Emerita Intersects 13.0 Meters Grading 0.2% Copper; 3.6% Lead; 13.1% Zinc; 1.35 g/t Gold and 120.9 g/t Silver and 22.9 Meters Grading 0.6% Copper; 2.0% Lead; 4.8% Zinc; 0.58 g/t Gold and 79.2 g/t Silver Extending La Romanera Deposit at Depth, Completes Environmental Base Line Studies at IBW

Emerita Intersects 13.0 Meters Grading 0.2% Copper; 3.6% Lead; 13.1% Zinc; 1.35 g/t Gold and 120.9 g/t Silver and 22.9 Meters Grading 0.6% Copper; 2.0% Lead; 4.8% Zinc; 0.58 g/t Gold and 79.2 g/t Silver Extending La Romanera Deposit at Depth, Completes Environmental Base Line Studies at IBW

Emerita Resources Corp. (TSX V: EMO; OTCQB: EMOTF; FSE: LLJA) (the "Company" or "Emerita") is pleased to announce additional assay results from the ongoing delineation drilling program at La Romanera Deposit, part of Emerita's wholly owned Iberian Belt West project ("IBW" or the "Project"). IBW hosts three previously identified massive sulphide deposits: La Infanta, La Romanera and El Cura. Results contained in this release are from La Romanera. All deposits are open for expansion along strike and at depth.

Assays have been received for two additional drill holes that were not included in the recently announced NI 43-101 compliant mineral resource estimate (Please see Emerita's news release dated May 23, 2023). See Figures 1, 2 and 3 for intercept locations and Table 1 for diamond drilling data. Drill holes LR146 and LR147 demonstrate that the deposit remains open at depth and is high grade and thick in this central area.

According to Ian Parkinson, EVP Corporate Development and Capital Markets for Emerita, "It is exciting to see such strong results as a follow up to the recently announced maiden mineral resource estimate at IBW. La Romanera is the cornerstone deposit on this Project and it appears to be sustaining excellent thicknesses and higher than average grades as we continue to expand the mineral resource at relatively shallow depth."

Drill Hole LR146:

The Upper Lens was intersected at 580.9 m down the hole. It encountered 13.0 meters grading 0.2% Copper; 3.6% Lead; 13.1% Zinc; 1.35 g/t Gold and 120.9 g/t Silver; including 6.0 meters grading 0.3% Copper; 4.8% Lead; 15.9% Zinc; 2.32 g/t Gold and 181.5 g/t Silver . The Lower Lens was intersected at 593.9 meters down the hole. It comprised 22.9 meters grading 0.6% Copper; 2.0% Lead; 4.8% Zinc; 0.58 g/t Gold and 79.2 g/t Silver; including 3.9 meters grading 0.3% Copper; 6.1% Lead; 9.1% Zinc; 2.36 g/t Gold and 247.8 g/t Silver .

Drill Hole LR147:

The Upper Lens was intersected at 649.3 m down the hole . It encountered 16.5 meters grading 0.4% Copper; 0.1% Lead; 0.2% Zinc; 0.17 g/t Gold and 22.1 g/t Silver, including 2.0 meters grading 0.4 % Copper; 0.1 % Lead; 0.4 % Zinc; 0.22 g/t Gold and 106.5 g/t Silver. The Lower Lens was intersected at 665.75 m down the hole. It comprised 17.2 meters grading 0.4% Copper; 2.0% Lead; 9.8% Zinc; 0.64 g/t Gold and 89.3 g/t Silver; including 7.0 meters grading 0.5% Copper; 2.9% Lead; 16.5% Zinc; 0.83 g/t Gold and 57.0 g/t Silver.

The current drilling program is focused on testing the extension of La Romanera deposit at depth. Drill holes LR152 and LR153 are in progress. Drill holes LR148, LR150 and LR151 are completed with assays pending and have intersected significant massive sulphide intervals including; 40.0 m (24.0 m for the Upper Lens; 16.0 m for the Lower Lens), 4.3 m and 40.9 m (27.8 m for the Upper Lens; 13.1m for the Lower Lens) of massive sulphides, respectively; increasing the potential for additional resources expansion.

A down-the-hole transient electromagnetic ("TEM") survey was completed in drillhole LR151, showing a conductor anomaly which continues for another 100 m at depth. The downhole TEM survey is being used by the exploration team to target the depth extension of La Romanera deposit.


230621_EMO_Fig 1

Figure 1: Diamond drilling plan map
View Figure 1 here:
https://www.globenewswire.com/NewsRoom/AttachmentNg/062d6db0-4a8f-4138-b20b-8e366248a59b


230621_EMO_Fig 2

Figure 2: Longitudinal section of the Lower Lens, La Romanera showing grade contours. Note the thick, high-grade trend of the deposit at depth where the extension drilling is focused. These areas are thicker and higher grade than the average resource grade which will provide an important contribution to a future resource estimate update.
View Figure 2 here:
https://www.globenewswire.com/NewsRoom/AttachmentNg/0008b42a-49c7-4a7f-98bc-728d39015784


230621_EMO_Fig 3

Figure 3: Longitudinal section of the Upper Lens, La Romanera showing grade contours. Note the thick, high grade trend at depth along the east side of the lens where the extension drilling is focused.
View Figure 3 here:
https://www.globenewswire.com/NewsRoom/AttachmentNg/d625b583-948d-4d69-9169-c9ac68d8b6f4

*ZnEq % formula used for Figure 2 and 3: ZnEq % = [(Zn grade * Zn recovery * Zn price) + (Pb grade * Pb recovery * Pb price) + (Cu grade * Cu recovery * Cu price) + (Ag grade * Ag recovery * Ag price) + (Au grade * Au recovery * Au price)] / (Zn recovery * Zn price)

Table 1: Diamond Drilling Data

DDH Easting Northing Elevation azimuth dip depth
(m)
FROM TO Width
(m)
Cu_% Pb_% Zn_% Au_g/t Ag_g/t LENS
LR146 646802 4172735 150 212 -62 645.5 580.9 593.9 13.0 0.2 3.6 13.1 1.35 120.9 UL
incl. 585.9 591.9 6.0 0.3 4.8 15.9 2.32 181.5 UL
LR146 593.9 616.8 22.9 0.6 2.0 4.8 0.58 79.2 LL
incl. 611.9 615.8 3.9 0.3 6.1 9.1 2.36 247.8 LL
LR147 646751 4172871 154 198 -56 701.3 649.3 665.8 16.5 0.4 0.1 0.2 0.17 22.1 UL
incl. 659.0 661.0 2.0 0.4 0.1 0.4 0.22 106.5 UL
LR147 665.8 682.9 17.2 0.4 2.0 9.8 0.64 89.3 LL
incl. 674.0 681.0 7.0 0.5 2.9 16.5 0.83 57.0 LL


Next Steps

The Company has recently strengthened its treasury with successful financings generating gross proceeds of $11 million which, coupled with the existing treasury, provides the runway to efficiently advance the Project towards permitting and a production decision. The key activities planned for the remainder of 2023 will be as follows:

  • Continue to expand La Romanera Deposit at IBW. The Company presently has six (6) diamond drills operating on the Project.
  • Complete the initial drilling on the historical El Cura deposit which is situated approximately midway between La Infanta and La Romanera of the IBW property. This program has commenced.
  • Complete metallurgical studies on La Romanera and La Infanta. This program has commenced, and the Company has contracted metallurgical support from SRK to work as part of the owners team and selected Wardell Armstrong LLP of the UK, who are highly experienced with Iberian Pyrite Belt deposits, to do the actual laboratory testing for the metallurgy.
  • Complete initial conceptual mine planning to a level appropriate to support site selection for future infrastructure as well as conversion of Exploration Licenses to Exploitation Licenses at IBW. Grupo IPH, a Spanish mining engineering firm based in Huelva that contracts for mines in the region is being contracted to complete this work.
  • Complete the initial exploration drilling campaign at the Nuevo Tintillo project. Drilling will commence after the summer season when heat related operating restrictions have been lifted.

Baseline Studies Completed

Emerita Resources has completed the Baseline Studies at the IBW project. The objectives of the studies are to gain an understanding of the current natural environment of the site, support further mine development decisions and management plans. The Company engaged the services of specialist Spanish companies with broad experience in Baseline Studies:

  • BIOGEOS, Estudios Ambientales SL
  • Diseño de Soluciones Medioambientales (DSM)
  • Laboratorios MICROAL SL

The Baseline Studies were initiated in June 2022, due to the need to integrate the environmental variability in both the current operational phase of the authorized exploration license and in the design stage of the future mining project within the regulatory framework of the Exploitation Concession associated with "IP. LA ROMANERA No. 15,029", which includes the La Romanera, El Cura and La Infanta deposits.

The Environmental Baseline Study lasted one year and consisted of the following technical analyses:

  • Diagnosis of the natural environment and landscape.
  • Analytical investigation of soils and water (surface and subsurface).
  • Hydrological and hydrogeological study (water balance).

The purpose of the work carried out has served to:

  • Establish a Mining-Environmental management process necessary to establish a zoning of areas, delimiting exclusion zones and admission zones for future activities and facilities linked to the future mining exploitation.
  • To update the official environmental information offered by the Environmental Administration.

Quality Assurance/Quality Control

Drilling at La Romanera is HQ size and core is placed into core trays at the drill site and transported directly from the site to Emerita's coreshack (15Km) from La Romanera and (8Km) from La Infanta. Once the cores are received at Emerita's coreshack they are photographed and geotechnical logging is performed. Geological, mineralogical and structural logging follows and mineralized zones are identified. The samples are marked every 1m or less, and respecting lithological contacts, with most of the samples 1.0m long. The zone immediately above and below the mineralized zones are also sampled. Core samples are sawed in half and half of the core is returned to the core tray for future reference. Once the core samples are cut, bagged and tagged, they are shipped to the ALS laboratory in Seville by Emerita personnel where sample preparation is done. In Seville, ALS performs the mechanical preparation of the samples and then the pulps are sent to ALS Ireland (ICP) and ALS Romania (fire assay). The analysis at ALS Lab corresponds to the ME-ICPore (19 elements) package, together with the Au-AA23 fire assay (Gold).

10% of the analyzed samples correspond to control samples (fine blanks, coarse blanks, high, medium and low grade standards). In addition, 10% of pulps are reanalyzed at a second independent certified laboratory (AGQ Lab Sevilla). When the analysis is completed, the certificates are received from the laboratory and the QA/QC protocol identifies any deviation or anomaly in the results and the entire batch is reassayed in such case. Once the data is approved by the QA/QC protocol assays are entered digitally directly into the database.

Qualified Person

The scientific and technical information in this news release has been reviewed and approved by Mr. Joaquin Merino, P.Geo, President of the Company and a Qualified Person as defined by NI 43-101 of the Canadian Securities Administrators.

About Emerita Resources Corp.

Emerita is a natural resource company engaged in the acquisition, exploration and development of mineral properties in Europe, with a primary focus on exploring in Spain. The Company's corporate office and technical team are based in Sevilla, Spain with an administrative office in Toronto, Canada.

For further information, contact:

Joaquin Merino
+34 (628) 1754 66 (Spain)

Vincent Chen
+1 778 990 9433 (Toronto)
info@emeritaresources.com

Cautionary Note Regarding Forward-looking Information

This press release contains "forward-looking information" within the meaning of applicable Canadian securities legislation. Forward-looking information includes, without limitation, the mineralization of the IBW Project; the timing of assay results; the prospectivity of the Project and Nuevo Tintillo; the economic viability of the Project; the results of metallurgical studies; the Company's ability to obtain an exploitation licence and other permits and approvals for the Project; site selection for infrastructure; the results of baseline studies and other studies and the Company's future plans. Generally, forward-looking information can be identified by the use of forward-looking terminology such as "plans", "expects" or "does not expect", "is expected", "budget", "scheduled", "estimates", "forecasts", "intends", "anticipates" or "does not anticipate", or "believes", or variations of such words and phrases or state that certain actions, events or results "may", "could", "would", "might" or "will be taken", "occur" or "be achieved". Forward- looking information is subject to known and unknown risks, uncertainties and other factors that may cause the actual results, level of activity, performance or achievements of Emerita, as the case may be, to be materially different from those expressed or implied by such forward-looking information, including but not limited to: general business, economic, competitive, geopolitical and social uncertainties; the actual results of current exploration activities; risks associated with operation in foreign jurisdictions; ability to successfully integrate the purchased properties; foreign operations risks; and other risks inherent in the mining industry. Although Emerita has attempted to identify important factors that could cause actual results to differ materially from those contained in 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 information 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 information. Emerita does not undertake to update any forward-looking information, except in accordance with applicable securities laws.

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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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

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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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