own internal coarse and pulp duplicate analysis to ensure proper sample preparation and equipment calibration.

GeoVector's QAQC program includes regular insertion of CRM standards, duplicates, and blanks into the sample stream with a stringent review of all results.

The results presented in the current Press Release are complete. QAQC and data validation was performed on these holes and no material errors were observed.

Qualified Person

Eric Hébert, Géo, Ph.D. from GeoVector Management Inc and consultant to Power Nickel, is the independent qualified person who has reviewed and approved the technical disclosure contained in this news release.

About Power Nickel Inc.

Power Nickel is a Canadian junior exploration company focusing on high-potential copper, gold and battery metal prospects in Canada and Chile.

On February 1, 2021 Power Nickel (then called Chilean Metals) completed the acquisition of its option to acquire up to 80% of the Nisk project from Critical Elements Lithium Corp. (CRE:TSXV)

The NISK property comprises a large land position (20 kilometres of strike length) with numerous high-grade intercepts. Power Nickel is focused on expanding the historical high-grade nickel-copper PGE mineralization with a series of drill programs designed to test the initial Nisk discovery zone and to explore the land package for adjacent potential Nickel deposits.1

Power Nickel announced on June 8th, 2021 that an agreement has been made to complete the 100% acquisition of its Golden Ivan project in the heart of the Golden Triangle. The Golden Triangle has reported mineral resources (past production and current resources) in total of 130 million ounces of gold, 800 million ounces of silver and 40 billion pounds of copper (Resource World). This property hosts two known mineral showings (gold ore and magee), and a portion of the past-producing Silverado mine, which was reportedly exploited between 1921 and 1939. These mineral showings are described to be Polymetallic veins that contain quantities of silver, lead, zinc, plus/minus gold, and plus/minus copper.

Power Nickel is also 100-per-cent owner of five properties comprising over 50,000 acres strategically located in the prolific iron-oxide-copper-gold belt of northern Chile. It also owns a 3-per-cent NSR royalty interest on any future production from the Copaquire copper-molybdenum deposit, that was sold to a subsidiary of Teck Resources Inc. Under the terms of the sale agreement, Teck has the right to acquire one-third of the 3-per-cent NSR for $3-million at any time. The Copaquire property borders Teck's producing Quebrada Blanca copper mine in Chile's first region.

For further information on Power Nickel Inc., please contact:

Mr. Terry Lynch, CEO
647-448-8044

terry@powernickel.com

For further information, readers are encouraged to contact:

Power Nickel Inc.
The Canadian Venture Building
82 Richmond St East, Suite 202
Toronto, ON

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.

Cautionary Note Regarding Forward-Looking Statements

This news release contains certain statements that may be deemed "forward-looking statements" with respect to the Company within the meaning of applicable securities laws. 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", "indicates", "opportunity", "possible" and similar expressions, or that events or conditions "will", "would", "may", "could" or "should" occur. 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, the Company's ability to raise sufficient capital to fund its planned activities at the NISK Property and for general working capital purposes; the timing and costs of future activities on the Company's properties; maintaining its mineral tenures and concessions in good standing; changes in economic conditions or financial markets; the inherent hazards associates with mineral exploration and mining operations; future prices of metals; changes in general economic conditions; accuracy of mineral resource and reserve estimates; the potential for new discoveries; the ability of the Company to obtain the necessary permits and consents required to explore, drill and develop the projects and if obtained, to obtain such permits and consents in a timely fashion relative to the Company's plans and business objectives for the projects; the general ability of the Company to monetize its mineral resources; and changes in environmental and other laws or regulations that could have an impact on the Company's operations, compliance with environmental laws and regulations, dependence on key management personnel and general competition in the mining industry. Forward-looking statements are based on the reasonable beliefs, estimates and opinions of the Company's management on the date the statements are made. Except as required by law, the Company undertakes no obligation to update these forward-looking statements in the event that management's beliefs, estimates or opinions, or other factors, should change.

1The resource estimates at Nisk are historical in nature and the Company's geology team has not completed sufficient work to confirm an NI 43-101 mineral resource. Mineral resource information is derived from the technical report titled "Resource Estimate for the NISK-1 Deposit, Lac Levac Property, Nemiscau, Québec" dated December 2009. The key assumptions, parameters, and methods used to prepare the mineral resource estimates are set out in the technical report. This report, prepared by RSW Inc in 2009, can be found on the SEDAR website.

SOURCE:Power Nickel Inc.



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

Highlights

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  • All drilling permits secured from the Bureau of Land Management (BLM) and the Arizona State Land Department (ASLD).
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" 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.

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Transaction

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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

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Highlights:

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    • 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."

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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%

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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

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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A total of 248,138,835 common shares were represented at the meeting, being 68.52% of the Company's issued and outstanding common shares as at the record date. Shareholders voted in favour of all matters brought before the Meeting, including setting the number of directors at nine, the election of management's nominees as directors, the appointment of auditors for the ensuing year, and the acceptance of the Company's approach to executive compensation, known as "say-on-pay".

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