Heritage Mining's Sampling Program Reports Highest Gold Assay Ever at the Drayton-Black Lake Project, 2,330g/t Gold

Heritage Mining's Sampling Program Reports Highest Gold Assay Ever at the Drayton-Black Lake Project, 2,330g/t Gold

(TheNewswire)

Heritage Mining Ltd.

Channel Sampling Program Confirms Multiple High-Grade Gold-Silver Vein Systems

Heritage Mining Ltd. (CSE: HML) (" Heritage " or the " Company ") is pleased to announce the results from its recent channel sampling program that evaluated fourteen prospects over five targets in the Alcona and Moretti areas (Table 1) located in the northeastern half of the Company's 15,257 Ha Drayton-Black Lake Project (" DBL "). DBL is located approximately 20km northeast of Sioux Lookout, Ontario (Fig. 1) and covers 30 km of the Central Volcanic and Southern Sedimentary domains within the Eagle-Wabigoon-Manitou (" EWM ") Greenstone Belt, which also hosts Treasury Metals Inc.'s (TSX: TML) Goliath Gold-Silver Complex immediately to the southwest

Channel Sampling Highlights

  • Sampling program evaluated fourteen prospects in the Alcona and Moretti areas

  • All channels reported anomalous gold silver and base metal mineralization, significant results include:

Alcona-New Millennium (Figure 1)

    • oo T7 Area - 11.2g/t Au and 51.4g/t Ag over 1.0m

    • oo T9 Area - 5.31g/t Au and 25.0g/t Ag over 0.5m

    • oo Quartz vein subcrop material discovered near to T9 shows visible gold and assayed 2,330g/t Au

Moretti-Main (Figure 2)

    • oo North Vein Prospect - 7.85g/t Au over 2.0m; incl. 19.2g/t Au and 72.8g/t Ag over 0.8m

    • oo channel was done near to where a rock chip grab sample assayed 208g/t Au (see press release November 04, 2022)

Alcona-Main (Figure 3)

    • oo Central Vein Set - 2.72g/t Au over 5.1m; incl. 9.41g/t Au and 25.7g/t Ag over 0.8m

    • oo Central Vein Set - 21.9g/t Au and 121g/t Ag over 1.0m

    • oo North Vein Set - 7.85g/t Au over 2.0m; incl. 19.2g/t Au and 72.8g/t Ag over 0.8m

    • oo Alcona Pond - 4.94g/t Au over 4.0m; incl. 15.75g/t Au and 45.1g/t Ag over 1.0m

Peter Schloo, CEO of Heritage Mining commented, "Our first pass channel sampling results have exceeded our expectations, confirming multiple high-grade Au-Ag mineralized vein systems at surface at Alcona, New Millennium and Moretti, similar to Treasury Metals' Goliath gold project .  These initial results have provided Heritage with valuable information on the style and tenor of gold and base metal mineralization at DBL , as we plan a more systematic field program for the wint er months and into the 2023 exploration season. The team collected a sample of quartz vein subcrop near T9 that reported a whopping 2,330g/t gold, this is the highest reported gold assay at DBL. It is our interpretation that gold, silver, and polymetallic mineralized quartz veins and stockwork zones extend along strike and with depth, and that our ongoing regional evaluation program will continue to identify new veins across this highly under-explored land package. The 2022 field team has done excellent work and our boots on the ground strategy continues to pay off as we further develop the Drayton-Black Lake Project ."

Summary:

Phase 1 channel sample results confirm widespread Au-Ag mineralization hosted in deformation zones ranging from discrete 3-5m wide shear structures (New Millennium) to broad (> 200m) composite deformation zones (Alcona Main Area). Channel results along with grab samples confirm the presence of extensive, structurally controlled and locally high-grade Au-Ag mineral systems.

Mineralization is typically associated with several styles of quartz-carbonate (+/- sulphide) veins ranging in thickness from less than 1.0cm to greater than 50cm wide. Vein orientations vary locally but in general reflect related and consistent structural settings at the prospect and target levels. Geophysical data indicates subtle folding patterns in magnetostratigraphy (e.g., mafic / felsic volcanic units) at both Alcona Main and New Millennium area, in addition to complex regional shear patterns throughout DBL. In several instances, veins and vein arrays are consistent with interpreted axial-parallel orientation and displacement. Many vein array orientations are also consistent with regional-scale structural elements that have not been previously recognized. This provides new context to historic results including more recent (e.g., 2018-2021) till geochemistry completed by previous operators.

Multi-element data from the Alcona Area suggest a strong positive relationship between Au-Ag-Te along with positive correlations between Au and several other potential pathfinder elements. Notably, mineralization at Moretti-Main displays lower Ag:Au ratios suggesting multiple mineralization styles may occur in the northeastern half of the Drayton-Black Lake property. This is similar to Treasury Metals' Goliath gold project (i.e. Goliath-Goldlund-Miller deposits) located 25- 65 km to the southwest in the EWM Greenstone Belt.

The Company is currently compiling and interpreting mapping and sampling data from the 2022 field program along with processing and interpretation of its newly acquired regional airborne Mag/EM survey data. In conjunction with data from previous operators,  staff are now preparing a follow-up program for a planned 2023 drill campaign.

Alcona-New Millennium

At least two mineralized deformation corridors consisting of multiple discrete zones of deformed volcanic rocks and shear parallel quartz veins.

  • Additional prospecting around historic trenches recovered a sample of mineralized quartz vein float with visible gold that returned 2,330g/t (D909175)

  • Heritage staff were able to expose and sample a small portion of in situ quartz vein and this sample (D909173) returned 18.9g/t Au

Nine (9) channels were completed over the T1, T7 and T9 prospects comprising an area of 500m by 200m. There are two distinct structural trends identified at New Millennium: oriented N-S (T1) and E-W (T7 and T9).

  • T9 was assessed over 40m of strike with three (3) channels. Anomalous gold mineralization was encountered in all channels. Highlights include (total length):

    • oo CH-22-18 (1.5m) - 0.81g/t Au over 1.5m; incl. 1.19g/t Au and 9.06g/t Ag over 0.5m

    • oo CH-22-17 (3.0m) - 4.69g/t Au and 23.4g/t Ag over 0.5m

    • oo CH-22-16 (4.2m) - 5.31g/t Au and 25.0g/t Ag over 0.5m

  • T7 was assessed over 10m with three (3) channels. Anomalous gold mineralization was encountered in all channels. Highlights include (total length):

    • oo CH-22-11 (3.0m) - 11.2g/t Au over and 51.4g/t Ag over 1.0m

  • T1 was assessed over 50m strike with three (3) channels. Anomalous gold mineralization was encountered in channel CH-22-15 (0.229g/t Au and 1.15g/t Ag over 1.0m).

  • Field staff also uncovered a large, previously unsampled, outcrop in the T7 prospect area with extensive veining and alteration. Systematic chip sampling across 5m (N=6) returned anomalous gold values up to 1.3g/t Au.


Click Image To View Full Size

Figure 1: Alcona-New Millennium area showing historic and 2022 rock chip and channel sample results

Moretti

Mineralized deformation corridor over 2,500m of strike 500m wide consisting of discrete zones of deformed volcanic rocks and shear parallel quartz veins ranging from cm to metre scale.

At Moretti-Main , six (6) channels were completed over the north and south vein prospects comprising an area of 150m by 130m. Both steep, shear-parallel veins and shallow discordant vein sets were evaluated.

  • At the north vein prospect, a large, well exposed shallow-dipping discordant (to the NE-trending Moretti shear) vein was channeled along strike to assess the bulk gold tenor of that vein and confirm historical sample results. Highlights include (total length):

    • oo CH-22-40 (10.0m) – 7.12g/t Au over 10m; incl. 51.5g/t Au and 1.38g/t Ag over 1.0m.

      •  Including internal dilution with no cutoff applied

    • oo The results compare well with historical sampling.

    • oo High-grade gold samples typically exhibit low Ag/Au ratios, in contrast to those from the Alcona area.

  • At the south vein prospect, two shear-parallel veins were channeled, and both returned positive gold values. Highlights include (total length):

    • oo CH-22-30 (1.5m) - 1.23g/t Au over 1.5m

    • oo CH-22-31 (3.0m) - 1.58g/t Au over 1.0m


Click Image To View Full Size

Figure 2: Moretti area showing historic and 2022 rock chip and channel sample results

At Moretti-Black Lake , fifteen (15) channels were completed on multiple new and historical prospects.

  • Au values ranged from below detection to trace with a positive correlation between Au and Ag noted even in the lower tenor results.

  • Several of the channel sites were selected to test local deformation zones with well-developed ductile shear fabrics and moderate to intense carbonate alteration. Quartz veins were typically mm-scale with an Fe-carbonate association.

Many vein array orientations are also consistent with regional-scale structural elements that have not been previously recognized. This provides new context to historic results including more recent (e.g., 2018-2021) till geochemistry completed by previous operators.

Alcona-Main

Mineralized deformation corridor over 1km strike by 200m wide consisting of multiple discrete zones of deformed volcanic rocks and shear parallel quartz veins open in all directions .

  • A total of 18 channel samples where completed, anomalous gold mineralization was encountered in all channels.

  • Confirm widespread Au-Ag mineralization at surface hosted in broad composite deformation corridors (200m) which is similar to the similar to the Goliath Deposit at Treasury Metals.


Click Image To View Full Size

Figure 3: Alcona Main area showing historic and 2022 rock chip and channel sample results

Nine (9) channels were completed over the North Vein Set and Central Vein Set prospects which comprise the eastern portion of the 200m wide Alcona Deformation Zone.

  • The North Vein Set was assessed over 220m of strike with six (6) channels. Anomalous gold mineralization was encountered in all channels. Highlights include (total length):

    • oo CH-22-03 (2.0m) - 7.85g/t Au over 2.0m; incl. 19.2g/t Au and 72.8g/t Ag over 0.8m

    • oo CH-22-04 (1.0m) - 1.06g/t Au over 1.0m; incl. 1.9g/t Au and 25.6g/t Ag over 0.5m

    • oo CH-22-07 (9.0 m) - 1.17g/t Au and 3.01g/t Ag over 1.0m

  • The Central Vein Set was assessed over 130m of strike with three (3) channels. Anomalous gold mineralization was encountered in all channels. Highlights include (total length):

    • oo CH-22-01 (5.1m) - 2.72g/t Au over 5.1m; incl. 9.41g/t Au and 25.7g/t Ag over 0.8m

    • oo CH-22-02 (8.5m) - 21.9g/t Au and 121g/t Ag over 1.0m

    • oo CH-22-08 (3.0m) - 0.86g/t Au over 3.0m; incl. 1.99g/t Au and 3.61g/t Ag over 1.0m

At Alcona-Pond , nine (9) channels were completed over the Pond prospect which comprise the western portion of the 200m wide Alcona Deformation Zone.

  • The 60m wide Pond prospect was assessed with six (6) channels. Anomalous gold mineralization was encountered in all channels. Highlights include (total length):

    • oo CH-22-21 (11.5m) - 4.94g/t Au over 4.0m; incl. 15.75g/t Au and 45.1g/t Ag over 1.0m

    • oo CH-22-22 (16.0m) - 2.17g/t Au over 3.5m; incl. 6.6g/t Au and 49.5g/t Ag over 1.0m

    • oo CH-22-23 (15.1m) - 4.85g/t Au and 11.35g/t Ag over 1.1m

  • The west extension Pond channel added to the mineralized strike length by an additional 70m. Highlights include (total length):

    • oo CH-22-26 (4.0m) - 0.78g/t Au over 3.0m; incl. 2.52g/t Au and 3.19g/t Ag over 1.0m

Table 1 . List of channel samples and prospects.

Count

AREA

TARGET

PROSPECT

CHANNEL

(4)

Moretti

Main

North

28, 29, 40 and 41

(2)

South

30 and 31

(3)

Black Lake

Emerald

35, 36, and 37

(2)

Drag

38 and 39

(2)

Bloom

42 and 43

(5)

Bloom Road

44, 45, 46, 47 and 48

(2)

Holbrook

33 and 34

(1)

Stockwork

32

(6)

Alcona

Main

North Vein Set

3, 4, 5, 6, 7 and 9

(3)

Central Vein Set

1, 2 and 8

(9)

Pond

Pond (+ E and W)

19, 20, 21, 22, 23, 24, 25, 26, and 27

(3)

New Millennium

T1

10, 14 and 15

(3)

T7

11, 12 and 13

(3)

T9

16, 17 and 18

(48)

(2)

(5)

(14)

(48)

For further information please see the Heritage's profile on SEDAR at www.sedar.com   .

ABOUT THE DRAYTON-BLACK LAKE PROJECT

The Drayton-Black Lake Project is located near the town of Sioux Lookout in Northern Ontario and comprises more than 15,000 Ha within the Eagle-Wabigoon-Manitou (" EWM ") Greenstone Belt along strike of and contiguous with Treasury Metals Inc.'s Goliath Gold-Silver Complex. There are numerous historic high-grade gold (silver, copper) prospects throughout the property within the Central Volcanic domain. All set within a broad multi-kilometer regional-scale deformation corridor with associated secondary and tertiary structural elements. Mineralization is typically shear-hosted quartz-carbonate veins with minor sulphides (1-5%). Locally, mineralized massive sulphide (Py +/- Cpy) occurrences have been documented. Some of the more sulphide rich Au + Au-Ag occurrences in the Southern Sedimentary domain have been notionally reclassified (e.g., Treasury Metal Goliath Deposit) as a hybrid or pre-orogenic atypical greenstone gold (POAGG).

Heritage employs a rigorous quality management system for field sampling and analysis. All samples and sample sites are described, photographed and geo-referenced and digitally archived at the time of sample collection. Material is securely bagged at the sample site and returned to the field office for secure storage. Sampled are delivered by Company personnel to the ALS laboratory in Thunder Bay, Ontario for prep. Samples are crushed (min. 1 kg) and pulverized (250 g; PREP-31A). Au values are determined by 50 g fire assay (Au-AA24), overlimit (Au) are treated with a gravimetric finish (Au-GRA22) and overlimit Ag are treated with acid digestion and ICP/FA finish (Ag-OG62). Multi-element analysis is provided by ICP-MS (ME-MS61). Blind duplicates, blanks, and CRM (Certified Reference Materials) are inserted on a regular basis and p ulps and rejects are retained for check and duplicate analysis.

Scientific and technical information contained in this press release has been prepared under the supervision of Stephen Hughes, P. Geo. Technical Advisor to HML, a qualified person within the meaning of National Instrument 43-101 – Standards of Disclosure for Mineral Projects .

Sampling protocols, quality control and assurance measures and geochemical results related to historic results quoted in this news release (e.g., sampling, drilling, trenching and other data) have not been verified by the Qualified Person and therefore must be regarded as estimates.

ABOUT HERITAGE MINING LTD.

The Company is a Canadian mineral exploration company advancing its two high grade gold-silver-copper projects in Northwestern Ontario. The Drayton-Black Lake and the Contact Bay projects are located near Sioux Lookout in the underexplored Eagle-Wabigoon-Manitou Greenstone Belt . Both projects benefit from a wealth of historic data, excellent site access and logistical support from the local community. The Company is well capitalized, with a tight capital structure.

For further information, please contact:

Heritage Mining Ltd.

Peter Schloo, CPA, CA, CFA

President, CEO and Director

Phone: (905) 505-0918

Email: peter@heritagemining.ca

FORWARD-LOOKING STATEMENTS

This news release contains certain statements that constitute forward looking information within the meaning of applicable securities laws. These statements relate to future events of the Company. Any statements that express or involve discussions with respect to predictions, expectations, beliefs, plans, projections, objectives, assumptions or future events or performance (often, but not always, using words or phrases such as "seek", "anticipate", "plan", "continue", "estimate", "expect", "forecast", "may", "will", "project", "predict", "potential", "targeting", "intend", "could", "might", "should", "believe", "outlook" and similar expressions are not statements of historical fact and may be forward looking information. All statements, other than statements of historical fact, included herein are forward-looking statements.

Forward looking information involves known and unknown risks, uncertainties and other factors which may cause the actual results, performance, or achievements of the Company to be materially different from any future results, performance or achievements expressed or implied by the forward-looking information. Such risks include, among others, the inherent risk of the mining industry; adverse economic and market developments; the risk that the Company will not be successful in completing additional acquisitions; risks relating to the estimation of mineral resources; the possibility that the Company's estimated burn rate may be higher than anticipated; risks of unexpected cost increases; risks of labour shortages; risks relating to exploration and development activities; risks relating to future prices of mineral resources; risks related to work site accidents, risks related to geological uncertainties and variations; risks related to government and community support of the Company's projects; risks related to global pandemics and other risks related to the mining industry. The Company believes that the expectations reflected in such forward-looking information are reasonable, but no assurance can be given that these expectations will prove to be correct and such forward‐looking information should not be unduly relied upon. These statements speak only as of the date of this news release. The Company does not intend, and does not assume any obligation, to update any forward‐looking information except as required by law.

This document does not constitute an offer to sell, or a solicitation of an offer to buy, securities of the Company in Canada, the United States, or any other jurisdiction. Any such offer to sell or solicitation of an offer to buy the securities described herein will be made only pursuant to subscription documentation between the Company and prospective purchasers. Any such offering will be made in reliance upon exemptions from the prospectus and registration requirements under applicable securities laws, pursuant to a subscription agreement to be entered into by the Company and prospective investors.

NOT INTENDED FOR DISTRIBUTION TO UNITED STATES NEWS WIRE SERVICES OR FOR DISSEMINATION IN THE UNITED STATES

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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

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Highlights:

  • G11-3552-29 intersected (from 189.3m):
    • 130.7m of 2.3% Zn+Pb (2.0% Zn and 0.3% Pb) and 13 g/t Ag, including
    • 7.5m of 20.1% Zn+Pb (19.1% Zn and 1.0% Pb) and 51 g/t Ag, including
    • 5.7m of 24.1% Zn+Pb (23.2% Zn and 1.0% Pb) and 60 g/t Ag, including
    • 2.2m of 37.5% Zn+Pb (36.9% Zn and 0.7% Pb) and 72 g/t Ag
    • Represents a 55m step-out down-dip from G11-3552-27
  • G11-3552-271 intersected (from 201.5m):
    • 70.5m of 3.4% Zn+Pb (2.2% Zn and 1.2% Pb) and 41 g/t Ag, including
    • 25.7m of 7.9% Zn+Pb (5.7% Zn and 2.2% Pb), 78 g/t Ag and 0.12% Cu and
    • 4.2m of 2.0% Zn+Pb (0.4% Zn and 1.6% Pb), 172 g/t Ag and 0.66% Cu, including
    • 0.9m of 3.6% Zn+Pb (0.9% Zn and 2.6% Pb), 511 g/t Ag and 2.01% Cu
    • Located 50m down-dip from G11-3552-25 (announced 06-Feb-2025)
  • G11-3552-29 expands the footprint of the recently announced 360m long, flat-lying zone of zinc-rich massive sulphide lenses by at least 50m down-dip, to a total of at least 125m down-dip
  • Drilling continues at Ballywire with two rigs testing further down-dip of the two holes released today, plus the NE extension; assay results are expected in due course
  • In several weeks, drilling will also begin testing (a) a Cu-Ag target below the Zn-Pb-Ag discovery horizon; and (b) a step-out target 1.3km to the ENE of the Ballywire discovery testing in the vicinity of the prospective 'D' gravity-high anomaly, at a locality with abundant calcite similar to the calcite typically observed immediately above high-grade mineralization along the discovery trend

"We are very pleased to see the NE massive sulphide zone expanded by a ninth consecutive high-grade hole," stated Bart Jaworski, CEO. "Additional excellent Ag and Cu values also continue to point to a stratigraphically deeper Cu-Ag horizon, which we are aiming to start drill testing for the very first time over the next few weeks. We also look forward to stepping out 1.3km ENE towards a very prospective area near the 'D' gravity high anomaly. This locality hosts abundant calcite bodies, commonly seen above high-grade mineralization at Ballywire. A nearby historic hole is also mineralized. With the Cu-Ag target, continued drilling to the NE and larger step outs along our prospective 6km trend, 2025 promises to be an exciting year of exploration for Group Eleven."

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Exhibit 1. Cross-Section Showing New Drilling (G11-3552-27, -29 and -31) at Ballywire Discovery

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;

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

To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/5685/245941_1b4f826a447618ea_003full.jpg

Note: Partial assays from G11-3552-27 previously announced on 06-Feb-25, consisting of 24.8m of 8.1% Zn+Pb, 80 g/t Ag;

New Step-Out Holes at Ballywire Discovery

The Ballywire prospect at the Company's 100%-owned PG West Project in Republic of Ireland, is a relatively new zinc-lead-silver discovery (first announced Sept-2022). In addition to 44 holes drilled and reported by Group Eleven to date, the most recent four holes (G11-3552-24, -26, -28, and -29) and additional assays for previously announced hole, G11-3552-27, are reported today (see Exhibits 1 to 7).

High-grade mineralization from G11-3552-27 and -29 (see Page 1 and Exhibits 1 to 4) consists predominantly of massive and semi-massive sulphide (sphalerite, galena, pyrite, chalcopyrite and suspected tennantite-tetrahedrite), as well as, disseminated and vein hosted sulphide mineralization. Mineralization occurs along and/or close to the base of the Waulsortian Limestone (see Exhibit 1).

Exhibit 3. Summary of Assays from G11-3552-24, -26, -27, -28 and -29 at Ballywire

ItemFrom
(m)
To
(m)
Int
(m)
Zn
(%)
Pb
(%)
Zn+Pb
(%)
Ag
(g/t)
Cu
(%)
G11-3552-27201.45271.9470.492.221.203.4140.80.09
Incl.212.07237.8125.745.692.217.9077.80.12
Incl.219.42235.0615.648.303.2811.59122.10.19
Incl.218.47222.213.7412.183.0515.2375.3-
And228.51235.066.5511.065.6516.71240.00.42
Incl.230.36233.903.5413.268.0121.27395.10.73
And267.72271.944.220.401.581.97171.60.66
Incl.268.64269.490.850.932.623.55511.02.01
G11-3552-29189.33320.05130.721.990.262.2513.0-
Incl.224.27229.615.344.100.794.8812.5-
And259.03266.567.5319.081.0120.0951.3-
Incl.259.03264.745.7123.160.9524.1160.0-
Incl.259.03261.252.2236.860.6837.5471.7-
And307.91320.0512.140.230.040.2766.20.12
Incl.315.26320.054.790.380.050.42149.40.27
Incl.318.00320.052.050.090.040.12301.00.52
G11-3552-24186.26199.2012.940.150.040.192.1-
Incl.193.76197.313.550.300.100.404.8-
And235.85236.760.910.010.010.0136.10.35
G11-3552-26215.80216.360.560.830.791.6271.5-
Incl.215.80215.970.172.522.254.77190.0-
G11-3552-28157.95174.8116.860.020.580.593.1-
Incl.166.42169.282.860.051.261.319.0-
And172.99174.811.820.072.122.196.8-
And179.67181.491.820.030.170.2064.10.16
And218.66220.501.840.000.000.012.70.26

 

Note: True width of the intervals above as a percentage of the intersected interval is 90% (G11-3552-27), 80-90% (G11-3552-29), 90-100% (G11-3552-24), 80-90% (G11-3552-26) and 90-100% (G11-3552-28)

Holes drilled as 300m step-outs to the NE (G11-3552-24, -26 and -28; see Exhibit 2) returned zones of mineralization narrower and weaker than those at the main discovery trend (see Exhibit 3). Disseminated copper mineralization, as well as, mineralized veins and fractures, however, are strengthening towards the north, suggesting massive sulphide mineralization may be present further north (see northern-most projected mineralized trend in Exhibit 4). A second mineralized trend is also emerging to the south where the interpreted Cu-Ag rich 'feeder' fault pierced by drilled along the main discovery trend (see solid purple line in Exhibits 2 and 4) appears to correlate with mineralization intersected in G11-3552-08 (see Exhibit 2). More drilling is ongoing in the NE area to test the above targets.

Key 2025 Exploration Targets at Ballywire Discovery

Copper-Silver Target

As drilling progresses at Ballywire, it is increasingly evident that there exists an interpreted Cu-Ag 'feeder' fault parallel to and spatially associated with the main Zn-Pb-Ag discovery at Ballywire (see Exhibit 2). This 'feeder' fault hosts mineralization with up to 5.90% Cu and 1,440 g/t Ag, interpreted to have been transported by mineralizing fluids from below by vertical to steeply-dipping structures (see Exhibit 5). Today's results provide further evidence, with grades up to 2.01% Cu and 511 g/t Ag (see Exhibit 3). Meanwhile, the stratigraphy of the region suggests that approximately 100-200m below the discovery horizon (base of the Waulsortian Limestone), is the Lower Limestone Shale horizon, which hosts four well known Cu-Ag historic occurrences in the surrounding area (see Denison, Oola, Gortdrum and Tullacondra in Exhibit 8, located approx. 5km, 9km, 10km and 45km away from Ballywire, respectively).

These historic Cu-Ag occurrences can be interpreted as the eroded remnants of originally more vertically extensive mineralizing systems, likely representing the roots of stratigraphically higher Zn-Pb-Ag mineralization. At Ballywire, there is a chance the mineralizing system is much larger than at the neighbouring deposits (based on relatively large footprint to date), and if it is there, any Cu-Ag mineralization would notionally be intact below the existing Zn-Pb-Ag mineralization.

Given the compelling nature of the above exploration model, Group Eleven aims to begin drilling this deeper Cu-Ag target over the coming several weeks.

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

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)

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

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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).

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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

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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.

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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

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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