Opawica Drills 18.7 G/T AU, 13.70 G/T AU, and 12.7 G/T AU at Bazooka

Opawica Drills 18.7 G/T AU, 13.70 G/T AU, and 12.7 G/T AU at Bazooka

(TheNewswire)

Opawica Explorations Inc.

Vancouver, B.C. TheNewswire - August 15, 2022 - Opawica Explorations Inc. (TSXV:OPW) (FSE:A2PEAD) (OTC:OPWEF) (the "Company" or "Opawica")  is pleased to announce the positive drill results on its wholly owned Bazooka Property.

Opawica's drill program on the Bazooka was designed in collaboration with Goldspot who used integrated and reinterpreted data sets (geochemical, geophysical, geological). As a result, Opawica was provided with a cohesive and informed geoscientific interpretation in efforts to help facilitate drill targeting on the Bazooka property. The drill targets that were generated were derived from an understanding gained from Goldspot based on their analysis. Structural interpretations and 3-D modelling were provided by Goldspot and led to the development of an updated geological model which includes fold events, numerous lithostratigraphic units, as well as faults.  The Company completing 5,022 m of drilling over 21 drill holes on the Bazooka and sent in a total of 1,658 rock samples, representing 2,092 linear metres for analysis (See Table 1).

The 21 drill holes were completed on 18 setups testing 18 different drill targets representing less than half of 48 drill targets generated by Goldspot.  Thirty (30) Goldspot drill targets have not been tested for gold mineralization.

Gold mineralization on the property occurs within mixed, up to 60-metre-wide (estimated true width), strong quartz-carbonate-sericite and talc-chlorite schists of sedimentary and ultramafic to mafic volcanic protoliths, respectively, and is referred to as the Main zone. The alteration and mineralization are spatially associated with the Cadillac-Larder Lake. The break/fault zone is at the base and is characterized by up to two-metre-wide (estimated true width), strongly graphitic fault. The graphitic fault generally marks the contact between the sedimentary and ultramafic metavolcanic rocks. This mineralization has been identified throughout the region in producing gold mines like the Yorbeau Resources Inc. Ryoun are acquiring, and more to come, our geological team is gathering a greater understanding of the system. Open to depth, north, south and to the west, we will use this new data to generate additional high priority drill targets for our phase two campaign. Opawica holds 7kms of the Cadillac-Larder fault zone within the Bazooka property, and the exploration team has only touched on 20%. It is well documented that this fault system contains multiple million-ounce deposits and Opawica is moving to uncover and expand the already known gold system."

The Company has engaged Abitibi Geophysics to undertake a DasVision 3D Induced Polarization (IP) over an area of 400x400m portion of the property.  The IP survey covers the main zone alteration where known zone of mineralization is up to 15m wide in quartz carbonate stock work.  The objective of the IP survey is to identify the lateral and vertical extension of known hydrothermal and mineralization zones. In addition, Opawica also plans to undertake downhole geophysics on recent drillholes. The new data will be integrated into the evolving geological model generated by Goldspot for follow up drill targeting.

A follow up program consisting of downhole geophysics (to better define drill targets and define areas for infill drilling) in and around known current and historical gold mineralization in the vicinity of the Bazooka shaft is now being planned.

Mineralization Highlights

18.70 Au g/t over 1 m is within a larger 43.9-meter section of Quartz-sericite stockwork with trace pyrite with visible gold at 279.4 meters.

The 13.70 Au g/t over 1.6 m is in silicified sherd zone with quartz veining with trace tourmaline and fuchsite.

12.70 Au g/t over 0.5 m is in quartz vein stockwork silicified zone with two visible gold flakes.

Table 1: Drill Results

Hole Name

From

To

Length (m)

Au g/t

Hole Name

From

To

Length (m)

Au g/t

OP-21-06

272.0

278.5

4.5

1.96

OP-22-19

332.0

330.0

1.0

4.31

Including

272.0

273.5

1.5

0.18

Including

332.0

332.5

0.5

8.47

273.5

275.0

1.5

5.51

332.5

333.0

0.5

0.14

275.0

276.5

1.5

0.18

OP-22-20

278.0

281.0

3.0

6.48

OP-21-07

194.0

197.0

3.0

2.67

Including

278.0

279.0

1.0

0.19

Including

194.0

195.5

1.5

0.35

279.0

280.0

1.0

18.70

195.5

197.0

1.5

4.99

280.0

281.0

1.0

0.56

OP-21-09

135.0

136.5

1.5

4.26

OP-22-20

283.3

284.4

1.1

2.40

OP-21-11

178.5

180.0

1.5

2.79

OP-22-22

173.0

180.2

7.2

2.34

OP-21-13

143.6

146.6

3.0

8.21

Including

173.0

174.0

1.0

6.30

Including

143.6

145.2

1.6

13.70

174.0

175.0

1.0

1.09

145.2

146.6

1.4

2.72

175.0

176.0

1.0

1.60

OP-21-13c

152.0

153.5

1.5

6.39

176.0

177.0

1.0

2.07

Including

152.0

153.0

1.0

0.07

177.0

178.0

1.0

2.42

153.0

153.5

0.5

12.70

178.0

179.0

1.0

1.51

OP-22-18

237.0

238.5

3.0

3.06

179.0

180.2

1.2

1.42

Including

237.0

238.5

1.5

5.90

OP-22-22

267.0

268.5

1.5

2.35

238.5

240.0

1.5

0.22

Assay results are presented as uncut weighted averages. Interval widths represent drilled NQ core lengths and true width is unknown currently. The balance of the drill results gave negligible values.

Assay samples were analyzed at Techni-Lab Abitibi Inc.(Act labs) 184 Rue Principale Ste-Germaine-Boule Quebec  (an ISO/IEC 17025:2005 accredited facility). The sampling program was undertaken by Company personnel under the direction of Mr. Yvan Bussieres, P.Eng., A secure chain of custody is maintained in transporting and storing of all samples. The rock samples underwent fire assays, 1E3 - Aqua Regia – ICPOES and select samples underwent gravimetries

Samples of mineralization were taken at 0.5-to-1.5-meter intervals, with sample intervals being adjusted to respect lithological and/or mineralogical contacts and isolate narrow veins or other structures that may yield higher grades.  The core was split in two separate sections. One half of the core, the other half is sent for analysis.

One half of the sampled intervals were bagged and tagged with one of the dual sample tags. The individual sample bags are sealed and placed into rice bags and marked with the contents. The samples are delivered in batches in January to Techni-Lab Abitibi Inc. (Actlabs) Ste-Germaine-Boule Quebec, for processing, crushing, pulverizing and analysis.

The Quality Assurance and Quality Control or QA/QC protocols are as follows: A blank sample is inserted at samples ended by the number 10, 30, 70 and 90 in the sample sequence – a blank sample usually consists of white ¾ inch rock that is known not to contain any metals.  A low-grade rock standard is inserted at samples ended by the number 50, in the sample sequence.  A high-grade rock standard is inserted at samples ended by the number 00, in the sample sequence.

Table 2 Drill Hole Locations

Drill Hole

NAD83E

NAD83N

AZ

Dip

Depth (M)

OP-21-06

641010

5339695

170

-68

320

OP-21-07

640966

5339649

170

-55

252

OP-21-08

640966

5339649

170

-55

45.5

OP-21-09

640833

5339533

165

-68

170

OP-21-10

640799

5339520

165

-70

150

OP-21-11

640733

5339568

150

-55

210

OP-21-12

640812

5339601

165

-52

65

OP-21-13

640735

5339608

150

-52.1

150

OP-21-13b

640734

5339608

159.8

-52.9

33.7

OP-21-13c

640735

5339608

159.8

-52.9

222

OP-21-14

640677

5339607

153

-55

192

OP-22-15

640814

5339740

163

-64

366

OP-22-16

640814

5339740

170

-55

351

OP-22-17

640773

5339753

168

-52

280.2

OP-22-17B

640773

5339753

168

-52

280.2

OP-22-18

640780

5339840

165

-60

462

OP-22-19

640783

5339813

172

-62

417

OP-22-20

640822

5339675

160

-68

333

OP-22-21

640822

5339675

174

-62

342

OP-22-22

640763

5339713

157

-64

381

5022.6

Subject to TSXV approval, the Company has repriced the following options to $0.10:

  • 1,650,000 options exercisable at $0.60 expiring June 8, 2026

  • 200,000 options exercisable at $0.34 expiring October 20, 2026

  • 495,000 options exercisable at $0.34 expiring December 22, 2026

About Opawica Explorations Inc.

Opawica Explorations is a junior Canadian exploration company with a strong portfolio of precious and base metal properties within the Rouyn-Noranda region of the Abitibi gold belt in Quebec, and in central Newfoundland and Labrador. The company's management has a great record in discovering and developing successful exploration projects. The company's objective is to increase shareholder value through the development of exploration properties using cost-effective exploration practices, acquiring further exploration properties and seeking partnerships by either joint venture or sale with industry leaders.

Opawica's Bazooka properties cover seven kilometres of the prolific CLLB. The Bazooka properties are bound to the west by the Wassamac gold property, which is 100 per cent owned by Richmont Mines Inc.

Yvan Bussieres, P.Eng., OIQ #31985, has reviewed and approved the technical content of this news release. * The Qualified Person has been unable to verify the information on the adjacent properties. Mineralization hosted on adjacent and/or nearby and/or geologically similar properties is not necessarily indicative of mineralization hosted on the Company's properties.

FOR FURTHER INFORMATION CONTACT

Blake Morgan

President and Chief Executive Officer

Opawica Explorations Inc.

Telephone: 604-681-3170

Fax: 604-681-3552

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

Forward-Looking Statements

This news release contains certain forward-looking statements, which relate to future events or future performance and reflect management's current expectations and assumptions. Such forward-looking statements reflect management's current beliefs and are based on assumptions made by and information currently available to the Company.  Readers are cautioned that these forward-looking statements are neither promises nor guarantees, and are subject to risks and uncertainties that may cause future results to differ materially from those expected including, but not limited to, market conditions, availability of financing, actual results of the Company's exploration and other activities, environmental risks, future metal prices, operating risks, accidents, labor issues, delays in obtaining governmental approvals and permits, and other risks in the mining industry.  All the forward-looking statements made in this news release are qualified by these cautionary statements and those in our continuous disclosure filings available on SEDAR at www.sedar.com.  These forward-looking statements are made as of the date hereof and the Company does not assume any obligation to update or revise them to reflect new events or circumstances save as required by applicable law.

Copyright (c) 2022 TheNewswire - All rights reserved.

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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 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:

  • 25-3552-31, a 65m step-out hole, intersected two strongly mineralized horizons:
    • Cu-Ag horizon (starting at 348.7m downhole)
      • 19.9m of 1.46% Cu and 356 g/t Ag, including
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      • 6.4m of 3.72% Cu and 838 g/t Ag
    • Zn-Pb-Ag horizon (starting at 297.0m downhole)
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      • 12.9m of 11.0% Zn+Pb (7.7% Zn and 3.2% Pb) and 57 g/t Ag, including
      • 3.7m of 20.4% Zn+Pb (15.8% Zn and 4.6% Pb) and 151 g/t Ag
  • Up to 10.45% Cu (over 0.80m) and up to 1,880 g/t Ag (over 0.86m) intersected in the Cu-Ag horizon; to the Company's knowledge, this represents the highest-grade Ag intercept in Ireland over the last >60 years (by any operator) and similarly, one of the highest-grade Cu intercepts
  • Cu-Ag horizon consists of replacement-style mineralization along the base of the Waulsortian Limestone in proximity to a fault structure; mineralization appears to consist mostly of tennantite-tetrahedrite (detailed mineralogy work to be undertaken in due course)
  • Noteworthy is the presence of elevated antimony in the Cu-Ag zone, grading 0.27% Sb within the above 6.4m interval (including 0.80m of 10.45% Cu, 1215 g/t Ag and 0.83% Sb)
  • This hole expands the footprint of the 2.6km long discovery trend by at least 65m down-dip, to a total of at least 170m down-dip along this section (and remains open further down-dip)
  • Drilling continues at Ballywire with two rigs testing (i) the NE extension and (ii) 1.3km ENE of the Ballywire discovery in the vicinity of the prospective 'D' gravity-high anomaly; a third rig was added this week, testing the deeper Cu-Ag target (below the Waulsortian Limestone)

"Intersecting spectacular copper-silver grades over significant thicknesses is a pivotal moment for the Ballywire discovery," stated Bart Jaworski, CEO. "These results not only strongly point to a stratigraphically deeper Cu-Ag horizon but also represent a proof of concept that substantial grades and thicknesses of copper and silver exist at the discovery, in addition to excellent grades of Zn-Pb. The growing presence of critical minerals at Ballywire, namely, copper, germanium and now potentially antimony, highlights the rising strategic importance of this discovery for Ireland, the EU and our shareholders. With today's Cu-Ag milestone, continued drilling to the NE and along our prospective 6km trend, plus the start of drilling with our third rig, we are poised to further grow shareholder value as the year progresses."

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Exhibit 1. Cross-Section Showing New Drilling (25-3552-31) at Ballywire Discovery

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https://images.newsfilecorp.com/files/5685/251260_exhibit1.jpg

Note: True width of mineralized intervals in 25-3552-31, as a percent of down-hole interval, is estimated to be 50-70%

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Exhibit 2. Plan Map Showing New Drilling and Intersected High-Grade Cu-Ag Mineralization

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/251260_exhibit2.jpg

New Step-Out Holes at Ballywire Discovery

The Ballywire prospect at the Company's 100%-owned PG West Project in Republic of Ireland, represents the most significant mineral discovery in Ireland in over a decade. First announced in Sept-2022, the discovery has 52 holes drilled and reported by Group Eleven to date, including the most recent four holes (25-3552-30, -31, -32, and -33) reported today (see Exhibits 1 to 7).

High-grade Zn-Pb mineralization from 25-3552-31 (see Page 1 and Exhibits 1 to 4) consists predominantly of sphalerite, galena and pyrite. High-grade Cu-Ag mineralization in this hole consists of suspected tennantite/tetrahedrite, chalcopyrite, sphalerite, galena and pyrite along and/or close to the base of the Waulsortian Limestone (see Exhibit 1). Noteworthy is the presence of elevated antimony within the Cu-Ag zone. For example, the 6.39m interval below, grading 3.72% Cu and 838 g/t Ag, also grades 0.27% Sb (including 0.80m of 10.45% Cu, 1215 g/t Ag and 0.83% Sb).

Exhibit 3. Summary of Assays from 25-3552-31 at Ballywire

ItemFrom
(m)
To
(m)
Int
(m)
Zn
(%)
Pb
(%)
Zn+Pb
(%)
Ag
(g/t)
Cu
(%)
25-3552-31155.00155.840.848.411.7010.1193.8-
And188.89192.613.722.340.222.5611.9-
Incl.190.82191.750.934.770.455.2225.2-
And296.95344.0747.123.131.374.5021.6-
Incl.300.76301.700.945.210.725.9313.9-
And309.07334.9625.895.102.277.3735.4-
Incl.310.00322.8812.887.723.2410.9557.4-
Incl.315.49319.203.7115.814.5620.37151.1-
And347.79370.4222.630.470.510.98315.81.30
Incl.348.71368.6019.890.490.571.07356.51.46
Incl.348.71360.7312.020.590.791.38560.12.30
Incl.353.39360.737.340.681.271.95768.03.36
Incl.354.34360.736.390.651.462.11838.03.72
Incl.354.34355.200.860.770.060.831880.05.73
And355.20356.090.890.090.020.11516.01.12
And356.09357.020.930.408.478.87399.01.16
And357.02357.980.960.361.151.51128.01.19
And357.98358.780.802.440.212.651215.010.45
And358.78359.841.060.330.060.38979.03.92
And359.84360.730.890.450.030.48871.03.52

 

Note: True width of the mineralized interval in hole 25-3552-31, as a percentage of the down-hole interval, is estimated to be 50-70%; for photographs of Cu-Ag rich core, see Appendix and www.groupelevenresources.com.

Three other holes released today were drilled in a 150m gap to the NE of 25-3552-31 (25-3552-30, -32 and -33; see Exhibit 2). Hole 25-3552-30 returned nil mineralization, 25-3552-32 returned three intervals of mineralization up to 0.94m of 2.4% Zn+Pb (0.9% Zn and 1.5% Pb) and 8 g/t Ag, and 25-3552-33 returned three intervals of mineralization up to 0.82m of 2.9% Zn+Pb (1.1% Zn and 1.8% Pb) and 7 g/t Ag. These zones of mineralization are narrower and weaker than those at the main discovery trend but generally in line with recent holes drilled further to the ENE (see holes G11-3552-24, -26 and 28 in news release dated 25-Mar-2025). Disseminated copper mineralization, as well as, mineralized veins and fractures, is strengthening towards the north, suggesting massive sulphide mineralization may be present further north (see northern-most purple line in Exhibit 4). A second mineralized trend is also emerging to the south where the interpreted Cu-Ag rich 'feeder' fault pierced by drilling along the main discovery trend appears to correlate with mineralization approx. 350m along strike to the ENE, intersected in G11-3552-08 (see solid and dashed purple lines in Exhibit 4). Drilling is ongoing in the NE area to test the above targets.

Copper-Silver Target

Today's results add to a growing body of evidence that support the interpretation of a Cu-Ag 'feeder' fault parallel to and spatially associated with the main Zn-Pb-Ag discovery at Ballywire (see Exhibit 4). With up to 10.45% Cu and 1,880 g/t Ag in a mineralized horizon near a steeply dipping structure, mineralizing fluids are interpreted to have emanated from deeper in the sedimentary sequence (see Exhibit 5). Meanwhile, the stratigraphy of the region suggests that the Lower Limestone Shale horizon exists approximately 100-200m below the discovery horizon (base of the Waulsortian Limestone). This horizon 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, the mineralizing system has the potential to be much larger than its neighbouring occurrences (based on a relatively larger footprint to date); additionally, any Cu-Ag mineralization would notionally be intact below the existing Zn-Pb-Ag mineralization.

Given the compelling nature of this exploration model, Group Eleven added a third rig and began drilling this deeper Cu-Ag target this week.

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Exhibit 4. Plan Map Showing Interpreted Cu-Ag 'Feeder' at Ballywire

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https://images.newsfilecorp.com/files/5685/251260_exhibit4.jpg

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Exhibit 5. Cross-Section Showing Hypothesized Cu-Ag Mineralization in the Lower Limestone Shale

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https://images.newsfilecorp.com/files/5685/251260_exhibit5.jpg

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Exhibit 6. Oblique 3D View of Cu-Ag Mineralization at Ballywire

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https://images.newsfilecorp.com/files/5685/251260_exhibit6.jpg

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

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

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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, 2024); (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) (FSE: 3GE) is drilling the most significant mineral discovery in the Republic of Ireland in over a decade. The Company announced the Ballywire discovery in September 2022, demonstrating high grades of zinc, lead, silver, copper, germanium and locally, antimony. 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)
  • 12.0m of 1.4% Zn+Pb, 560 g/t Ag, 2.30% Cu and 0.17% Sb (25-3552-31), including
  • 6.4m of 2.1% Zn+Pb, 838 g/t Ag, 3.72% Cu and 0.27% Sb (25-3552-31)

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.sedarplus.ca and readers are urged to review these materials, including the technical reports filed with respect to the Company's mineral properties.

APPENDIX - CORE PHOTOS
COPPER-SILVER ZONE IN HOLE 25-3551-31
(With Key Assay Results and Brief Descriptions of Key Mineralogy)

Core Boxes 103-105

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Core Boxes 106-108

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Core Boxes 109-111

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(1) Close-Up Core Photo

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Above: Dolomitized Waulsortian Limestone, cross-cut by sulphide bearing veins (suspected tennatite-tetrahedrite, chalcopyrite and/or pyrite)

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(2) Close-Up Core Photo

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Above: Suspected tennantite/tetrahedrite (grey), chalcopyrite and pyrite (yellow) and calcite (white)

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(3) Close-Up Core Photo

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Above: Chalcopyrite with some pyrite (yellow) and suspected tennantite/tetrahedrite (grey), calcite (white)

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(4) Close-Up Core Photo

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Above: Semi-massive chalcopyrite and pyrite (yellow), galena (reflective grey)

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(5) Close-Up Core Photo

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Above: Waulsortian Limestones (grey), calcite (white), pyrite and chalcopyrite (yellow)

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(6) Close-Up Core Photo

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Above: Suspected tennantite and tetrahedrite (dark grey), chalcopyrite (yellow), calcite (white)

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(6a) Close-Up Core Photo

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Above: Suspected tennantite and tetrahedrite (dark grey), chalcopyrite (yellow), calcite (white)

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(7) Close-Up Core Photo

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Above: Suspect tennantite and tetrahedrite (dark grey), chalcopyrite (yellow), calcite (white)

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(8) Close-Up Core Photo

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Above: Chalcopyrite (yellow), suspected tennantite/tetrahedrite (grey), calcite (white)

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(9) Close-Up Core Photo

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Above: Fault zone (juxtaposing sub-Waulsortian lithologies against Waulsortian Limestone)

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