Grid Battery Metals Exploration Team Completes Phase 1 of its 2024 Exploration Plan on the Clayton Valley Lithium Project

Grid Battery Metals Exploration Team Completes Phase 1 of its 2024 Exploration Plan on the Clayton Valley Lithium Project

(TheNewswire)

Grid Battery Metals Inc..

Coquitlam, BC TheNewswire - May 30, 2024 - Grid Battery Metals Inc. (the "Company" or "Grid") (TSXV: CELL, OTCQB: EVKRF FRA: NMK2) announces that it has completed the first phase of its springsummer exploration program at its Clayton Valley Lithium Property near Silver Peak, Nevada, which includes a detailed infill soil sampling program and a previously announced MT geophysical survey.

At the Clayton Valley Lithium Project, the Company contracted the services of Rangefront Geological ("Rangefront") to perform both a detailed infill soil sampling of the southern section of the claim block and to oversee a Magnetotelluric (" MT") geophysical survey to obtain information about subsurface resistivity and geology performed by KLM Geoscience LLC ("KLM") over the entire property.  The infill soil sampling exploration work has now been completed and samples have been transported to the assay lab pending results. Together these geological techniques should help predict geological structure and possible locations for lithium accumulation.  This is part of a methodical and systematic approach to high quality mineral exploration for this highly sought after metal in Nevada and will assist the Company in determining next steps for the overall exploration plan, including but not limited to a subsequent drilling program.

Recent Infill Soil Samples Taken (Clayton Valley Lithium Project)

The MT geophysical survey was performed by the KLM and was overseen by Grid's Qualified Professional, Mr. Steven McMillin P.G.

MT survey profiles


Click Image To View Full Size

Mr. Steven McMillin P.G. comments "The MT survey was completed over eleven profiles. The results were plotted in horizontal slices at 250m, 500m and 750m with bedrock depths that range from 216 to 406 m within the Grid claims as announced on May 2, 2024 .   A major northeast fault interpreted from gravity bisects the claim block and is best apparent in the 500m slice even though the slice is below the basin floor. This suggests that the fault may be a fluid conduit at depth. The fault is less apparent in the strong near-surface anomaly in the 250m slice that may reflect a spread of fluids within the basin sediments away from the fault. The 750m depth slice is likely below the basin floor and conductivity is mostly focused near the basin bounding faults".

Tim Fernback, Grid President & CEO comments "Now that the infill detailed soil sampling and MT geophysical survey programs are complete at Clayton Valley, we will gather as a group to interpret the geological data and assay lab results to plan our next steps at Clayton Valley.  This next step will likely include a 3D Leapfrog model of the subsurface to identify additional drilling targets, and a subsequent drilling program later in the year to test the depth of the lithium bearing claystone.  We are very excited about the results to date on the property."

Prior Exploration Programs

This current work associated with the first phase of the 2024 exploration plan compliments prior exploration work on the Clayton Valley Lithium Project which includes a soil sampling program over the entire property and an initial prior drilling program consisting of three reverse circulation holes totaling 356 meters (1155 feet).  The holes were intended to test the presence of lithium bearing clay members of the lakebed sediments.  Drillhole RCV-01, drilled to a depth of 130m (425 feet), was designed to twin a geothermal gradient hole drilled by a previous explorer.  Results of this hole correlated with the log of the previous hole including intervals of volcanic ash and dark green clay. Hole RCV-02, located approximately 1260 meters north of RCV-01 was drilled to a depth of 135.6m (445 ft) and penetrated a section consisting primarily of rhyolitic volcanic ash and interbedded sediments.  It penetrated a 4.5-meter section of dark green clay before entering the metamorphic alluvium.  Poor drilling conditions and high-water flows ended the hole before reaching the target depth but after successfully evaluating the lake sediment section. Hole RCV-03, located 3,890m (12,762 ft) north from Hole RCV-01, was designed to look for a perched section of volcanoclastic sediments beneath an alluvial fan.  Previous water well logs indicated a layer of clay, ash, and silt beneath the alluvium and above the bedrock. Apparently, this hole was located too close to the pediment and encountered metamorphosed dolomite at a depth of 56 meters (185 feet) and about the projected elevation of the sedimentary section.  The hole lost circulation in an apparent karst horizon at 68.5 meters (225 feet) and was terminated at 79.2 meters (260 ft) without regaining sample return.

Grid's Clayton Valley Lithium Project (RC Drilling Locations Identified)


Click Image To View Full Size

Tim Fernback, Grid President & CEO comments "Clayton Valley Nevada is home to North America's only lithium brine producer (Albemarle Corporation's Silver Peak Mine) and our property is immediately to the west of their lithium property and production facility.  Recently, Century Lithium (our neighbor to the east of the Silver Peak Mine) has just released their Positive Feasibility Study by T. Lane et al. (2024). Measured and Indicated resources totaling 1,207.33 million tonnes (Mt) at an average grade of 957 parts per million (ppm) lithium (Li) containing 1.155 Mt of Li or 6.148 Mt of lithium carbonate equivalent (LCE), a 40-year mine life and an after-tax NPV 8 of $3.01 billion. Additional information is in Century Lithium's NI-43-101 by Fayram et al. (2020) 43-101 Report .

With the MT survey that has just been completed, together with the results of the planned detailed soil sampling program in the southern area of our Clayton Valley claim block, these results will allow us to determine next steps for our exploration programs later in the year."

It should be noted that results from any adjacent property(s) are not an indication of what may be found on the Company's property(s).

About Rangefront Geological

Elko Nevada-based Rangefront Geological has combined in-depth expertise with cutting-edge technology to provide mining consulting services, contract labor, field crew services, and vehicular support to the mining industry.  With services available across North America, Rangefront works closely with its clients to provide high-quality mineral exploration services.

About KLM Geoscience LLC

KLM ( https://www.klmgeoscience.com/ ) is an industry leading, Nevada-based geophysical exploration company.  Established in 2014, KLM specializes in a wide array of geophysical   methods.  Using state of the art equipment, KLM's services include induced polarization (IP), natural-source magnetotellurics (MT, AMT), controlled-source audio-frequency magnetotellurics (CSAMT), passive seismic and magnetic potential field surveys.  With a head office location in Nevada, this allows KLM to rapidly mobilize and begin work at a moment's notice throughout the Western United States and beyond.  KLM has been a preferred vendor for Grid and its management team for many years.

Qualified Person

Mr. Steven McMillin, P.G. is a Qualified Person as defined by National Instrument 43-101 and has approved the technical information contained within this news release.

About Grid Battery Metals Inc.

Grid Battery Metals Inc. is a Canadian based exploration company whose primary listing is on the TSX Venture Exchange.  The Company's maintains a focus on exploration for high value battery metals required for the electric vehicle (EV) market.

  www.gridbatterymetals.com .

About Texas Springs Property

The Company owns a 100% interest in the Texas Spring Property which consists of mineral lode claims located in Elko County, Nevada. The Property is in the Granite Range southeast of Jackpot, Nevada, about 73 km north-northeast of Wells, Nevada. The target is a lithium clay deposit in volcanic tuff and tuffaceous sediments of the Humbolt Formation. A Phase 1 exploration program at the Texas Springs Property (Fall 2023) yielded average lithium grades of 2010 ppm, applying a 1,000 ppm cut-off, and up to  5,610 ppm Lithium .

The Texas Spring property adjoins the southern border of the Nevada North Lithium Project - owned by Surge Battery Metals Inc. ("Surge") (TSXV: NILI, OTC: NILIF) and comprised of 725 mineral claims.  Surge's first round of drilling identified strongly mineralized lithium bearing clays. The average lithium content within all near surface clay zones intersected in the 2022 drilling program, applying a 1000 ppm cut-off, was 3254 ppm. (Press release March 29, 2023 ).  More recent results have shown higher grade lithium up to 8070 ppm on this property after initial drilling (Press release September 12, 2023 ). Our exploration results are on-trend with these results.

About Clayton Valley Lithium Project

The Company owns a 100% interest in 113 lithium lode and placer claims covering over 640 hectares in Clayton Valley. Clayton Valley is a down-dropped closed basin formed by the Miocene age Great Basin extension and is still active due to movement along the Walker Lane structural zone.  As a result, the basin has preserved multiple layers of lithium bearing volcanic ash, resulting from multiple eruptive events over the past 6 million years including eruptions from the 700,000-year-old Long Valley Caldera system and related events.  These ash layers are thought to contribute to the lithium brines extracted by Albemarle and are also likely involved in the formation of the exposed lithium rich clay deposits on the east side of Clayton Valley.

Volt Canyon Lithium Property

The Company owns a 100% interest in 80 placer claims covering approximately 635 hectares of alluvial sediments and clays located 122 km northeast of Tonopah, Nevada.

References

Prefeasibility Study Clayton Valley Lithium Project, Esmerelda County, Nevada, August 5, 2020, Amended March 15, 2021, Todd Fayram MMSA-QP (CMS), Terre A. Lane MMSA-QP (GRE), J.J. Brown, SME-RM (GRE), NI43-101 Technical Report for Century Lithium

Century Lithium Announces Positive Feasibility Study for the Clayton Valley Lithium Project, Nevada, April 29, 2024, Terre A Lane MMSA-QP (GRE), Hamid Samari, Principal Geologist, Todd-Fayram, Sr. V.P Metallurgy-Century Lithium, Alan Drake, Process Engineering, Haiming (Peter)Yuan Principal Geotechnical Engineer, Paul Blauch, Technical Director, Farza Kossari, Cost Estimating Engineer, Century Lithium Press Release.

On Behalf of the Board of Directors

"Tim Fernback"

Tim Fernback, President & CEO

Contact Information:

Email: info@gridbatterymetals.com

Phone: 604- 428-5690

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. This news release may contain forward-looking statements which include, but are not limited to, comments that involve future events and conditions, which are subject to various risks and uncertainties. Except for statements of historical facts, comments that address resource potential, upcoming work programs, geological interpretations, receipt and security of mineral property titles, availability of funds, and others are forward-looking. Forward-looking statements are not guarantees of future performance and actual results may vary materially from those statements. General business conditions are factors that could cause actual results to vary materially from forward-looking statements. It should be noted that results from any adjacent property(s) are not an indication of what may be found on the Company's property(s).

Copyright (c) 2024 TheNewswire - All rights reserved.

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Exploring Highly Prolific Lithium Assets in Nevada

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(TheNewswire)

Grid Battery Metals Inc..

Coquitlam, BC TheNewswire - March 17, 2025 - Grid Battery Metals Inc. (the "Company" or "Grid Battery") (TSXV: CELL, OTCQB: EVKRF FRA: NMK2) announces that further to its news release dated August 29, 2024, and the TSX Venture Exchange's ("Exchange") conditional acceptance letter dated October 9, 2024, the Company has now closed the "related party" transaction subject to final Exchange approval.

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Grid Battery Metals Update - Fall 2024 Drilling Results on its Clayton Valley Lithium Project

Grid Battery Metals Update - Fall 2024 Drilling Results on its Clayton Valley Lithium Project

(TheNewswire)

Grid Battery Metals Inc..

Coquitlam, BC TheNewswire - January 21, 2025 - Grid Battery Metals Inc. (the "Company" or "Grid") ( TSXV: CELL, OTCQB: EVKRF FRA: W47 ) is pleased to announce the results of its fall 2024 reverse circulation drilling program on the Company's claim block at Silver Peak, Clayton Valley, Esmeralda County, Nevada.  This strategic land package, covering approximately 2,300 acres (930 ha), directly adjoins the western portion of lithium producer Albemarle's (NYSE: ALB) evaporation ponds and is nearby Century Lithium Corp.'s (TSXV: LCE) (OTCQB: CYDVF) proposed 5,430-acre Angel Island Lithium Mine, which recently released a Positive Feasibility Study detailing a 40-year mine life and an after-tax NPV8 of $3.01 billion .

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Grid Battery Metals Update - Drilling Completed on its Clayton Valley Lithium Project

Grid Battery Metals Update - Drilling Completed on its Clayton Valley Lithium Project

Grid Battery Metals Inc. (the "Company" or "Grid") (TSXV: CELL)(OTCQB:EVKRF)(FRA:W47) is pleased to announce that its reverse circulation drilling program has now been completed on the Company's claim block at Silver Peak, Clayton Valley, Esmeralda County, Nevada. This strategic land package, covering approximately 2,300 acres (930 ha), directly adjoins the western portion of lithium producer Albemarle's (NYSE:ALB) evaporation ponds and is nearby Century Lithium Corp.'s (TSXV:LCE)(OTCQB:CYDVF) proposed 5,430-acre Angel Island Lithium Mine, which recently released a Positive Feasibility Study detailing a 40-year mine life and an after-tax NPV8 of $3.01 billion

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Grid Battery Metals Drilling Update on its Clayton Valley Lithium Project

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(TheNewswire)

Grid Battery Metals Inc..

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Grid Battery Metals Begins Drilling the Clayton Valley Lithium Project

Grid Battery Metals Begins Drilling the Clayton Valley Lithium Project

(TheNewswire)

Grid Battery Metals Inc..

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HIGHLIGHTS

- Trading commences on OTCQB under the ticker VTXXF.

- OTCQB recognised as an Established Public Market by the SEC.

- Offers enhanced investor benefits, including streamlined trading access for U.S.- based investors to VTX.

- Enables engagement with a network of U.S. investors, data distributions and media partners.

- ASX compliance qualifies for exemption under US regulations, minimising additional costs.

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- No new shares in Vertex have been issued as part of the quotation on the OTCQX Market in the USA.

"The US market will take a keen interest in Vertex, an Australian gold company which will be recognised for its high-grade, future free cash generation, exploration upside, and its Australian dollar market value. The OTCQB quotation makes Vertex more readily accessible to a wider audience at a time when the US market is bullish gold and witnessing record Gold prices". Roger Jackson Executive Chairman

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The ability to trade in the Company's existing ordinary shares on the ASX will not be affected by having the OTCQB facility and no new ordinary shares have been issued. VTX will continue to make announcements and disclosures to the Australian Securities Exchange through the Market Operating Rules and Listing Rule requirements.

The OTCQB is acknowledged by the SEC as an Established Public Market and serves as a prominent platform for U.S. and international companies in the entrepreneurial and growth stages. Eligibility requires companies to maintain up-to-date financial reporting (in line with ASX listing rule obligations), meet a minimum bid price requirement, and complete an annual verification and management certification process. As a trusted and transparent marketplace with streamlined access to U.S. investors, the OTCQB supports companies in building shareholder value, enhancing liquidity, and achieving fair market valuation.

The Company would like to thank David Batista of Viriathus Capital who have acted as Sponsor for the Company's application to commence cross-trading on the OTCQB.



About Vertex Minerals Limited:  

Vertex Minerals Limited (ASX:VTX) is an Australian based gold exploration company developing its advanced Hargraves and Hill End gold projects located in the highly prospective Eastern Lachlan Fold Belt of Central West NSW. Other Company assets include the Pride of Elvire gold project and Taylors Rock gold/nickel/lithium project both located in the Eastern Goldfields of WA. The focus of Vertex Minerals is to advance the commercial production of gold from its NSW projects embracing an ethical and environmentally sustainable approach.



Source:
Vertex Minerals Limited

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Group Eleven Intersects 7.5m of 20.1% Zn+Pb and 51 g/t Ag, incl. 2.2m of 37.5% Zn+Pb and 72 g/t Ag at Ballywire in Step-Out Drilling; Upcoming Drilling at Cu-Ag Target and 'D' Gravity Anomaly

Group Eleven Intersects 7.5m of 20.1% Zn+Pb and 51 g/t Ag, incl. 2.2m of 37.5% Zn+Pb and 72 g/t Ag at Ballywire in Step-Out Drilling; Upcoming Drilling at Cu-Ag Target and 'D' Gravity Anomaly

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 (and additional assays from a previously announced hole) 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:

  • G11-3552-29 intersected (from 189.3m):
    • 130.7m of 2.3% Zn+Pb (2.0% Zn and 0.3% Pb) and 13 g/t Ag, including
    • 7.5m of 20.1% Zn+Pb (19.1% Zn and 1.0% Pb) and 51 g/t Ag, including
    • 5.7m of 24.1% Zn+Pb (23.2% Zn and 1.0% Pb) and 60 g/t Ag, including
    • 2.2m of 37.5% Zn+Pb (36.9% Zn and 0.7% Pb) and 72 g/t Ag
    • Represents a 55m step-out down-dip from G11-3552-27
  • G11-3552-271 intersected (from 201.5m):
    • 70.5m of 3.4% Zn+Pb (2.2% Zn and 1.2% Pb) and 41 g/t Ag, including
    • 25.7m of 7.9% Zn+Pb (5.7% Zn and 2.2% Pb), 78 g/t Ag and 0.12% Cu and
    • 4.2m of 2.0% Zn+Pb (0.4% Zn and 1.6% Pb), 172 g/t Ag and 0.66% Cu, including
    • 0.9m of 3.6% Zn+Pb (0.9% Zn and 2.6% Pb), 511 g/t Ag and 2.01% Cu
    • Located 50m down-dip from G11-3552-25 (announced 06-Feb-2025)
  • G11-3552-29 expands the footprint of the recently announced 360m long, flat-lying zone of zinc-rich massive sulphide lenses by at least 50m down-dip, to a total of at least 125m down-dip
  • Drilling continues at Ballywire with two rigs testing further down-dip of the two holes released today, plus the NE extension; assay results are expected in due course
  • In several weeks, drilling will also begin testing (a) a Cu-Ag target below the Zn-Pb-Ag discovery horizon; and (b) a step-out target 1.3km to the ENE of the Ballywire discovery testing in the vicinity of the prospective 'D' gravity-high anomaly, at a locality with abundant calcite similar to the calcite typically observed immediately above high-grade mineralization along the discovery trend

"We are very pleased to see the NE massive sulphide zone expanded by a ninth consecutive high-grade hole," stated Bart Jaworski, CEO. "Additional excellent Ag and Cu values also continue to point to a stratigraphically deeper Cu-Ag horizon, which we are aiming to start drill testing for the very first time over the next few weeks. We also look forward to stepping out 1.3km ENE towards a very prospective area near the 'D' gravity high anomaly. This locality hosts abundant calcite bodies, commonly seen above high-grade mineralization at Ballywire. A nearby historic hole is also mineralized. With the Cu-Ag target, continued drilling to the NE and larger step outs along our prospective 6km trend, 2025 promises to be an exciting year of exploration for Group Eleven."

Cannot view this image? Visit: https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_002.jpg

Exhibit 1. Cross-Section Showing New Drilling (G11-3552-27, -29 and -31) at Ballywire Discovery

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_002full.jpg

Note: Partial assays from G11-3552-27 previously announced on 06-Feb-25, consisting of 24.8m of 8.1% Zn+Pb, 80 g/t Ag;

Cannot view this image? Visit: https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_003.jpg

Exhibit 2. Plan Map Showing New Drilling and Interpreted Cu-Ag 'Feeder' Structure

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_003full.jpg

Note: Partial assays from G11-3552-27 previously announced on 06-Feb-25, consisting of 24.8m of 8.1% Zn+Pb, 80 g/t Ag;

New Step-Out Holes at Ballywire Discovery

The Ballywire prospect at the Company's 100%-owned PG West Project in Republic of Ireland, is a relatively new zinc-lead-silver discovery (first announced Sept-2022). In addition to 44 holes drilled and reported by Group Eleven to date, the most recent four holes (G11-3552-24, -26, -28, and -29) and additional assays for previously announced hole, G11-3552-27, are reported today (see Exhibits 1 to 7).

High-grade mineralization from G11-3552-27 and -29 (see Page 1 and Exhibits 1 to 4) consists predominantly of massive and semi-massive sulphide (sphalerite, galena, pyrite, chalcopyrite and suspected tennantite-tetrahedrite), as well as, disseminated and vein hosted sulphide mineralization. Mineralization occurs along and/or close to the base of the Waulsortian Limestone (see Exhibit 1).

Exhibit 3. Summary of Assays from G11-3552-24, -26, -27, -28 and -29 at Ballywire

ItemFrom
(m)
To
(m)
Int
(m)
Zn
(%)
Pb
(%)
Zn+Pb
(%)
Ag
(g/t)
Cu
(%)
G11-3552-27201.45271.9470.492.221.203.4140.80.09
Incl.212.07237.8125.745.692.217.9077.80.12
Incl.219.42235.0615.648.303.2811.59122.10.19
Incl.218.47222.213.7412.183.0515.2375.3-
And228.51235.066.5511.065.6516.71240.00.42
Incl.230.36233.903.5413.268.0121.27395.10.73
And267.72271.944.220.401.581.97171.60.66
Incl.268.64269.490.850.932.623.55511.02.01
G11-3552-29189.33320.05130.721.990.262.2513.0-
Incl.224.27229.615.344.100.794.8812.5-
And259.03266.567.5319.081.0120.0951.3-
Incl.259.03264.745.7123.160.9524.1160.0-
Incl.259.03261.252.2236.860.6837.5471.7-
And307.91320.0512.140.230.040.2766.20.12
Incl.315.26320.054.790.380.050.42149.40.27
Incl.318.00320.052.050.090.040.12301.00.52
G11-3552-24186.26199.2012.940.150.040.192.1-
Incl.193.76197.313.550.300.100.404.8-
And235.85236.760.910.010.010.0136.10.35
G11-3552-26215.80216.360.560.830.791.6271.5-
Incl.215.80215.970.172.522.254.77190.0-
G11-3552-28157.95174.8116.860.020.580.593.1-
Incl.166.42169.282.860.051.261.319.0-
And172.99174.811.820.072.122.196.8-
And179.67181.491.820.030.170.2064.10.16
And218.66220.501.840.000.000.012.70.26

 

Note: True width of the intervals above as a percentage of the intersected interval is 90% (G11-3552-27), 80-90% (G11-3552-29), 90-100% (G11-3552-24), 80-90% (G11-3552-26) and 90-100% (G11-3552-28)

Holes drilled as 300m step-outs to the NE (G11-3552-24, -26 and -28; see Exhibit 2) returned zones of mineralization narrower and weaker than those at the main discovery trend (see Exhibit 3). Disseminated copper mineralization, as well as, mineralized veins and fractures, however, are strengthening towards the north, suggesting massive sulphide mineralization may be present further north (see northern-most projected mineralized trend in Exhibit 4). A second mineralized trend is also emerging to the south where the interpreted Cu-Ag rich 'feeder' fault pierced by drilled along the main discovery trend (see solid purple line in Exhibits 2 and 4) appears to correlate with mineralization intersected in G11-3552-08 (see Exhibit 2). More drilling is ongoing in the NE area to test the above targets.

Key 2025 Exploration Targets at Ballywire Discovery

Copper-Silver Target

As drilling progresses at Ballywire, it is increasingly evident that there exists an interpreted Cu-Ag 'feeder' fault parallel to and spatially associated with the main Zn-Pb-Ag discovery at Ballywire (see Exhibit 2). This 'feeder' fault hosts mineralization with up to 5.90% Cu and 1,440 g/t Ag, interpreted to have been transported by mineralizing fluids from below by vertical to steeply-dipping structures (see Exhibit 5). Today's results provide further evidence, with grades up to 2.01% Cu and 511 g/t Ag (see Exhibit 3). Meanwhile, the stratigraphy of the region suggests that approximately 100-200m below the discovery horizon (base of the Waulsortian Limestone), is the Lower Limestone Shale horizon, which 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, there is a chance the mineralizing system is much larger than at the neighbouring deposits (based on relatively large footprint to date), and if it is there, any Cu-Ag mineralization would notionally be intact below the existing Zn-Pb-Ag mineralization.

Given the compelling nature of the above exploration model, Group Eleven aims to begin drilling this deeper Cu-Ag target over the coming several weeks.

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Exhibit 4. Plan Map Showing Interpreted Cu-Ag 'Feeder' and Calcite Body Targets at Ballywire

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_004full.jpg

Note: Calcite bodies occurring at the discovery trend are not shown here (shown in Exhibit 6 instead)

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Exhibit 5. Cross-Section Showing Hypothesized Location of Cu-Ag Mineralization

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https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_005full.jpg

Calcite Body Vectors

As drilling progresses at Ballywire, it is increasingly evident that high-grade Zn-Pb-Ag mineralization at Ballywire is spatially associated with steeply dipping bodies of calcite (see Exhibit 6), interpreted to represent the 'exhaust' from the mineralization process below (i.e. dissolved limestone at the mineralized horizon is re-precipitated as calcite bodies immediately above). These calcite bodies may prove to be a strong exploration vector along the undrilled remainder of Ballywire's prospective 6km trend.

Two shallow historic holes, located 1.3km ENE from the current boundary of the Ballywire discovery, intercepted such calcite bodies (see Exhibits 4 and 7), yet were never followed up. This locality is also near the prospective 'D' gravity high anomaly and historic hole, 99-3352-05 (see Exhibit 7), which intersected mineralization of a tenor typically seen peripheral to massive sulphide zones at the discovery trend. Group Eleven aim to test this locality in the coming weeks.

Separately, two historic holes approx. 300m and 600m to the WSW, respectively, from the current boundary of the Ballywire discovery, also intercepted abundant calcite zones (see Exhibits 4 and 7) and were never followed up. Group Eleven aims to test these locations in due course.

Looking forward, six (6) drill holes (G11-3552-30 to -35; see Exhibit 2) are in progress with results expected in due course. Exhibit 2 shows drilling to date across 1.25km of the overall 2.6km long trend (see Exhibit 4) of significantly mineralized drill intercepts. This in turn is hosted within a 6km long prospective trend defined by four gravity high anomalies, only one of which (anomaly 'C') is systematically drilled to date (see Exhibit 7).

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Exhibit 6. Oblique 3D View of Calcite Bodies Spatially Associated with Mineralization at Ballywire

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_006full.jpg

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

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

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/245941_exhibit7.jpg

Notes to Exhibit 8: (a) Pallas Green MRE is owned by Glencore (see Glencore's Resources and Reserves Report dated December 31, 2023); (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

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/245941_figure8.jpg

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) and (FSE: 3GE) is a mineral exploration company focused on advanced stage zinc exploration in the Republic of Ireland. Group Eleven announced the Ballywire discovery in September 2022. 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)

Ballywire is located 20km from Company's 77.64%-owned Stonepark zinc-lead deposit2, which itself is located adjacent to Glencore's Pallas Green zinc-lead deposit3. 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.com and readers are urged to review these materials, including the technical reports filed with respect to the Company's mineral properties.

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