Heritage Mining Ltd. Completes 2022 Field Program

Heritage Mining Ltd. Completes 2022 Field Program

(TheNewswire)

Heritage Mining Ltd.

NOT INTENDED FOR DISTRIBUTION TO UNITED STATES NEWS WIRE SERVICES OR FOR DISSEMINATION IN THE UNITED STATES

Multiple high-grade gold vein systems channel sampled at Drayton-Black Lake

Heritage Mining Ltd. (CSE:HML) (" Heritage " or the " Company ") is pleased to report the completion of the 2022 field program at the Company's 15,257 Ha Drayton-Black Lake Project (" DBL" ). DBL is located approximately 20 km northeast of Sioux Lookout, Ontario (Fig. 1) and covers 30 km of the Central Volcanic and Southern Sedimentary domains within the Eagle-Wabigoon-Manitou (" EWM ") Greenstone Belt, which also hosts Treasury Metals Inc.'s Goliath Gold-Silver Complex immediately to the southwest. This year's exploration program included property-wide MagEM airborne geophysical surveying, regional mapping, prospecting and sampling in addition to the recently completed channel sampling work

Program Highlights

Alcona : Mineralized deformation corridor over 1,000 m (up to 200 m wide) consisting of multiple discrete zones of deformed volcanic rocks and shear parallel quartz veins.

  • Main Prospect - 2022 grab samples returned values up to 58.1 g/t Au

    • Nine channels completed (50 sample assays pending) over 250 m of strike

    • Individual quartz – carbonate – sulphide veins up to 60 cm wide

  • Pond Prospect - 2022 grab samples returned values up to 24.6 g/t Au

    • Nine channels completed (80 sample assays pending), over 250 m of strike

    • Up to meter scale quartz – carbonate – sulphide veins

Alcona-New Millennium : At least two mineralized deformation corridors consisting of multiple discrete zones of deformed volcanic rocks and shear parallel quartz veins.

  • New Millennium Prospect - 2022 grab samples returned values up to 46.5 g/t Au

    • Nine channels completed (42 sample assays pending)

    • Multiple quartz veins from 0.50 to 1.0 m wide, with carbonate and sulphides

    • Multi-element analysis of vein material averaged 19.3 g/t Au, 97.6 g/t Ag and 76 ppm Te

Moretti: Mineralized deformation corridor over 2,500 m consisting of discrete zones of deformed volcanic rocks and shear parallel quartz veins ranging from cm to metre scale. Drilling by previous operators identified narrow high-grade Au intervals (e.g., 18.78 g/t over 0.6 m and 190.7 g/t over 0.24 m) and an 8.5 tonne bulk sample returned 14.62 g/t Au (ca. 1950).  Refer to assessment file 52J04NE9387.

  • Moretti - 2022 grab sampling returned values up to 208 g/t Au

    • Seven channels completed (30 samples pending assays)

    • Multiple shear-parallel quartz veins, associated (Fe-) carbonate alteration, coarse gold observed

  • Black Lake - 2022 grab samples returned values up to 0.95 g/t Au

    • Sixteen channels completed (68 sample assays pending)

    • Evaluated multiple deformation zones with centimeter to meter quartz veins

Forster Area : Reconnaissance prospecting identified sheeted quartz veins referred historically to as the "Hi Grade Showing".

  • "Hi Grade Showing" - Five (5) samples collected, assays pending

    • Field confirmed the 6-meter-wide zone with multiple cm-scale quartz-carbonate veins that was historically sampled

    • Conecho Mines Ltd's 1951 report indicates "samples with no visible gold reported up to 1.52 oz (or 47.3g/t gold) and a grab sample with pin-point size visible gold reported 4.40 oz (or 136.8g/t gold), refer to Assessment file 52G13NW0039

Peter Schloo, CEO of Heritage Mining commented, "Our first pass field program at Drayton-Black Lake Project confirms the area is a highly prospective, yet significantly underexplored mineral district. Our systematic boots on the ground exploration philosophy has been highly successful, with the team discovering multiple new veins and extending known vein systems along strike.  Multiple meter-scale quartz veins and quartz stockwork zones reported high grade gold assays in rock grabs from Alcona-Main (58.1 g/t Au), Alcona-New Millennium ( 46.5 g/t Au ) and Moretti ( 208.0 g/t Au ) project areas (see Figure 1).  To optimize our drill target prioritization, we recently completed systematic channel-sampling across these high-grade structures and look forward to reporting assays when received.  These initial results, along with the highly anticipated channel-sample data, will provide Heritage valuable information as we plan systematic follow up for the winter and into the 2023 exploration program."


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Figure 1: (Top Left) Alcona Pond Vein Area (Top Right) Sheeted quartz veins at New Millennium (Bottom Left) Coarse gold collected in the Moretti Area (Bottom Right) Quartz veins within the Hi Grade Vein showing at the Forster Area.

Program Summary

The 2022 field program focused on characterizing known high-grade mineralization for the planned follow-up drill program (e.g., vein type, structural setting, alteration and mineralogical characteristics) and was successful in confirming numerous surface exposures of high-grade Au and Au-Ag mineralization throughout the property. This is the first time a systematic "belt-scale" approach has been undertaken in the Drayton-Black Lake area, building off a compilation of historic exploration program data sets, enhanced with new systematic mapping, sampling and multi-element geochemistry to develop multi-scale exploration vectors.

A recently completed channel sampling program included forty-eight individual channels) ranging from 1 to 18 m in length (average 3-5 m), see Figure 2.  In total, 323 samples (279 rocks and 44 QAQC samples) were submitted for Au + multi-element analysis. Samples were delivered to the lab in Thunder Bay in three batches. Outcrops were cleaned and mapped prior to marking for channel sampling. Channels were oriented to cross veins and deformed host rock and or oriented to cut dominant or distinct vein arrays or deformation/alteration exposures. Samples were marked at 1 m intervals (from start to end) and subdivided into 0.5 m intervals where single veins or discrete mineralization was noted. Where only partial samples (within marked metreage) were collected due to cover or poor ground conditions, a percent sample was noted. Sample weights averaged 3-5 kg. Blind field duplicates (where required by our Quality Management System) were prepared by collecting an individual sample, bagging, mixing and splitting the sample to provide two equal (by weight) sub-samples for that interval.


Click Image To View Full Size

Figure 2. Drayton-Black Lake property with regional geology showing 2022 rock sample and channel sample (collar) locations.

Several significant relationships (e.g., high Ag and Te tenors) and new prospect areas were recognized and these data will be used to improve exploration vectors as the Company advances the Property. Our work has confirmed that DBL contains an extensive, shallow, high-grade Au (+Au-Ag), structurally controlled mineral system that includes many untested high-grade prospects (e.g., New Millennium) and other prospects that have only seen limited drill-testing by previous operators (e.g., Alcona-Pond and Moretti Main). Several new prospects (Au >0.1 ppm) were also identified through regional prospecting and will be added the prospect pipeline for additional follow-up work.

Based on field observations and analytical results, the Company has noted the lack of visible gold (" VG ") in many samples with grades above 20-30 g/t Au. Preliminary multi-element analysis indicates a positive relationship between Au-Ag-Te. Therefore, to better understand the character of the high-grade Au mineralization and improve exploration vectors, the Company has initiated a deportment study for Alcona, Moretti and New Millennium. Six (6) samples have been sent to Actlabs in Dryden, Ontario for complete multi-element and QEMSCAN (Quantitative Evaluation of Materials by Scanning Electron Microscopy) analysis.

For further information please see the Heritage's profile on SEDAR at www.sedar.com   .

ABOUT THE DRAYTON-BLACK LAKE PROJECT

The Drayton-Black Lake Project is located near the town of Sioux Lookout in Northern Ontario and comprises more than 15,000 Ha within the Eagle-Wabigoon-Manitou ("EWM") Greenstone Belt along strike of and contiguous with Treasury Metals Inc.'s Goliath Gold-Silver Complex. There are numerous historic high-grade gold (silver, copper) prospects throughout the property within the Central Volcanic domain. All set within a broad multi-kilometer regional-scale deformation corridor with associated secondary and tertiary structural elements. Mineralization is typically shear-hosted quartz-carbonate veins with minor sulphides (1-5%). Locally, mineralized massive sulphide (Py +/- Cpy) occurrences have been documented. Some of the more sulphide rich Au + Au-Ag occurrences in the Southern Sedimentary domain have been notionally reclassified (e.g., Treasury Metal Goliath Deposit) as a hybrid or pre-orogenic atypical greenstone gold (POAGG).

Heritage employs a rigorous quality management system for field sampling and analysis. All samples and sample sites are described, photographed and geo-referenced and digitally archived at the time of sample collection. Material is securely bagged at the sample site and returned to the field office for secure storage. Sampled are delivered by Company personnel to the ALS laboratory in Thunder Bay, Ontario for prep. Samples are crushed (min. 1 kg) and pulverized (250 g; PREP-31A). Au values are determined by 50 g fire assay (Au-AA24), overlimit (Au) are treated with a gravimetric finish (Au-GRA22) and overlimit Ag are treated with acid digestion and ICP/FA finish (Ag-OG62). Multi-element analysis is provided by ICP-MS (ME-MS61). Blind duplicates, blanks and CRM (Certified Reference Materials) are inserted on a regular basis and p ulps and rejects are retained for check and duplicate analysis.

Scientific and technical information contained in this press release has been prepared under the supervision of Stephen Hughes, P. Geo. Technical Advisor to HML, a qualified person within the meaning of National Instrument 43-101 – Standards of Disclosure for Mineral Projects .

Sampling protocols, quality control and assurance measures and geochemical results related to historic results quoted in this news release (e.g., sampling, drilling, trenching and other data) have not been verified by the Qualified Person and therefore must be regarded as estimates.

ABOUT HERITAGE MINING LTD.

The Corporation is a Canadian mineral exploration company advancing its two high grade gold-silver-copper projects in Northwestern Ontario. The Drayton-Black Lake and the Contact Bay projects are located near Sioux Lookout in the underexplored Eagle-Wabigoon-Manitou Greenstone Belt . Both projects benefit from a wealth of historic data, excellent site access and logistical support from the local community. The Corporation is well capitalized, with a tight capital structure.

For further information, please contact:

Heritage Mining Ltd.

Peter Schloo, CPA, CA, CFA

President, CEO and Director

Phone: (905) 505-0918

Email: peter@heritagemining.ca

FORWARD-LOOKING STATEMENTS

This news release contains certain statements that constitute forward looking information within the meaning of applicable securities laws. These statements relate to future events of Heritage Mining Ltd. (" Heritage " or the " Corporation "). Any statements that express or involve discussions with respect to predictions, expectations, beliefs, plans, projections, objectives, assumptions or future events or performance (often, but not always, using words or phrases such as "seek", "anticipate", "plan", "continue", "estimate", "expect", "forecast", "may", "will", "project", "predict", "potential", "targeting", "intend", "could", "might", "should", "believe", "outlook" and similar expressions) are not statements of historical fact and may be forward looking information. All statements, other than statements of historical fact, included herein are forward-looking statements.

Forward looking information involves known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements of the Corporation to be materially different from any future results, performance or achievements expressed or implied by the forward-looking information. Such risks include, among others, the inherent risk of the mining industry; adverse economic and market developments; the risk that the Corporation will not be successful in completing additional acquisitions; risks relating to the estimation of mineral resources; the possibility that the Corporation's estimated burn rate may be higher than anticipated; risks of unexpected cost increases; risks of labour shortages; risks relating to exploration and development activities; risks relating to future prices of mineral resources; risks related to work site accidents, risks related to geological uncertainties and variations; risks related to government and community support of the Corporation's projects; risks related to global pandemics and other risks related to the mining industry. The Corporation believes that the expectations reflected in such forward-looking information 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. These statements speak only as of the date of this news release. The Corporation does not intend, and does not assume any obligation, to update any forward‐looking information except as required by law.

This document does not constitute an offer to sell, or a solicitation of an offer to buy, securities of the Corporation in Canada, the United States or any other jurisdiction. Any such offer to sell or solicitation of an offer to buy the securities described herein will be made only pursuant to subscription documentation between the Corporation and prospective purchasers. Any such offering will be made in reliance upon exemptions from the prospectus and registration requirements under applicable securities laws, pursuant to a subscription agreement to be entered into by the Corporation and prospective investors.

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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 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."

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

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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;

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

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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

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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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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

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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

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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, 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

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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) 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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