Power Nickel Files the NI 43-101 Technical Report for the Mineral Resource Estimate of the Nisk Project

Power Nickel Files the NI 43-101 Technical Report for the Mineral Resource Estimate of the Nisk Project

Power Nickel Inc. (the "Company" or "Power Nickel") (TSX-V:PNPN)(OTCBB:CMETF)(Frankfurt IVVI) has filed on SEDAR the Technical Report entitled "NI 43 101 Technical Report and Mineral Resource Estimate for the Nisk Project, Eeyou Istchee James Bay territory, Québec". The Technical Report was prepared by 3DGeo Solution Inc. (3DGS) of Val-d'Or, Québec, to support the disclosure of the Nisk Project 2022 Mineral Resource Estimate on July 19, 2022. The Technical Report is available on SEDAR and will be made available on the company's website

Power Nickel Inc., Tuesday, August 30, 2022, Press release picture

Outlined below is a summary of Power Nickel's Nisk Project Mineral Resource Estimate; with an effective date of May 17, 2022:

The Mineral Resource has been defined in both Open-Pit and Underground mining scenarios

The combined estimated Indicated Resources is 2.6 million tonnes grading 1.20 %NiEq, using a base case cut-off grade of 0.33 %NiEq for open pit constrained resources and a base case cut-off grade of 0.91 %NiEq for underground constrained resources.

The combined estimated Inferred Resources is 1.4 million tonnes grading 1.29 %NiEq, using a base case cut-off grade of 0.33 %NiEq for open pit constrained resources and a base case cut-off grade of 0.91 %NiEq for underground constrained resources.

The Nisk Project is located south of James Bay, a region that is the site of several mining projects (Figure 1) and improving infrastructure (Figure 2).

Figure 1 - Location of the Nisk Project with respect to the location of other known deposits.

Power Nickel Inc., Tuesday, August 30, 2022, Press release picture

Figure 2 - Location of the Nisk Project with respect to the current infrastructure available in the area.

Power Nickel Inc., Tuesday, August 30, 2022, Press release picture

Power Nickel completed the acquisition of its option to acquire up to 80% of the Nisk Project from Critical Elements Lithium Corp. The Nisk Project comprises a significant land position (20 kilometers of strike length) with numerous high-grade Nickel intercepts. Since completion of the option, Power Nickel retained 3DGeo Solution Inc to create a geological model of the Nisk Project and used this as a guide to the very successful initial Power Nickel 2400-metre drill program completed last December and reported in March of 2022.

Based on this drill program and the historical drill results, 3DGeo Solution Inc. was mandated to produce a NI 43-101 compliant Mineral Resource Estimate and Technical Report. Engineering work related to defining a constraining pit shell and underground mineable shapes was contracted to InnovExplo Inc. The Highlights of the Mineral Resource Estimate and Technical Report are below.

Table 1 - 2022 Nisk Project Mineral Resource Estimate.

Note: NiEq = Nickel Equivalent, Ni = Nickel, Cu = Copper, Co = Cobalt, Pt = Platinum, Pd = Palladium, Au = Gold, Ag = Silver, % = Percent, g = Gram, t = Metric tonne

Notes to Accompany Mineral Resource Table:

1. The Independent Qualified Persons for the purposes of this Mineral Resource Estimate (MRE), as defined in NI 43-101, is Kenneth Williamson, P.Geo.. (OGQ # 1490) of Solution 3DGéo inc. The effective date of the estimate is May 17, 2022.

2. The estimate of the mineral resources of the Nisk Project complies with the "CIM Estimation of Mineral Resources and Mineral Reserves Best Practice Guidelines" of November 29, 2019. The Mineral Resources were estimated in accordance with the Canadian Institute of Mining, Metallurgy, and Petroleum (CIM), CIM Standards on Mineral Resources and Reserves, Definitions (2014), and Best Practices Guidelines (2019) prepared by the CIM Standing Committee on Reserve Definitions and adopted by the CIM Council.

3. These mineral resources are not mineral reserves since their economic viability has not been demonstrated.

4. The resources are presented before dilution and in situ and are considered to have reasonable prospects of economic extraction. Isolated and discontinuous blocks with a grade greater than the selected cut-off grade are excluded from the estimate of underground mineral resources. The blocks that must be included, i.e., isolated blocks with a grade below the cut-off grade located within potentially mineable volumes, have been included in the mineral resource estimate.

5. As of May 17, 2022, the database included a total of 66 drill holes (59 historic and seven recent 2021 drill holes) totaling 15,266.3 meters of drilling.

6. A value of half of the assay lab detection limit for each element was used as a grade for the un-assayed core.

7. The assays were grouped within the mineralized domains in composites of 1.00 meters in length.

8. The block model was prepared using Leapfrog® Geo and Edge software. The block model consists of 2-meter parent blocks and sub-blocks of 1 meter. The block model has a dip azimuth of 340°.

9. An interpolation according to the "inverse distance squared" ("ID2") method was performed to estimate the grades in the interpreted mineralized volume.

10. An interpolation according to the "inverse distance squared" ("ID2") method was performed to estimate the Density (SG) in the interpreted mineralized volume. Sample intervals with missing SG values were calculated based on a strong correlation with %Ni. The calculation used was SG = (0.7001 x %Ni) + 2.6751.

11. The "Open Pit" mineral resources are presented at a cut-off grade of 0.33 %NiEq and are confined within a "Whittle" pit shell. The "Underground" mineral resources are presented at a cut-off grade of 0.91 %NiEq and are confined within volumes defined using "DSO" (Deswik Stope Shape Optimizer). These volumes correspond to groups of contiguous blocks with a reasonable size to be exploited by underground mining methods.

12. The engineering work required for the cut-off grade estimation and the creation of the DSO volumes were performed by InnovExplo Inc., and the following economic parameters were used: US $8.00/lb Nickel, $3.00/lb Cu, $25.00/lb Cobalt, $1000/Oz Platinum, $1000/Oz Palladium, $1300/Oz Gold, and $17.00/Oz Silver; Exchange rate of USD/CAD 1.30, metallurgical recovery of 85%, total processing cost CA $40.00/t, mining cost CA $6.00/t, mining overburden cost CA $4.20/t, underground mining cost CA $110.00/t, G&A cost CA $12.20/t, northern logistics costs CA $10.00/t. It should be noted that the G&A cost could be underestimated depending on the extraction sequence chosen.

13. The independent qualified person is not aware of any environmental, licensing, legal, title-related, tax, socio-political or marketing-related issue, or any other relevant issue that could have a material impact on the estimate of mineral resources.

14. The numbers of tonnes are rounded to the nearest hundred to reflect uncertainties, which may cause slight differences.

"Power Nickel was extremely pleased with the inaugural Mineral Resource Estimate and Technical Report. When taken in context with our very conservative assumptions and the clear infill drilling opportunities, as outlined below in the two figures showing isometric views of the potentially economic pit-constrained and underground stope-constrained mineral resources, we feel we have shown Nisk has significant commercial potential. The resource update has clearly indicated some additional infill drilling is needed, and these holes, as well as step-out targets, are now in the process of being permitted as part of our upcoming fully funded drill program," commented Power Nickel CEO Terry Lynch. "We already have permitted several drill targets to the flanks of the current deposit designed to extend the deposit and test new potential pods for additional resources. Historically, Nickel Sulfide deposits don't exist in isolated solo deposits but typically have a string of pearl formation where multiple pearls or pods of resources are assembled in a close geographic area. The next round of drilling, commencing in September, will focus on infill drilling targets outlined by the Mineral Resources Estimate and Technical Report and on this search to extend and discover new Nickel pods. We expect this phase of drilling to continue through the fall with a minimum of 3,000 meters drilled and a maximum of 7,000 meters depending on our ability to continue to intersect the Black Peridotite rock, which is carrying the Nickel grade in the Nisk deposit."

Figure 3 shows the grade of the Nickel Equivalent (%NiEq) mineral resources, and Figure 4 shows the mineral resource classification (indicated and inferred). Note that portions of the deposit still contain unclassified mineral potential and requiring more infill drilling to potentially include this in a future updated MRE.

Power Nickel Inc., Tuesday, August 30, 2022, Press release picture

Figure 3 - Isometric view of the 2022 Nisk Project Mineral Resource Estimate, showing both the open pit constrained resources (using a cut-off grade of 0.33 %NiEq) and the underground constrained resources (at a cut-off grade of 0.91 %NiEq).

Power Nickel Inc., Tuesday, August 30, 2022, Press release picture


Figure 4 - Isometric view of the 2022 Nisk Project Mineral Resource Classification, showing both the open pit constrained resources (using a cut-off grade of 0.33 %NiEq) and the underground constrained resources (at a cut-off grade of 0.91 %NiEq).

Power Nickel Inc., Tuesday, August 30, 2022, Press release picture

Table 2 shows the different cut-off grade (CoG) sensitivities based on Nickel Price (+/- 10% and 20% of the base case scenario). The base case scenario is highlighted in light yellow. Table 3 shows the CoG and correlated Nickel metal prices in USD$ per pound.

Table 2 - 2022 Nisk Project Mineral Resource Estimate Cut-off Grade Sensitivity.

Power Nickel Inc., Tuesday, August 30, 2022, Press release picture

Note: NiEq = Nickel Equivalent, Ni = Nickel, Cu = Copper, Co = Cobalt, Pt = Platinum, Pd = Palladium, Au = Gold, Ag = Silver, % = Percent, g = Gram, t = Metric tonne; Base Case highlighted in light yellow.

Table 3 - 2022 Nisk Project Mineral Resource Estimate Cut-off Grade Sensitivity with Correlated Nickel Price Sensitivity.

Power Nickel Inc., Tuesday, August 30, 2022, Press release picture

Qualified Persons

This Technical Report has been prepared by Kenneth Williamson, P.Geo., M.Sc. and Matthew DeGasperis, P.Geo., B.Sc., from 3DGS. The 2022 MRE was designed by Kenneth Williamson, P.Geo., M.Sc.

Kenneth Williamson, P.Geo., M.Sc., is a professional geologist member in good standing of the Ordre des Géologues du Québec (OGQ license #1490) and the Professional Geoscientists of Ontario (license #2176) and is the independent qualified person ("QP") as defined by NI 43-101 for all sections of the Technical Report.

Matthew DeGasperis, P.Geo., B.Sc., is a professional geologist member in good standing of the Ordre des Géologues du Québec (OGQ license #2261) and the Professional Geoscientists of Ontario (license #3438) and is the independent qualified person ("QP") as defined by NI 43-101 for all sections of the Technical Report, except for Item 14 - Mineral Resource Estimate. Work performed on Item 14 has been done under the direct supervision of Kenneth Williamson, P.Geo.

About Power Nickel Inc.

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

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

The NISK property comprises a significant land position (20 kilometers of strike length) with numerous high-grade intercepts. Power Nickel, formerly Chilean Metals, is focused on confirming and expanding its current high-grade nickel-copper PGE mineralization historical resource by preparing a new Mineral Resource Estimate in accordance with NI 43-101, identifying additional high-grade mineralization, and developing a process to potentially produce nickel sulphates responsibly for batteries to be used in the electric vehicles industry.

Power Nickel (then called Chilean Metals) announced on June 8th, 2021, that an agreement has been made to complete the 100% acquisition of its Golden Ivan project in the heart of the Golden Triangle. The Golden Triangle has reported mineral resources (past production and current resources) in a total of 67 million ounces of gold, 569 million ounces of silver, and 27 billion pounds of copper. This property hosts two known mineral showings (gold ore and magee) and a portion of the past-producing Silverado mine, which was reportedly exploited between 1921 and 1939. These mineral showings are described as polymetallic veins containing quantities of silver, lead, zinc, plus/minus gold, and plus/minus copper.

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

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

Mr. Terry Lynch, CEO
647-448-8044
terry@powernickel.com

For further information, readers are encouraged to contact:

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

SOURCE:Power Nickel Inc.



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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."

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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

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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