Tinka Drills 98 Metres at 8.8% Zinc Including 36 Metres at 19.0% Zinc at Ayawilca and Provides Exploration Update

Tinka Resources Limited ("Tinka" or the "Company") (TSXV:TK)(BVL:TK)(OTCQB:TKRFF) is pleased to announce results for five recent drill holes from the Ayawilca Project and to provide an update on the Company's exploration activities. All five drill holes were resource confirmation holes from West Ayawilca, and all intersected strong zinc mineralization. The Company has now successfully completed its 11,000-metre drill program at Ayawilca which commenced midway through 2022. Two drill rigs were demobilized during May 2023 and independent mining consultants have now been engaged to complete an updated mineral resource estimate

The 2022-23 drill program has significantly improved the geological model of the mineralized zinc bodies at West and South Ayawilca and improved the confidence in the continuity of mineralization. One exploration hole at South Ayawilca has results pending. The next steps for the project include an updated resource estimate to be announced during Q3 2023 and the continuation of low impact exploration.

Key Highlights - Drill hole results from West Ayawilca:

Hole A23-216

  • 97.9 metres at 8.8% zinc and 16 g/t silver from 197.90 metres depth, including
    • 35.8 metres at 19.0% zinc and 35 g/t silver from 260.0 metres depth, including
      • 13.5 metres at 25.3% zinc and 44 g/t silver from 265.5 metres depth.

Hole A23-217

  • 71.9 metres at 5.5% zinc and 8 g/t silver from 186.1 metres depth, including
    • 45.8 metres at 6.4% zinc and 10 g/t silver from 210.4 metres depth, including
      • 4.85 metres at 15.2% zinc and 23 g/t silver from 210.4 metres depth.

Hole A23-213

  • 30.4 metres at 6.0% zinc from 180.0 metres depth, including
    • 1.2 metres at 37.2% zinc from 207.3 metres depth, and
  • 30.5 metres at 5.1% zinc from 260.0 metres depth.

Hole A22-211

  • 38.15 metres at 6.3% zinc, 1.1% lead and 28 g/t silver from 151.0 metres depth, including
    • 6.6 metres at 9.2% zinc, 5.2% lead and 81 g/t silver from 182.55 metres depth.

Hole A22-214

  • 13.1 metres at 3.7% zinc from 243.9 metres depth

True thicknesses of these intercepts are estimated to be at least 75% of the downhole thicknesses.

Dr. Graham Carman, Tinka's President and CEO, stated: "The 2022-23 drill program has been one of the most successful drill programs since Tinka began exploring at Ayawilca. The latest results highlight the quality of the zinc mineralization at Ayawilca in terms of both grade and thickness and provide strong confidence in the geological resource."

"We have confirmed at West Ayawilca that two pipe-like sulphide bodies hosted by brecciated limestones extend through the 100-200-metre-thick limestones and are connected by massive sulphides at the base. At South Ayawilca, very high-grade massive sulphide zinc mineralization is concentrated in a folded limestone at shallower depth - this discovery has the potential to be a ‘starter mine' which could provide early payback."

"Our contention that Ayawilca is one of the best zinc exploration and development projects in the Americas has been reinforced by the recent drill program. I wish to thank our staff, our stakeholders at the project and our drilling contractor for their hard work which has enabled this drill program to be successfully completed. We now look forward to the mineral resource update for the Ayawilca Zinc Zone and Tin Zone deposits, which will be released during Q3 2023. In the meantime, low impact exploration is continuing at Ayawilca and at our nearby Silvia copper-gold project."

Discussion - Geology of the Zinc Zone Deposits at Ayawilca

A total of 11,115 metres were drilled in 33 holes at Ayawilca during the 2022-23 drill program (see Figure 1). Around 90% of the drill holes were focused at West and South Ayawilca for resource confirmation and definition purposes. Two holes were also drilled at Central Ayawilca for the dual purposes of exploration and a hydrological study.

The 2022-23 drill program has considerably improved our understanding of the geology of the Ayawilca Zinc Zone and improved the confidence in the geometry of the mineralized bodies at West and South. Two of the most important conclusions from the drilling include:

  1. At West Ayawilca, two pipe-like zinc sulphide bodies hosted by brecciated limestones extend through the 100- to 200-metre-thick limestone sequence along a northwest-southeast trend and are connected by massive sulphide mineralization at the base of the limestone;
  2. At South Ayawilca, very high-grade massive sulphide zinc mineralization is concentrated within a tightly folded limestone at relatively shallow depth - this discovery has the potential to be a ‘starter mine' which could provide early payback of capital.

West Ayawilca
The footprint of the zinc mineralization hosted by limestones at West Ayawilca covers an area of approximately 700 metres by 300 metres projected to surface (see Figure 1). Drilling in 2022-23 focused on defining the geometry of two pipe-like breccia bodies which host continuous, semi-massive sulphide (SMS) mineralization within the limestone. The breccia bodies have surface dimensions of between 100 to 200 metres and are elongated along a northwest-southeast direction. Zinc mineralization extends over a vertical thickness of between 100 to 150 metres through the entire brecciated limestone sequence up to the overlying sandstones. The breccia bodies are connected by massive sulphide (MS) zinc mineralization at the base of the limestone.

Zinc sulphide (as sphalerite) is the dominant economic mineralization. Silver and lead (as silver sulphosalts and galena) is typically more common around the edges of the zinc bodies and in carbonate-rich veins. Iron sulphides are common including pyrite, marcasite, and pyrrhotite. Carbonate (siderite, an Fe-rich variety) is the dominant gangue mineral.

The new interpretation of the geology at West Ayawilca is the result of a redesigned drill program in 2022-23 which targeted the northwest-southeast trend rather than the late-stage east-west trending veins which outcrop. All 13 holes at West Ayawilca in the 2022-23 program were drilled on an east-west orientation (mostly angled to the west) in contrast to previous holes which were mostly orientated north-south. The improvement in vertical continuity of the mineralization is positive for the project, as it will likely lead to more cost-effective mining with less dilution.

The brecciation of the limestones is interpreted to have occurred as result of karst dissolution and collapse of the limestones, possibly during the early stages of hydrothermal activity. The mineralization is focused within the hinge of a major anticline fold immediately adjacent to the Colquipucro Fault (see cross sections, Figure 2). A longitudinal section showing the geometry of the zinc mineralization along the northwest-southeast trend is shown in Figure 3.

Photographs of the typical massive sulphide zinc mineralization and the semi-massive sulphide breccia mineralization at West Ayawilca is shown in Figure 4.

South Ayawilca
The highest-grade area of zinc mineralization at the project is located at South Ayawilca. Massive sulphide (MS) mineralization has been identified over an area (projected to surface) of approximately 400 metres by 200 metres elongated in a northeast-southwest direction (see Figures 1 and 3). Very high-grade massive sulphide zinc mineralization is focused in the hinge zone of an anticline fold structure. Drill results including cross sections from South Ayawilca can be reviewed in the following disclosures - see news release January 9th 2023; and news release March 6th 2023.

Update on Exploration Activities at Ayawilca

Tinka's geologists have recently sampled manganese-altered outcrops at Ayawilca which are interpreted to be surface expressions of the Silver Zone discovery (see news release May 2nd 2023). The results of this sampling, together with the final drill hole at South Ayawilca, will be announced as soon as assays become available and interpreted.

Other news: Tinka recently received approval for the extension of the environmental permit (EIAsd) at Ayawilca for a period of three more years until May 2026. The modified and extended EIAsd has combined the two previous individual permits at Ayawilca and Colquipucro into one large permit which also incorporates several undrilled exploration targets as well as potential future mine components. The successful approval of the EIAsd is an important milestone for the project, as it will allow the Company to continue with its exploration and development plans into the medium term.

Table 1. Summary of drill hole results in this release

Hole

From (m)

To (m)

Interval (m)

Zn %

Pb %

Ag g/t

In ppm

Sn %

Cu %

Area

A22-211

151.00

189.15

38.15

6.32

1.13

28

9

West

incl

182.55

189.15

6.60

9.21

5.20

81

0

0.44

0.23

A23-213

157.50

159.50

2.00

10.87

0.36

33

7

West

and

180.00

210.40

30.40

6.00

0.03

8

26

incl

207.30

208.50

1.20

37.17

0.07

31

235

and

260.00

290.50

30.50

5.06

0.02

9

142

A23-214

243.90

256.95

13.05

3.71

0.06

11

1

West

A23-216

197.90

295.80

97.90

8.84

0.03

16

145

West

incl

260.00

295.80

35.80

19.00

0.03

35

387

0.19

0.11

incl

265.50

279.00

13.50

25.28

0.04

44

567

0.20

0.15

A23-217

186.10

258.00

71.90

5.52

0.04

8

129

West

incl

210.40

256.20

45.80

6.43

0.04

10

180

incl

210.40

215.25

4.85

15.20

0.10

23

344

A23-219*

212.70

219.00

6.30

6.05

0.33

9

91

Central

and

297.40

304.00

6.60

-

-

-

-

1.00

0.05

* Hole A23-219 at Central Ayawilca was primarily a hydrological hole drilled for the purposes of understanding the underground aquifer. This hole intersected minor zinc and tin mineralization, which will be incorporated into the updated resource estimate.

Note on sampling and assaying

Drill holes are diamond HQ size core holes with recoveries generally above 80% and often close to 100%. The drill core is marked up, logged, and photographed on site. The cores are cut in half at the Company's core storage facility, with half-cores stored as a future reference. Half-core was bagged on average over 1 to 2 metre composite intervals and sent to SGS laboratory in Lima for assay in batches. Standards and blanks were inserted by Tinka into each batch prior to departure from the core storage facilities. At the laboratory samples are dried, crushed to 100% passing 2mm, then 500 grams pulverized for multi-element analysis by ICPMS using multi-acid digestion. Samples assaying over 1% zinc, lead, or copper and over 100 g/t silver were re-assayed using precise ore-grade AAS techniques. Samples within massive sulphide zones were also assayed for tin using fusion and AAS finish.

Figure 1. Drill hole map of 2022-2023 holes at Ayawilca highlighting large zinc sulphide bodies (pink shade)

Tinka Resources Ltd., Wednesday, June 7, 2023, Press release picture

Figure 2. Cross sections through West Ayawilca highlighting Zinc Zone mineralization hosted by Pucara limestone

Tinka Resources Ltd., Wednesday, June 7, 2023, Press release picture

Tinka Resources Ltd., Wednesday, June 7, 2023, Press release picture

Figure 3. Longitudinal north - south section of West and South Ayawilca highlighting 2022-23 drill results in red.

Tinka Resources Ltd., Wednesday, June 7, 2023, Press release picture

Figure 4. Photographs of zinc mineralization in hole A23-216:

  1. Massive sulphide mineralization at the base of the limestone (sp = sphalerite, py = pyrite)
  2. Breccia hosted semi-massive sulphide mineralization (cl = clay and carbonate alteration)

Tinka Resources Ltd., Thursday, June 8, 2023, Press release picture

Table 2. Drill hole details for 2022-2023 drill program including drill collar coordinate information

Drill holeEastingNorthingElevationAzimuthDipDepth mAreaComment
A22-190

333281

8845755

4167

180

-50

498.95

CentralResults reported
A22-191

333169

8845799

4182

180

-55

478.80

CentralResults reported
A22-192

333345

8845195

4208

232

-74

385.90

SouthResults reported
A22-193

332766

8845659

4237

68

-65

365.40

WestResults reported
A22-194

333143

8845231

4226

135

-73

380.20

SouthResults reported
A22-195

333149

8845353

4221

148

-65

426.90

SouthResults reported
A22-196

333035

8845307

4235

174

-45

382.10

SouthResults reported
A22-197

332912

8845693

4220

264

-55

412.60

WestResults reported
A22-198

332900

8845768

4222

265

-53

451.10

WestResults reported
A22-199

333046

8845067

4195

303

-66

344.10

SouthResults reported
A22-200

332821

8845889

4246

260

-58

352.00

WestResults reported
A22-201

333342

8845195

4208

310

-73

58.90

South (deepening of A17-066)Results reported
A22-202

333046

8845066

4197

283

-52

270.15

SouthResults reported
A22-203

332839

8845685

4228

264

-60

350.00

WestResults reported
A22-204

333090

8845061

4196

307

-60

334.30

SouthResults reported
A22-205

332839

8845685

4227

244

-72

352.70

WestResults reported
A22-206

333044

8845064

4197

270

-58

217.30

SouthResults reported
A22-207

332710

8845883

4252

254

-74

332.00

WestResults reported
A22-208

333044

8845064

4197

270

-70

282.55

SouthResults reported
A22-209

332738

8845927

4251

257

-68

314.15

WestResults reported
A22-210

333047

8845065

4197

297

-48

259.80

SouthResults reported
A22-211

332785

8845707

4236

260

-75

295.00

WestResults here
A23-212

333047

8845065

4197

228

-79

324.30

SouthResults reported
A23-213

332853

8845650

4225

258

-65

316.00

WestResults here
A23-214

332710

8845883

4252

255

-67

287.10

WestResults here
A23-215

333047

8845065

4197

180

-80

295.10

SouthResults reported
A23-216

332710

8845883

4252

220

-73

310.00

WestResults here
A23-217

332853

8845650

4225

240

-78

300.00

WestResults here
A23-218

333109

8845020

4190

330

-75

323.70

SouthResults reported
A23-219

333219

8845582

4182

180

-85

336.80

CentralResults here
A23-220

333047

8845065

4197

308

-62

328.10

SouthResults reported
A23-221

333118

8845102

4207

332

-69

400.60

SouthResults reported
A23-223

333118

8845102

4207

335

-62

348.40

SouthResults pending
TOTAL

11,115.00

Notes: Datum for coordinates is WGS84 Zone 18S. Azimuth is true azimuth

The Qualified Person, Dr. Graham Carman, Tinka's President and CEO, and a Fellow of the Australasian Institute of Mining and Metallurgy, has reviewed and verified the technical contents of this release.

Readers are encouraged to read the NI 43-101 Technical Report entitled "Ayawilca Polymetallic Project, Central Peru, NI 43-101 Technical Report on Updated Preliminary Economic Assessment" available for download on Tinka's website at www.tinkaresources.com. The Technical Report was prepared by Mining Plus Peru S.A.C. ("Mining Plus") as principal consultant, Transmin Metallurgical Consultants ("Transmin"), Envis E.I.R.L ("Envis"), and SLR Consulting (Canada) Ltd ("SLR").

On behalf of the Board,

"Graham Carman"
Dr. Graham Carman, President & CEO

Further Information:
www.tinkaresources.com

Mariana Bermudez 1.604.685.9316
info@tinkaresources.com

Stay up to date by subscribing for news alerts at Contact Tinka and by following Tinka on Twitter, LinkedIn and Facebook.

About Tinka Resources Limited

Tinka is an exploration and development company with its flagship property being the 100%-owned Ayawilca zinc-silver-tin project in central Peru. The Zinc Zone deposit has an estimated Indicated Mineral Resource of 19.0 Mt @ 7.15% Zn, 16.8 g/t Ag & 0.2% Pb and Inferred Mineral Resource of 47.9 Mt @ 5.4% Zn, 20.0 g/t Ag & 0.4% Pb (dated August 30, 2021). The Ayawilca Tin Zone has an estimated Inferred Mineral Resource of 8.4 Mt grading 1.0% Sn. Tinka is recently completed an 11,000-metre resource definition drill program at West Ayawilca and South Ayawilca.

Forward Looking Statements: Certain information in this news release contains forward-looking statements and forward-looking information within the meaning of applicable securities laws (collectively "forward-looking statements"). All statements, other than statements of historical fact are forward-looking statements. Forward-looking statements are based on the beliefs and expectations of Tinka as well as assumptions made by and information currently available to Tinka's management. Such statements reflect the current risks, uncertainties and assumptions related to certain factors including, without limitations: timing of planned work programs and results varying from expectations; delay in obtaining results; changes in equity markets; uncertainties relating to the availability and costs of financing needed in the future; equipment failure, unexpected geological conditions; imprecision in resource estimates or metal recoveries; success of future development initiatives; competition and operating performance; environmental and safety risks; the Company's expectations regarding the Ayawilca Project PEA; the political environment in which the Company operates continuing to support the development and operation of mining projects; risks related to negative publicity with respect to the Company or the mining industry in general; the threat associated with outbreaks of viruses and infectious diseases, including the novel COVID-19 virus; delays in obtaining or failure to obtain necessary permits and approvals from local authorities; community agreements and relations; and, other development and operating risks. Should any one or more of these risks or uncertainties materialize, or should any underlying assumptions prove incorrect, actual results may vary materially from those described herein. Although Tinka believes that assumptions inherent in the forward-looking statements are reasonable, forward-looking statements are not guarantees of future performance and accordingly undue reliance should not be put on such statements due to the inherent uncertainty therein. Except as may be required by applicable securities laws, Tinka disclaims any intent or obligation to update any forward-looking statement.

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

SOURCE:Tinka Resources Ltd.



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Tinka Announces Filing of Technical Report on an Updated Preliminary Economic Assessment of the Ayawilca Polymetallic Project

Tinka Resources Limited ("Tinka" or the "Company") (TSXV:TK)(BVL:TK)(OTCQB:TKRFF) announces that the Company has filed a National Instrument 43-101 Technical Report entitled "NI 43-101 Technical Report on a Preliminary Economic Assessment of the Ayawilca Polymetallic Project, Peru" ("Technical Report") in support of the Company's news release dated February 28, 2024 (the "News Release"). There are no material differences in the Technical Report from the information disclosed in the News Release. The effective date of the Technical Report is February 28, 2024

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Tinka Resources Limited (TSXV: TK) (OTCQB: TKRFF)

https://tinkaresources.com/

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Highlights:

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    • 7.5m of 20.1% Zn+Pb (19.1% Zn and 1.0% Pb) and 51 g/t Ag, including
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    • 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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Note: Partial assays from G11-3552-27 previously announced on 06-Feb-25, consisting of 24.8m of 8.1% Zn+Pb, 80 g/t Ag;

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

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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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