Group Eleven Welcomes Franz Bollmann to the Board of Directors

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) ("Group Eleven" or the "Company") is pleased to announce that Franz Bollmann has been appointed to the Board of Directors. Mr. Bollmann has been nominated by Glencore Canada Corporation (which owns 16.1% of the Company) and will replace Gatlin Smeijers, who has stepped down from the Board, effective March 31, 2025, to pursue another opportunity.

Bart Jaworski, CEO of Group Eleven, commented: "We are delighted to welcome Franz to the team and look forward to working with him to further grow shareholder value. On behalf of the Company, I would also like to thank Gatlin for his valuable insights and guidance during his tenure as director and wish him the very best on his new endeavour."

Mr. Bollmann currently serves as Finance Manager at Glencore Zinc and as a Director of Glencore Servicios Corporativos Spain. Mr. Bollmann joined Glencore in 2014, working across finance, commercial, and business development roles in the Latam region. He also served as a director of Volcan Compañia Minera. Prior to joining Glencore, Mr. Bollmann worked in sales and trading at Raymond James in the United States. He holds a degree in Finance and a minor in Mathematics from the University of Arkansas.

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 zinc-lead-silver discovery in September 2022. Ballywire is located 20km from Company's 77.64%-owned Stonepark zinc-lead deposit¹, which itself is located adjacent to Glencore's Pallas Green zinc-lead deposit². The Company's two largest shareholders are Glencore Canada Corp. (16.1% interest) and Michael Gentile (16.0%). Additional information about the Company is available at www.groupelevenresources.com.

ON BEHALF OF THE BOARD OF DIRECTORS
Bart Jaworski, P.Geo.
Chief Executive Officer

E: b.jaworski@groupelevenresources.com | T: +353-85-833-2463
E: j.webb@groupelevenresources.com | T: 604-644-9514

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Information

This press release contains forward-looking statements within the meaning of applicable securities legislation. Such statements include, without limitation, statements regarding the future results of operations, performance and achievements of the Company, including the timing, content, cost and results of proposed work programs, the discovery and delineation of mineral deposits/resources/ reserves and geological interpretations. Although the Company believes that such statements are reasonable, it can give no assurance that such expectations will prove to be correct. Forward-looking statements are typically identified by words such as: believe, expect, anticipate, intend, estimate, postulate and similar expressions, or are those, which, by their nature, refer to future events. The Company cautions investors that any forward-looking statements by the Company are not guarantees of future results or performance, and that actual results may differ materially from those in forward looking statements as a result of various factors, including, but not limited to, variations in the nature, quality and quantity of any mineral deposits that may be located. All of the Company's public disclosure filings may be accessed via www.sedar.com and readers are urged to review these materials, including the technical reports filed with respect to the Company's mineral properties.

¹ Stonepark MRE is 5.1 million tonnes of 11.3% Zn+Pb (8.7% Zn and 2.6% Pb), Inferred (Apr-17-2018)
² Pallas Green MRE is 45.4 million tonnes of 8.4% Zn+Pb (7.2% Zn + 1.2% Pb), Inferred (Glencore, Dec-31-2024)

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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."

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;

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

Item	From (m)	To (m)	Int (m)	Zn (%)	Pb (%)	Zn+Pb (%)	Ag (g/t)	Cu (%)
G11-3552-27	201.45	271.94	70.49	2.22	1.20	3.41	40.8	0.09
Incl.	212.07	237.81	25.74	5.69	2.21	7.90	77.8	0.12
Incl.	219.42	235.06	15.64	8.30	3.28	11.59	122.1	0.19
Incl.	218.47	222.21	3.74	12.18	3.05	15.23	75.3	-
And	228.51	235.06	6.55	11.06	5.65	16.71	240.0	0.42
Incl.	230.36	233.90	3.54	13.26	8.01	21.27	395.1	0.73
And	267.72	271.94	4.22	0.40	1.58	1.97	171.6	0.66
Incl.	268.64	269.49	0.85	0.93	2.62	3.55	511.0	2.01
G11-3552-29	189.33	320.05	130.72	1.99	0.26	2.25	13.0	-
Incl.	224.27	229.61	5.34	4.10	0.79	4.88	12.5	-
And	259.03	266.56	7.53	19.08	1.01	20.09	51.3	-
Incl.	259.03	264.74	5.71	23.16	0.95	24.11	60.0	-
Incl.	259.03	261.25	2.22	36.86	0.68	37.54	71.7	-
And	307.91	320.05	12.14	0.23	0.04	0.27	66.2	0.12
Incl.	315.26	320.05	4.79	0.38	0.05	0.42	149.4	0.27
Incl.	318.00	320.05	2.05	0.09	0.04	0.12	301.0	0.52
G11-3552-24	186.26	199.20	12.94	0.15	0.04	0.19	2.1	-
Incl.	193.76	197.31	3.55	0.30	0.10	0.40	4.8	-
And	235.85	236.76	0.91	0.01	0.01	0.01	36.1	0.35
G11-3552-26	215.80	216.36	0.56	0.83	0.79	1.62	71.5	-
Incl.	215.80	215.97	0.17	2.52	2.25	4.77	190.0	-
G11-3552-28	157.95	174.81	16.86	0.02	0.58	0.59	3.1	-
Incl.	166.42	169.28	2.86	0.05	1.26	1.31	9.0	-
And	172.99	174.81	1.82	0.07	2.12	2.19	6.8	-
And	179.67	181.49	1.82	0.03	0.17	0.20	64.1	0.16
And	218.66	220.50	1.84	0.00	0.00	0.01	2.7	0.26

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.

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

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

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

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

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_005full.jpg

Calcite Body Vectors

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

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

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

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

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

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

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

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

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

Notes to Exhibit 8: (a) Pallas Green MRE is owned by Glencore (see Glencore's Resources and Reserves Report dated December 31, 2023); (b) Stonepark MRE: see the 'NI 43-101 Independent Report on the Zinc-Lead Exploration Project at Stonepark, County Limerick, Ireland', by Gordon, Kelly and van Lente, with an effective date of April 26, 2018, as found on SEDAR; and (c) the historic estimate at Denison was reported by Westland Exploration Limited in 'Report on Prospecting Licence 464' by Dermot Hughes dated May, 1988; the historic estimate at Gortdrum was reported in 'The Geology and Genesis of the Gortdrum Cu-Ag-Hg Orebody' by G.M. Steed dated 1986; and the historic estimate at Tullacondra was first reported by Munster Base Metals Ltd in 'Report on Mallow Property' by David Wilbur, dated December 1973; and later summarized in 'Cu-Ag Mineralization at Tullacondra, Mallow, Co. Cork' by Wilbur and Carter in 1986; the above three historic estimates have not been verified as current mineral resources; none of the key assumptions, parameters and methods used to prepare the historic estimates were reported and no resource categories were used; significant data compilation, re-drilling and data verification may be required by a Qualified Person before the historic estimates can be verified and upgraded to be compliant with current NI 43-101 standards; a Qualified Person has not done sufficient work to classify them as a current mineral resource and the Company is not treating the historic estimates as current mineral resources. 'Rathdowney Trend' is the south-westerly projection of the Rathdowney Trend, hosting the historic Lisheen and Galmoy mines.

Exhibit 8. Regional Map of Ballywire Discovery and Surrounding Cu-Ag Historic Occurrences

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

Qualified Person

Technical information in this news release has been approved by Professor Garth Earls, Eur Geol, P.Geo, FSEG, geological consultant at IGS (International Geoscience Services) Limited, and independent 'Qualified Person' as defined under Canadian National Instrument 43-101.

Sampling and Analytical Procedures

All core drilled at Ballywire is NQ (47.6mm) and is cut using a rock saw. Sample intervals vary between 0.42m to 1.3m with the majority of samples in the 0.79m to 0.99m range. The half-core samples are bagged, labelled and sealed at Group Elevens core store facility in Limerick, Ireland. Selected sample bags are examined by the Qualified Person. Transport is via an accredited courier service and/or by Group Eleven staff to ALS Laboratories in Loughrea Co. Galway, Ireland. Sample preparation at the ALS facility comprises fine crushing 70%

Quality Assurance/Quality Control (QA/QC) Information

Group Eleven inserts certified reference materials ("CRMs" or "Standards") as well as blank material, to its sample stream as part of its industry-standard QA/QC programme. The QC results have been reviewed by the Qualified Person, who is satisfied that all the results are within acceptable parameters. The Qualified Person has validated the sampling and chain of custody protocols used by Group Eleven.

About Group Eleven Resources

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

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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Group Eleven Closes $2.5m Private Placement

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) ("Group Eleven" or the "Company") is pleased to announce it has closed its previously announced non-brokered private placement for gross proceeds of $2,500,000 (the "Offering") through the issuance of 13,157,894 units (each, a "Unit") sold at a price of $0.19 per Unit.

Each Unit consists of one common share in the capital of the Company and one-half of one common share purchase warrant (each whole warrant, a "Warrant"). Each Warrant entitles the holder thereof to acquire one additional common share at a price of $0.28 per common share for a period of two years from the date of issuance.

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Group Eleven Announces Upsize of Private Placement to $2,500,000 from $1,500,000

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) ("Group Eleven" or the "Company") is pleased to announce that further to its news release earlier today (February 18, 2025), it is increasing the size of its non-brokered private placement (the "Offering") from up to 7,894,736 units (the "Units") to up to 13,157,894 Units at a price of $0.19 per Unit for gross proceeds of $2,500,000. All currency in this news release is denominated in Canadian dollars.

Each Unit will consist of one common share in the capital of the Company (a "Common Share") and one-half of one common share purchase warrant (each whole warrant, a "Warrant"). Each Warrant will be exercisable into one Common Share at a price of $0.28 per Warrant for a period of two years from the date of issuance.

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Group Eleven Announces $1,500,000 Non-Brokered Private Placement, Including Participation from Michael Gentile

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) ("Group Eleven" or the "Company") is pleased to announce a non-brokered private placement (the "Offering") for gross proceeds of up to $1,500,000 comprising of up to 7,894,736 units (each, a "Unit") at a price of $0.19 per Unit. All currency in this news release is denominated in Canadian dollars.

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Group Eleven Intersects 15.6m of 11.6% Zn+Pb, 122 g/t Ag and 0.19% Cu, incl. 3.5m of 21.3% Zn+Pb, 395 g/t Ag and 0.73% Cu at Ballywire; Silver and Copper Values Continue to Impress

Group Eleven Resources Corp. (TSXV: ZNG) (OTC Pink: GRLVF) (FSE: 3GE) ("Group Eleven" or the "Company") is pleased to announce results from the latest two holes of 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:

G11-3552-27 intersected (from 213.0m):
- 24.8m of 8.1% Zn+Pb (5.8% Zn and 2.3% Pb), 80 g/t Ag and 0.12% Cu, including
- 15.6m of 11.6% Zn+Pb (8.3% Zn and 3.3% Pb), 122 g/t Ag and 0.19% Cu, including
- 6.6m of 16.7% Zn+Pb (11.1% Zn and 5.7% Pb), 240 g/t Ag and 0.42% Cu, including
- 3.5m of 21.3% Zn+Pb (13.3% Zn and 8.0% Pb), 395 g/t Ag and 0.73% Cu
- Located in middle of 270m gap between two previously released drill fences
G11-3552-25 intersected (from 187.2m):
- 16.2m of 2.8% Zn+Pb (2.1% Zn and 0.7% Pb) and 8 g/t Ag, including
- 4.6m of 7.4% Zn+Pb (5.6% Zn and 1.8% Pb) and 21 g/t Ag, including
- 1.9m of 12.9% Zn+Pb (9.6% Zn and 3.3% Pb) and 39 g/t Ag
- Located 50m NNW from G11-3552-27
Above results confirm the extent of the recently announced flat-lying zone of zinc-rich massive sulphide lenses at least 360m along strike and remaining open to the NE
Massive sulphide zone is pierced by G11-3552-27 and seven previously released holes, of which three are referenced below:
- G11-3552-12: 29.6m of 10.6% Zn+Pb and 78 g/t Ag (released 11-Jun-24)
- G11-3552-18: 11.8m of 11.6% Zn+Pb and 48 g/t Ag (released 22-Oct-24)
- G11-3552-19: 15.3m of 14.5% Zn+Pb and 56 g/t Ag (released 14-Nov-24)
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

"It is great to see the NE massive sulphide zone now consistently intersected by eight high-grade holes over a strike length of 360m and open to the NE," stated Bart Jaworski, CEO. "Excellent silver and significant copper values are also noteworthy because they increasingly point to a stratigraphically deeper horizon known to be highly prospective for copper and silver in this part of Ireland. Namely, the Gortdrum Cu-Ag mine, active in the 1960s and 70s, is located 10km NE of Ballywire, whereas, the Denison and Tullacondra Cu-Ag historic occurrences are 5km SE and 45km SW of Ballywire, respectively. A deeper Cu-Ag horizon at Ballywire is one of our key targets for 2025.

Our two other key targets include: (i) exploration drilling along strike from the drilled 2.6km-long discovery area towards the encompassing 6km long prospective trend and (ii) up and down dip from the discovery trend in search of parallel zones of mineralization. We eagerly await results from drilling down dip of today's results and along the NE extension."

Exhibit 1. Cross-Section A-A' of G11-3552-25, -27 (Filling In 270m Gap Between Fences) at Ballywire

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/239839_figure1.png

Exhibit 2. Plan Map Showing Key New Drilling (G11-3552-25, -27) at Ballywire

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/239839_figure2.png

Exhibit 3. Emerging Massive Sulphide Zone and Upcoming Drill Results at Ballywire

To view an enhanced version of this graphic, please visit:
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Recent Holes from 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 42 holes drilled and reported by Group Eleven to date, the most recent two holes (G11-3552-25 to -27) are reported today (see Exhibits 1 to 6). Note, a second batch of assays totalling over 50m within G11-3552-27 is still pending.

High-grade mineralization from G11-3552-25 and -27 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 4. Summary of Assays from G11-3552-25 and -27 at Ballywire

Item	From (m)	To (m)	Int (m)	Zn (%)	Pb (%)	Zn+Pb (%)	Ag (g/t)	Cu (%)
G11-3552-25	187.15	203.35	16.20	2.14	0.69	2.83	8.00	-
Incl.	187.15	195.51	8.36	3.59	1.11	4.70	14.49	-
Incl.	190.87	195.51	4.64	5.59	1.82	7.41	20.97	-
Incl.	192.69	194.60	1.91	9.59	3.32	12.92	39.19	-
G11-3552-27	213.00	237.81	24.81	5.84	2.28	8.11	80.4	0.12
Incl.	219.42	235.06	15.64	8.30	3.28	11.59	122.1	0.19
Incl.	219.42	222.21	2.79	15.57	3.77	19.35	92.79	0.03
And	228.51	235.06	6.55	11.06	5.65	16.71	240.0	0.42
Incl.	230.36	233.90	3.54	13.26	8.01	21.27	395.1	0.73

Note: True width of the overall mineralized package in all holes above is estimated at approx. 90-100% of the intersected interval

Overall, recent drilling suggests the emergence of two distinct styles of mineralization. First, relatively flat-lying zinc-rich massive sulphide lenses and second, 'other high-grade mineralization', dominated by variably dipping massive sulphides, as well as, vein-hosted and disseminated mineralization (see Exhibits 1-3). Both styles occur at or near the base of the Waulsortian Limestone and offer great exploration opportunities as drilling progresses.

Looking forward, seven (7) drill holes (G11-3552-24, -26, -28 and 29 to -32; see Exhibit 3) are in progress with results expected in due course. Exhibit 3 shows drilling to date across 1.25km of the overall 2.6km long trend (see Exhibit 2) of significantly mineralized drill intercepts (open in all directions). 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 5).

Exhibit 5. Regional Gravity at Ballywire Showing 6km Long Prospective Trend

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Notes to Exhibit 6: (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.

Exhibit 6. Regional Map of PG West (100% Interest) and Stonepark (77.64% Interest)

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Note: Two westernmost prospecting licenses were surrendered in December 2024 from the Stonepark Project, reflecting decreasing prospectivity and the Company's preference to focus on core prospects (Ballywire and Carrickittle West)

Consultant

The Company has engaged ProConsul Capital Ltd. ("ProConsul") to provide investment marketing consulting services (the "Services") commencing February 6th, 2025. In consideration for the Services, the Company will pay a fee of C$6,000/month and has agreed to grant stock options to ProConsul, the number and terms of which stock options will be determined at a later date. The agreement is subject to TSX Venture Exchange acceptance and renewable on a month-to-month basis unless terminated by either party on 30 days written notice.

Qualified Person

Quality Assurance/Quality Control (QA/QC) Information

About Group Eleven Resources

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 deposit¹, which itself is located adjacent to Glencore's Pallas Green zinc-lead deposit². The Company's two largest shareholders are Glencore Canada Corp. (17.1% interest) and Michael Gentile (16.5%). 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

Cautionary Note Regarding Forward-Looking Information

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Hole ID	X	Y	Z	Azi	Dip	Depth (m)	From (m)	To (m)	Interval (m)	Au (g/t)	Cu (%)	AuEq (g/t)
LDR-25-05	549448	5525296	375	227	-45	214.2	131.7	135.0	3.3	6.6	0.0	6.6
						Including	131.7	134	2.3	9.1	0.0	9.1
LDR-25-06	549560	5525483	375	215	-51	474.0	Pending Assays
LDR-25-07	549453	5525313	375	215	-55	261.0
LDR-25-08	549524	5525441	375	246	-57	516.0
LDR-25-09	549445	5525319	375	238	-54	252.0
LDR-25-10	549489	5525229	375	220	-60	237.0

Hole ID	From	To	Interval	Mineral 1	%	Mineral 2	%	Mineral 3	%	Visible Gold		Total Sulphide (%)
LDR-25-08	89.0	90.0	1.0	Pyrite	2.0					-		2.0
LDR-25-08	166.4	211.1	44.7	Pyrite	0.5					-		0.5
LDR-25-08	211.1	216.0	4.9	Pyrite	0.1					-		0.1
LDR-25-08	216.0	216.6	0.6	Pyrite	1.0					-		1.0
LDR-25-08	216.6	354.8	138.2	Pyrite	0.1					-		0.1
LDR-25-08	360.4	361.3	0.9	Chalcopyrite	0.5	Pyrite	1.0			-		1.5
LDR-25-08	363.9	392.1	28.2	Chalcopyrite	0.3	Pyrite	0.5			-		0.8
LDR-25-08	392.1	397.3	5.3	Pyrite	0.3					-		0.3
LDR-25-08	397.3	405.6	8.3	Chalcopyrite	0.1					-		0.1
LDR-25-08	405.6	406.1	0.5	Chalcopyrite	0.3	Pyrite	30.0			-		30.3
LDR-25-08	406.1	407.9	1.8	Chalcopyrite	0.5	Pyrite	1.5			-		2.0
LDR-25-08	407.9	408.3	0.4	Pyrite	7.0	Chalcopyrite	0.1			-		7.1
LDR-25-08	408.3	409.0	0.7	Pyrite	0.1					-		0.1
LDR-25-08	409.0	409.4	0.4	Pyrite	25.0	Chalcopyrite	25.0			-		50.0
LDR-25-08	409.4	411.7	2.3	Chalcopyrite	3.0	Pyrite	7.0			-		10.0
LDR-25-08	411.7	411.9	0.2	Sphalerite	2.0	Chalcopyrite	0.5	Pyrite	15.0	-		17.5
LDR-25-08	411.9	415.1	3.2	Chalcopyrite	1.0	Pyrite	3.0			-		4.0
LDR-25-08	415.1	420.8	5.8	Chalcopyrite	0.3	Pyrite	1.0			-		1.3
LDR-25-08	420.8	423.3	2.4	Chalcopyrite	1.5	Pyrite	2.5			-		4.0
LDR-25-08	423.3	428.3	5.1	Chalcopyrite	0.1	Pyrite	0.1			-		0.2
LDR-25-08	428.3	455.0	26.7	Pyrite	0.5					-		0.5
LDR-25-08	457.6	458.1	0.4	Sphalerite	0.1	Chalcopyrite	1.0	Pyrite	0.5	-		1.6
LDR-25-08	461.2	461.8	0.6	Chalcopyrite	2.0					-		2.0
LDR-25-08	463.8	464.6	0.9	Chalcopyrite	5.0	Pyrite	2.0			0.1	%	7.1
LDR-25-08	464.6	478.6	14.0	Chalcopyrite	1.0	Pyrite	0.5			-		1.5
LDR-25-08	478.6	479.7	1.1	Chalcopyrite	3.0	Pyrite	8.0			-		11.0
LDR-25-08	480.6	516.0	35.4	Chalcopyrite	0.2	Pyrite	0.1			-		0.3

Criteria	JORC Code explanation	Commentary
Sampling techniques	Nature and quality of sampling (eg cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling.	All drilling conducted by Cygnus Metals at the Chibougamau Project was completed under the supervision of a registered professional geologist as a Qualified Person (QP) who is responsible and accountable for the planning, execution, and supervision of all exploration activity as well as the implementation of quality assurance programs and reporting. All Cygnus drilling reported is NQ size (47.8 mm diameter).
	Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.	All sample collection, core logging, and specific gravity determinations were completed by Cygnus Metals under the supervision of a professionally qualified registered geologist. NQ core was marked for splitting during logging and is sawn using a diamond core saw with a mounted jig to assure the core is cut lengthwise into equal halves. Half of the cut core is placed in clean individual plastic bags with the appropriate sample tag. QA/QC is done in house by Cygnus Metals geologists with oversight from the Senior Geologist. The check samples (blanks and standards – 4% of total samples with another 2% of core duplicates taken on half split core) that were inserted into the sample batches are verified against their certified values and are deemed a pass if they are within 3 standard deviations of the certified value. The duplicates are evaluated against each other to determine mineralization distribution (nugget). If there are large discrepancies in the check samples, then the entire batch is requested to be re-assayed. The samples are then placed in bags for shipment to the offsite laboratory's facility. The remaining half of the core is retained and incorporated into Cygnus's secure, core library located on the property.
	Aspects of the determination of mineralisation that are Material to the Public Report. In cases where ‘industry standard' work has been done this would be relatively simple (eg ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay'). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (eg submarine nodules) may warrant disclosure of detailed information.	Industry standard sampling practices were used with sample lengths ranging from 0.3 m to 1.0 m and respected geological contacts. Sample tags were placed at the beginning of each sample interval and the tag numbers were recorded in an MS Excel database. Sampling practice is considered to be appropriate to the geology and style of mineralisation.
Drilling techniques	Drill type (eg core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what method, etc).	Diamond core was drilled using surface diamond rigs with industry recognised contractors Miikan Drilling. Miikan is a joint venture between Chibougamau Diamond Drilling Ltd., the First Nations community of Ouje-Bougoumou and the First Nations community of Mistissini both located in the Eeyou Istchee territory. Drilling was conducted using NQ core size. Directional surveys have been taken at 50m intervals.
Drill sample recovery	Method of recording and assessing core and chip sample recoveries and results assessed. Measures taken to maximise sample recovery and ensure representative nature of the samples. Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material.	Diamond core recovery was measured for each run and calculated as a percentage of the drilled interval. Overall, the core recoveries are excellent in the Chibougamau area. As a result, no bias exists.
Logging	Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies.	All core was geologically and geotechnically logged. Lithology, veining, alteration and mineralisation are recorded in multiple tables of the drillhole database.
	Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography.	Geological logging of core is qualitative and descriptive in nature.
	The total length and percentage of the relevant intersections logged.	100% of the core has been logged.
Sub-sampling techniques and sample preparation	If core, whether cut or sawn and whether quarter, half or all core taken. If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. For all sample types, the nature, quality and appropriateness of the sample preparation technique. Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples. Measures taken to ensure that the sampling is representative of the in-situ material collected, including for instance results for field duplicate/second-half sampling. Whether sample sizes are appropriate to the grain size of the material being sampled.	The NQ diameter the core was sawn in half following a sample cutting line determined by geologists during logging and submitted for analysis on nominal 1m intervals or defined by geological boundaries determined by the logging geologist. Each core sample is assigned a tag with a unique identifying number. Sample lengths are typically one metre but can be depending on zone mineralogy and boundaries. This sampling technique is industry standard and deemed appropriate. Samples sizes are considered appropriate to grain size of the materials being sampled.
Quality of assay data and laboratory tests	The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total.	Sample (NQ size half core) preparation and fire assay analysis were done at Bureau Veritas Commodities Canada Ltd ("BV") in Timmins, Ontario, and ICP-ES multi-elements analysis was done at BV in Vancouver, B.C. Samples were weighed, dried, crushed to 70% passing 2 mm, split to 250 g, and pulverized to 85% passing 75 µm. Samples are fire assayed for gold (Au) (30 g) and multi-acid digestion ICP-ES finish, for 23 elements (including key elements Ag, Cu, Mo). Samples assaying >10.0 g/t Au are re-analysed with a gravimetric finish using a 30 g charge. Samples assaying >10% Cu are re-analysed with a sodium peroxide fusion with ICP-ES analysis using a 0.25 g charge.
	For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.	None used.
	Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.	At Bureau Veritas, laboratory QC procedures involve the use of internal certified reference material as assay standards, along with blanks, duplicates and replicates.
Verification of sampling and assaying	The verification of significant intersections by either independent or alternative company personnel.	Verification of sampling was made by Cygnus Metals and other professional consultant geologists.
	The use of twinned holes.	No hole is twinned.
	Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols.	All logging data was completed, core marked up, logging and sampling data was entered directly into the database. The logged data is stored on the site server directly.
	Discuss any adjustment to assay data.	There was no adjustment to the assay data.
Location of data points	Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.	The location of the drillholes and the aiming points for the orientation of the drillholes were indicated on the ground using identified stakes. The stakes marking the location of the drillholes were set up and located with a Garmin GPS model "GPSmap 62s" (4m accuracy). Surveys are collected using a Reflex EZ-Shot® single-shot electronic instrument with readings collected at intervals of approximately every 30 m downhole plus a reading at the bottom of the hole.
	Specification of the grid system used.	The grid system used is UTM NAD83 (Zone 18).
	Quality and adequacy of topographic control.	A Digital Terrane Model (DTM) has been used to accurately plot the vertical position of the holes, which is considered to provide an adequate level of topographic control.
Data spacing and distribution	Data spacing for reporting of Exploration Results.	The drill spacing for recent drilling is considered appropriate for this type of exploration. Due to the historic nature and mix of underground and surface drilling the drill hole spacing for historic drill results is highly variable.
	Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied.	No resource estimation is made.
	Whether sample compositing has been applied.	No sample compositing has been applied.
Orientation of data in relation to geological structure	Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type.	Recent drilling is orientated approximately at right angles to the currently interpreted strike of the known interpreted mineralisation. Due to the historic nature of the drilling the drill hole orientation for historic drill results is highly variable.
Orientation of data in relation to geological structure	If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.	No bias is considered to have been introduced by the existing sampling orientation.
Sample security	The measures taken to ensure sample security.	Core was placed in wooden core boxes close to the drill rig by the drilling contractor. The core was collected daily by the drilling contractor and delivered to the secure core logging facility. Access to the core logging facility is limited to Cygnus employees or designates.
Audits or reviews	The results of any audits or reviews of sampling techniques and data.	No audits or reviews of sampling techniques or data have been undertaken, therefore information on audits or reviews is not yet available.

Criteria	JORC Code Explanation	Commentary
Mineral tenement and land tenure status	Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings.	The data reported within this announcement is from the Chibougamau Project. The Chibougamau project consists of 3 properties which include: Copper Rand, 14,383 ha (15 mining concession and 311 exploration claims) Corner Bay – Devlin (1 mining license, 141 exploration claims owned 100% by CBAY and 17 claims owned 56.4% by CBAY/43.6% Pan American Silver) Joe Mann (2 mining concessions, 82 claims owned 100% by CBAY, and 68 claims and 1 mining concession owned 65% by CBAY/35% by SOQUEM) CBAY Minerals Inc. ("CBAY"), a wholly owned subsidiary of Cygnus, is the owner of all claims and leases, except where otherwise noted above. The properties collectively making up the Project are in good standing based on the Ministry of Energy and Natural Resources (Ministère de l'Énergie et des Ressources Naturelles) GESTIM claim management system of the Government of Québec.
Mineral tenement and land tenure status	The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area.	All tenure is in good standing.
Exploration done by other parties	Acknowledgment and appraisal of exploration by other parties.	The Chibougamau Copper and Gold project comprising Corner Bay, Devlin, Cedar Bay and Joe Mann has seen an extensive exploration history dating back to the early 1900s. The Preliminary Economic Assessment (as referred to in the Company's announcement of 15 October 2024) provides a detailed history of the exploration activities undertaken by previous explorers. Corner Bay was first identified as a prospect in 1956 1956 – 1972 eight drilling programs totalling 1,463 m and various geophysical and electromagnetic (EM) surveys 1973 – 1981 Riocanex and Flanagan McAdam: ground geophysical surveys and 43 diamond drill holes 1982 – 1984 Riocanex and Corner Bay Exploration: 38 drill holes and metallurgical test work 1988 – 1991 Corner Bay Exploration: diamond drilling, geophysical surveys and geological characterisation with initial MRE 1992 – 1994 SOQUEM optioned and acquired a 30% interest, and completed diamond drilling 1994 Explorations Cache Inc and Resources MSV Inc: diamond drilling 2004 – 2006 GéoNova and MSV: 98 diamond drill holes and first Technical Report on the Corner Bay project reporting a MRE 2007 – 2009 Campbell: diamond drilling and bulk sample 2012 - 2019 CBAY / AmAuCu: diamond drilling and MRE Devlin identified in 1972 by airborne survey flown by the MERN 1979 – 1981 diamond drilling, geophysical surveys 1981 development commenced Joe Mann identified in 1950 with the commencement of mining activities occurring in 1956 The Joe Mann mine operated underground during three different periods from 1956 to 2007 In July 2012, Resources Jessie acquired the Joe Mann mine property, but conducted only surface exploration work Cedar Bay was discovered prior to 1927 by Chibougamau McKenzie Mines Ltd From initial discovery to 2013 various surface and underground drilling campaigns and geophysical surveys undertaken by various companies Colline was first discovered with mapping and sampling and then drilled in the 1950s with follow up drilling in 1955. In the 1950s a shaft was sunk but the deposit was never mined. The deposit was later tested with three drill holes and six regional drill holes throughout two drilling campaigns in 1984 and 1986/87. Exploration at Colline has been halted historically with the discovery of and focus on other deposits in the region. Golden Eye (previously known as Dore Ramp) was drilled in a few different phases from 1984 to 1992. A total of 47 drill holes from surface are reported during that period A double ramp of approximately 1 kilometre was excavated in 1991-92 to a vertical depth of 160 meters Underground drilling campaign of 46 holes totaling 10,200 meters tested the deposit mainly to a depth of 240 meters (only five holes tested the deposit between 300 and 600 meters)
Geology	Deposit type, geological setting and style of mineralisation.	Corner Bay and Devlin are located at the northeastern extremity of the Abitibi subprovince in the Superior province of the Canadian Shield and are examples of Chibougamau-type copper-gold deposits. The Abitibi subprovince is considered as one of the largest and best-preserved greenstone belts in the world and hosts numerous gold and base metal deposits. The Corner Bay deposit is located on the southern flank of the Doré Lake Complex (DLC). It is hosted by a N 15° trending shear zone more or less continuous with a strong 75° to 85° dip towards the west. The host anorthosite rock is sheared and sericitized over widths of 2 m to 25 m. The deposit is cut by a diabase dyke and is limited to the north by a fault structure and to the south by the LaChib deformation zone. The Corner Bay deposit consists of three main mineralized lodes (subparallel Main Lode 1 and Main Lode 2 above the dyke, and Main Lode below the dyke that make up the bulk of the deposit. The Corner Bay deposit has been traced over a strike length to over 1,100 m to a depth of 1,350 m and remains open at depth. The mineralization is characterized by veins and/or lenses of massive to semi-massive sulphides associated with a brecciated to locally massive quartz-calcite material. The sulphide assemblage is composed of chalcopyrite, pyrite, and pyrrhotite with lesser amounts of molybdenite and sphalerite. Late remobilized quartz-chalcopyrite-pyrite veins occur in a wide halo around the main mineralization zones. Devlin is a flat-lying, copper-rich lodes-hosted deposit in a polygenic igneous breccia that is less than 100 m from the surface. The tabular bodies have been modelled as four nearly horizontal lodes: a more continuous lower zone and three smaller lodes comprising the upper zone. Mineralization is reflected as a fracture zone often composed of two or more sulphide-quartz lodes and stringers. Thickness of the mineralized zones range from 0.5 m to 4.4 m. It has been diluted during modelling to reflect a minimum mining height of 1.8 m. The Joe Mann deposit is characterized by east-west striking shear hosted lodes that extend beyond 1,000 m vertically with mineralization identified over a 3 km strike length. These shear zones form part of the Opawica-Guercheville deformation zone, a major deformation corridor cutting the mafic volcanic rocks of the Obatogamau Formation in the north part of the Caopatina Segment. The gabbro sill hosts the Main Zone and the West Zone at the mine, while the South Zone is found in the rhyolite. These three subvertical E-W (N275°/85°) ductile-brittle shear zones are sub-parallel to stratigraphy and to one another, with up to 140 m to 170 m of separation between them. These shear zones are hosted within a stratigraphic package composed of iron-magnesium (Fe-Mg) carbonate and sericite altered gabbro sills, sheared basalts, and intermediate to felsic tuffs intruded by various felsic intrusions. The Joe Mann gold mineralization is hosted by decimetre scale quartz-carbonate lodes (Dion and Guha 1988). The lodes are mineralized with pyrite, pyrrhotite, and chalcopyrite disposed in lens and lodelets parallel to schistosity, and occasionally visible gold. There are some other minor, mineralized structures, e.g., North and South-South Zones, with limited vertical and horizontal extensions.
Drill hole Information	A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: easting and northing of the drill hole collar elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar dip and azimuth of the hole down hole length and interception depth hole length. If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.	All requisite drillhole information is tabulated elsewhere in this release. Refer Appendices A and B of the body text.
Data aggregation methods	In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut-off grades are usually Material and should be stated.	For recent results, drill hole intersections are reported above a lower cut-off grade of 2g/t AuEq over widths of greater than 1m.
	Where aggregate intercepts incorporate short lengths of high-grade results and longer lengths of low-grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail.	A maximum of 1m internal waste was allowed.
	The assumptions used for any reporting of metal equivalent values should be clearly stated.	Individual grades for the metals included in the metal equivalents calculation for the exploration results are in Appendices A, B and C of this release. Metal equivalents for exploration results have been calculated at a copper price of US$8,750/t, gold price of US$2,350/oz and silver price of US$25/oz. Copper equivalents are calculated based on the formula CuEq(%) = Cu(%) + (Au(g/t) x 0.77258)+(Ag(g/t) x 0.00822). Gold equivalents are calculated based on the formula AuEq(g/t) = Au(g/t) +(Cu(%) x 1.29436)+(Ag(g/t) x 0.01064). Metallurgical recovery factors have been applied to the metal equivalents calculations, with copper metallurgical recovery assumed at 95% and precious metal (gold and silver) metallurgical recovery assumed at 85% based upon historical production at the Chibougamau Processing Facility, and the metallurgical results contained in Cygnus' announcement dated 28 January 2025. It is the Company's view that all elements in the metal equivalent calculations have a reasonable potential to be recovered and sold.
Relationship between mineralisation widths and intercept lengths	These relationships are particularly important in the reporting of Exploration Results. If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (eg ‘down hole length, true width not known').	All intersections reported in the body of this release are down hole. For recent drill holes, holes are drilled as close to orthogonal to the plane of the mineralized lodes as possible. True width is estimated to be about 80% of the downhole drill intersection
Diagrams	Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include,but not be limited to a plan view of drill hole collar locations and appropriate sectional views.	Refer Figure 1 (Long Section of Golden Eye) and 2 (Long Section through the Chibougamau North Camp illustrating Golden Eye) in the body of the announcement. Plan view of recent drilling relative to historic drilling and the 1992 ramp access (see Figure 3 below).
Balanced reporting	Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.	Recent infill drilling at Golden Eye totals 6 holes for 1,954m, with assay results for 1 drill hole received to date. All results greater than 2g/t AuEq over greater than 1m width have been reported.
Other substantive exploration data	Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances.	There is no other substantive exploration data.
Further work	The nature and scale of planned further work (eg tests for lateral extensions or depth extensions or large-scale step-out drilling). Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive.	The Company plans to conduct drill testing of additional mineralisation as well as step out drilling of existing lodes to further enhance the resources quoted in this release. More information is presented in the body of this report. Diagrams in the main body of this release show areas of possible resource extension on existing lodes. The Company continues to identify and assess multiple other target areas within the property boundary for additional resources.

Lumina Gold Corp.
	:
Signed: *"Marshall Koval"*

Marshall Koval, President & CEO, Director

Deposit	Category	Tonnes (k)	Cu Grade (%)	Au Grade (g/t)	Cu Metal (kt)	Au Metal (koz)	CuEq Grade (%)
Corner Bay (2022)	Indicated	2,700	2.7	0.3	71	22	2.9
Corner Bay (2022)	Inferred	5,900	3.4	0.3	201	51	3.6
Devlin (2022)	Measured	120	2.7	0.3	3	1	2.9
	Indicated	660	2.1	0.2	14	4	2.3
	Measured & Indicated	780	2.2	0.2	17	5	2.4
	Inferred	480	1.8	0.2	9	3	2.0
Joe Mann (2022)	Inferred	610	0.2	6.8	1	133	5.5
Cedar Bay (2018)	Indicated	130	1.6	9.4	2	39	8.9
Cedar Bay (2018)	Inferred	230	2.1	8.3	5	61	8.5
Total	Measured & Indicated	3,600	2.5	0.6	90	66	3.0
Total	Inferred	7,200	3.0	1.1	216	248	3.8

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