Pan Global Reports Multiple High-Grade Polymetallic Drill Intercepts at the Aguilas Project, Spain

Pan Global Reports Multiple High-Grade Polymetallic Drill Intercepts at the Aguilas Project, Spain

7.3% LEAD+ZINC AND 9.1 G/T SILVER OVER 5.25 METERS
37.6% LEAD+ZINC AND 6.8 G/T SILVER OVER 0.55 METERS

Pan Global Resources Inc. (TSXV: PGZ) (OTC Pink: PGNRF) ("Pan Global" or the "Company") is pleased to report results for ten new drill holes on the 25-kilometer long Zumajo faultbreccia zone and historical mine trend at the Company's 100%-owned Aguilas Project in the Cordoba Province, southern Spain.

Tim Moody, Pan Global President and CEO, commented: "The resumption of drilling on the Aguilas Project, approximately 200 kilometers north of our Escacena Project, included testing three targets on the 25-kilometer long Zumajo historic Pb-Ag mine trend. Encouraging drill results were received from the ten hole program, with significant polymetallic (lead, zinc and silver) assays returned from our first ever drill holes at the Minguillo Target and follow-up drill holes at the Vacadillas target. The mineralization remains open at depth and along strike at both targets."

Further commenting, "The vertical extent of this type of mineralization can be several hundred meters as is characteristic of the important historic Linares and La Carolina Pb-Ag vein mining districts less than 100km to the east. The drilling is currently wide-spaced and tested the mineralization to shallow depths of less than 150m on small parts of the Zumajo vein/breccia system. Additional drilling is required to further evaluate this potentially important mineral trend. Together with the announcement of multiple drill targets at Escacena last week, these results further support the compelling prospectivity of the Pan Global exploration portfolio."

Highlights:

  • 22MID01: 6.0m at 0.7% Pb, 4.6% Zn, 3.5g/t Ag from 102.0m, including
    • 2.2m at 1.9% Pb, 12.3%Zn, 9.2g/t Ag from 104.9m
  • 22MID02: 5.25m at 2.4% Pb, 4.9% Zn, 9.1g/t Ag from 156.5m, including
    • 0.55m at 20.8% Pb, 16.8% Zn, 66.4g/t Ag from 157.55m and
    • 0.6m at 0.94% Pb, 10.4% Zn, 6.8g/t Ag and from 160.10m
  • 22VAD01: 7.5m at 2.35% Pb, 0.74% Zn, 13.6 g/t Ag from 113.5m, including
    • 4.5m at 3.9% Pb, 1.1% Zn, 22.4g/t Ag from 112.5m
    • 1.5m at 10.9% Pb, 0.2 % Zn, 56.9 g/t Ag from 113.5m
  • 22VAD04: 3.75m at 4.9% Pb, 0.2% Zn, 36.1g/t Ag from 98.65m, including
    • 0.55m at 32.7% Pb, 0.13% Zn, 233g/t Ag from 98.65m

Drill Results

The Aguilas Project mineral rights, drill hole and target locations are provided in Figure 1 below. Assay results are summarized in Table 1 below and drill collar information is provided in Table 2.

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Figure 1 - Aguilas Project shaded terrain map showing soil geochemistry anomalies, drill hole and priority target locations (2022 drill areas - yellow highlight)

To view an enhanced version of Figure 1, please visit:
https://images.newsfilecorp.com/files/5190/139674_ff14022104f778ce_001full.jpg

Table 1 - Aguilas Project new drill results summary

HoleFromToIntervalCuPbZnAgAu



m%%%g/tg/t
22MID0110210860.010.684.623.50.003

104.9107.12.20.041.8512.259.20.006
 








22MID02156.5161.755.250.022.44.939.10.005
inc.157.55161.754.23.06.1011.30.006
inc.157.55158.10.550.0320.816.7566.40.001
inc.160.1160.70.60.040.9410.406.80.003
 








22VAD0189.790.715.5119.40.002

112.51207.52.350.7413.60.002
inc.113.51184.50.013.881.1122.40.004
inc.113.51151.510.880.1756.90.007
inc.113.5113.80.333.70.101590.02
inc.116117.251.250.010.662.719.80.003
 








22VAD0284.586.11.60.011.080.025.70.001









22VAD03No significant results
 








22VAD0498.65102.43.750.014.940.2036.10.004
inc.98.6599.20.550.0132.70.132330.022









22VAD0546.9492.10.580.013.20.001

80.281.751.550.060.360.383.10.002

101104.853.850.010.375.00.002









22NAD01
22NAD02No significant results
22NAD03







 

Table 2 - Aguilas Project drill hole collar information (Total 1530.5m) - Coordinates in ERTS89, UTM Zone 30N

Hole_IDEastingNorthingAzimuth (º)Dip (º)End Depth (m)
22VAD013753104240309220-65157.1
22VAD023754224240197220-60145.95
22VAD033751364240388215-60151.05
22VAD043744614240844210-65166.05
22VAD053742024240977210-65171
22MID013667794246071200-60127.5
22MID023663964246177204-67175.25
22NAD013795774236771220-55152.1
22NAD023796684236697220-70146.65
22NAD033797104236661220-70137.85

 

Minguillo Target

Drill holes 22MID01 and 22MID02 are the first holes at the Minguillo Target. The holes are approximately 400m apart and confirmed significant high grade polymetallic (Pb, Zn and Ag) mineralization extending beneath the Mina Pasqualin and Mina Chinche historic underground mine workings (see figures 2 and 3 below). The mineralization includes coarse sphalerite and galena over intervals of approximately 5m to 6m within a steep north-dipping quartz-carbonate vein and breccia zone up to 11m thick. The mineralization remains wide open at depth and along strike, associated with a Pb-Zn soil geochemistry anomaly that extends from the mine workings for approximately 3 kilometers along the Zumajo Fault Trend.

Hole 22MID01 tested approximately 30m below the lowest underground mine level at Pasqualin and intersected 6.0m at 0.7% Pb, 4.6% Zn, 3.5g/t Ag from 102.0m downhole, including 2.2m at 1.9% Pb, 12.3% Zn, 9.2g/t Ag.

Hole 22MID02 tested approximately 30m beneath the lowest underground mine level at Chinches and intersected 5.25m at 2.4% Pb, 4.9% Zn, 9.1g/t Ag from 156.5m, including 0.55m at 20.8% Pb, 16.8% Zn, 66.4g/t Ag and 0.6m at 0.94% Pb, 10.4% Zn, 6.8g/t Ag.

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Figure 2 - Minguillos Target: plan view (top) and long section (bottom) showing the locations of the Mina Pascualin and Mina Chinche historic mine workings, drill holes and Pb-Zn soil geochemistry anomaly

To view an enhanced version of Figure 2, please visit:
https://images.newsfilecorp.com/files/5190/139674_ff14022104f778ce_002full.jpg

 

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Figure 3 - Minguillo Target geology cross-section with drill hole 22MID01 and historical Mina Pascualin underground mine workings

To view an enhanced version of Figure 3, please visit:
https://images.newsfilecorp.com/files/5190/139674_ff14022104f778ce_003full.jpg

Vacadilla Target

The Vacadilla Target coincides with a semi-continuous zone of lead and zinc mineralization over more than 2 kilometers strike associated with abundant historic surface and shallow underground mine workings, including Mina San Juan and Mina San Rafael (see figures 4 and 5 below). New drill holes 22VAD01 to 22VAD05 were designed to follow-up previous wide spaced drilling by Pan Global in 2019 (see Pan Global press release - May 14, 2019). Holes 22VAD01 and 22VAD04 intersected significant high grade Pb-Zn-Ag mineralization with coarse galena and lesser sphalerite over intervals of approximately 4m to 7.5m. The results indicate mineralization potentially continues over more than 500m strike associated with the San Rafael mine workings and remains open below approximately 150m depth and is also wide open at depth in the east at the Dos Centimos zone. Additional potential is apparent, associated with a strong Pb-Zn soil anomaly over 2km strike extending from the mine workings and in potential parallel veins/breccias.

Hole 22VAD01 intersected 7.5m at 2.35% Pb and 13.6 g/t Ag from 112.5m including 4.5m at 3.9% Pb, 1.1% Zn and 22.4g/t Ag and 1m at 5.51% Pb and 19.4g/t Ag from 89.7m in the hanging wall. The results extend the mineralization approximately 45m below previous drill hole VAC06 and confirms additional mineralization within a narrow parallel fault or splay to the main structure.

Hole 22VAD04, drilled in the west of the San Rafael underground mine workings, intersected a 7m interval with breccia and veining, including 3.75m at 4.9% Pb, 36.1 g/t Ag and 0.2 % Zn from 98.65m and exceptionally high grades up to 32.7% Pb and 233 g/t Ag over 0.55m.

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Figure 4 - La Vacadilla Target plan view (above) and long section (below) showing the locations of the historic San Juan, San Rafael and Dos Centimos underground mine workings, drill holes and Pb-Zn soil geochemistry anomaly

To view an enhanced version of Figure 4, please visit:
https://images.newsfilecorp.com/files/5190/139674_ff14022104f778ce_004full.jpg

 

Cannot view this image? Visit: https://images.newsfilecorp.com/files/5190/139674_ff14022104f778ce_005.jpg

Figure 5 - Vacadilla Target geology cross-section with new drill hole 22VAD01 and previous drill hole VAC006 at Dos Centimos showing grade increasing at depth

To view an enhanced version of Figure 5, please visit:
https://images.newsfilecorp.com/files/5190/139674_ff14022104f778ce_005full.jpg

Navalaencina Target

New drill holes 22NAD01 to 22NAD03 are the first holes at the Navalaencina Target in the far southeast of the Zumajo structure, approximately 5km southeast of the Vacadilla Target. The holes tested a lead-zinc-(copper) soil anomaly and trend of historic surface and shallow San Antonio underground mine workings. Mine dump material includes samples with coarse galena, chalcopyrite and bornite. All three holes intersected broad zones of alteration and brecciation over intervals of approximately 20m within the granitic host rocks with anomalous levels of Cu and Pb over narrow intervals in holes 22NAD01 and 22NAD03.

Quality Control/Quality Assurance

All drill holes were diamond drill core size HQ (63mm) and all samples were ½ core. Nominal sample size was 1m core length and ranged from 0.4 to 2m. Sample intervals were defined using geological contacts with the start and end of each sample physically marked on the core. Diamond blade core cutting and sampling was supervised at all times by Pan Global employees. Duplicate samples of ¼ core were taken approximately every 30 samples and Certified Reference materials inserted every 25 samples in each batch.

Samples were delivered to ALS laboratory in Seville, Spain and assayed at the ALS laboratory in Ireland. All samples were crushed and split (method CRU-31, SPL22Y), and pulverized using (method PUL-31). Gold analysis was by 50gm Fire assay with ICP finish (method Au-ICP22) and multi element analysis was undertaken using a 4-acid digest with ICP AES finish (method ME-ICP61). Over grade base metal results were assayed using a 4-acid digest ICP AES (method OG-62) and AAS (method Pb-AAOre for samples >20% Pb).

Soil geochemistry anomalies in the Vacadilla Target area are defined using 4 acid ICP multielement analyses and selected samples using 30gm fire assay for Au. At the Minguillos and Navalaencina Targets, soil samples were analyzed by portable XRF.

About the Aguilas Project

The Aguilas Project is located in the Cordoba Province, approximately 200 km northeast of Pan Global's Escacena Project, in Andalucia, Spain. The Project includes nine "Investigation Permits" totalling a16,259 hectares and is owned 100% by Pan Global. The Project includes two major fault zones, including the northwest trending Zumajo structure and northeast trending Torrubia structure, both entirely within and cross-cutting the Carboniferous age Pedroches Batholith. The Zumajo structure extends approximately 25 kilometers with continuous trend of hydrothermal quartz-carbonate veins and breccias up to approximately 20m width with polymetallic (Pb-Zn-Ag-Cu) mineralization and numerous historical surface mine workings and shafts. The Torrubia structure extends for approximately 15 km and is characterised by quartz-carbonate breccia to widths of more than 50 meters, with strong red hematite alteration, numerous ancient/historic copper mine workings and high-level iron oxide copper gold (IOCG)-style mineralization. Mining for Cu and Pb-Ag ceased in the area the early 1900's and has no history of zinc mining. Pan Global is undertaking the first modern exploration and drilling in the majority of the area. Numerous parallel fault trends have also been identified throughout the project area and remain prospective for base and precious metal mineralization.

About Pan Global Resources

Pan Global Resources Inc. is actively engaged in base and precious metal exploration in southern Spain and is pursuing opportunities from exploration through to mine development. The Company is committed to operating safely and with respect to the communities and environment where we operate.

Qualified Persons

James Royall, VP Exploration for Pan Global Resources and a qualified person as defined by National Instrument 43-101, has reviewed the scientific and technical information for this news release. Mr. Royall is not independent of the Company.

On behalf of the Board of Directors
www.panglobalresources.com
.

FOR FURTHER INFORMATION PLEASE CONTACT:
tmoody@panglobalresources.com

+44 7766 253145

Statements which are not purely historical are forward-looking statements, including any statements regarding beliefs, plans, expectations or intentions regarding the future. It is important to note that actual outcomes and the Company's actual results could differ materially from those in such forward-looking statements. The Company believes that the expectations reflected in the forward-looking information included in this news release are reasonable but no assurance can be given that these expectations will prove to be correct and such forward-looking information should not be unduly relied upon. Risks and uncertainties include, but are not limited to, economic, competitive, governmental, environmental and technological factors that may affect the Company's operations, markets, products and prices. Readers should refer to the risk disclosures outlined in the Company's Management Discussion and Analysis of its audited financial statements filed with the British Columbia Securities Commission.

The forward-looking information contained in this news release is based on information available to the Company as of the date of this news release. Except as required under applicable securities legislation, the Company does not intend, and does not assume any obligation, to update this forward-looking information.

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.

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

Highlights

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  • 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).
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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.

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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 .

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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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  • 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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