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Pirate Gold Intersects 0.24% Cu Eq over 299.4m, Including 0.43% Cu Eq over 56.5m, at Moby Dick Discovery

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Pirate Gold Intersects 0.24% Cu Eq over 299.4m, Including 0.43% Cu Eq over 56.5m, at Moby Dick Discovery

 

 

 

 

 

  • PGC-26-118: Collared approximately 100m west of discovery holes PGC-26-058 and PGC-26-068, the hole intersected 0.24% Cu Eq over 299.4m from 12.6m downhole.
  • Higher-grade intervals: The broad interval includes 0.43% Cu Eq over 56.5m, including 0.52% Cu Eq over 35.6m, and a separate interval of 0.43% Cu Eq over 19.8m.
  • Mineralization continues at depth: PGC-26-118 re-entered copper-gold mineralization below a mafic dyke, returning 0.23% Cu Eq over 72.7m, including 0.33% Cu Eq over 37.0m.
  • Follow-up drilling: Assays are pending from 11 additional holes targeting Moby Dick, with visible chalcopyrite logged in eight holes.
  • Next phase underway: Barge drilling is preparing to test beneath Crippleback Lake, while MobileMT surveying is targeting the deeper potential across Crippleback.
  • Episode 18 of Pirate Gold Treasure Hunters now airing:

 

https://youtu.be/tIhp4RaQUxc

 

Pirate Gold Corp. (TSX-V: YARR) (OTCQB: YARRF) is pleased to report assay results from drilling at the Moby Dick copper-gold discovery and the Western EM anomaly within the Crippleback Intrusive Suite at its 100%-owned Treasure Island Project in Central Newfoundland. The Treasure Island Project covers over 90 km of strike along the Valentine Lake Fault Zone in Canada’s newest gold district.

 

Moby Dick Drilling

 

PGC-26-118 was collared approximately 100m west of discovery holes PGC-26-058 and PGC-26-068 and drilled parallel to them. Beginning at the bedrock interface at 12.6m, the hole intersected 0.24% Cu Eq (0.13% Cu; 0.087 g/t Au; 1.72 g/t Ag) over 299.4m to 312.0m. This interval includes 0.43% Cu Eq (0.21% Cu; 0.184 g/t Au; 2.00 g/t Ag) over 56.5m, including 0.52% Cu Eq (0.24% Cu; 0.238 g/t Au; 2.06 g/t Ag) over 35.6m, and a separate interval of 0.43% Cu Eq (0.26% Cu; 0.112 g/t Au; 4.12 g/t Ag) over 19.8m. The hole obliquely intersected a late-stage mafic dyke from 334.0m to 423.0m before re-entering the mineralized zone. From 424.0m to 496.7m, PGC-26-118 returned 0.23% Cu Eq (0.12% Cu; 0.084 g/t Au; 1.65 g/t Ag) over 72.7m, including 0.33% Cu Eq (0.17% Cu; 0.121 g/t Au; 2.32 g/t Ag) over 37.0m.

 

Figure 1. Chalcopyrite mineralization in PGC-26-118 at approximately 294.9m.*

 

 Figure 2. Recent drilling at Moby Dick and the Western EM anomaly.

 

“With copper-gold mineralization encountered from the bedrock surface to nearly 500 metres downhole in PGC-26-118, we are beginning to see the scale taking shape at Moby Dick. The broad mineralized envelope in this hole, alongside the higher-grade core encountered in PGC-26-068, is an encouraging result that adds to our confidence in the size and continuity of the system.

 

“The additional drilling is giving us a much clearer understanding of the orientation of this large zone and indicates that the core of the Moby Dick EM anomaly continues beneath Crippleback Lake. The arrival of the barge drill is an important next step, allowing us to test this highly prospective area for the first time. At the same time, the Mobile MT survey will help us see deeper into the system, refine our geological model and identify the strongest targets for continued drilling.

 

“We are also encouraged by the first hole into the Western EM anomaly, which displays a geophysical signature similar to Moby Dick. The hole returned a broad anomalous copper-gold interval with several narrow higher-grade zones, confirming that this target warrants additional work. With new access established from the south, we will be able to approach the anomaly from a better direction and more effectively test what we believe could be another significant target within the broader Crippleback system,” said Greg Matheson, VP Exploration.

 

“Each round of drilling is making Moby Dick more compelling. Broad copper-gold mineralization has now been intersected in three holes, yet most of the four-kilometre alteration system remains untested. With assays pending, barge drilling preparing to test beneath Crippleback Lake and Mobile MT underway, we have multiple opportunities to expand the mineralized footprint and target what we believe could be the stronger parts of this large system,” said Denis Laviolette, Executive Chairman and CEO.

 

Additional Moby Dick Results

 

PGC-26-088 was drilled approximately 1,800m east of PGC-26-118 at the southeastern end of the Moby Dick alteration anomaly. The hole encountered broad argillic clay alteration from the bedrock interface at 28.5m to 398.0m, where drilling ended due to swelling clay. No visible copper mineralization was noted, although pyrite occurred throughout the hole. Near the bedrock surface, PGC-26-088 intersected 0.18% Cu Eq (0.08% Cu; 0.04 g/t Au; 4.70 g/t Ag) over 20.0m, overlapping an interval of 1.26% Zn over 21.6m. Additional copper mineralization from 164.9m to 177.0m returned 0.12% Cu Eq (0.09% Cu; 0.024 g/t Au; 0.77 g/t Ag) over 12.1m. From 241.9m to 277.3m, the hole returned 0.11% Cu Eq (0.06% Cu; 0.026 g/t Au; 1.80 g/t Ag) over 35.4m. This interval coincides with zinc mineralization from 240.9m to 251.0m, which returned 0.52% Zn over 10.1m. The relationship between the copper-gold and zinc mineralization remains unclear, and zinc is not included in the reported copper-equivalent grades.

 

Western EM Anomaly Drilling

 

The Western EM anomaly is a low-resistivity zone identified by the 2026 airborne EM survey approximately 2.5 kilometres west of the Moby Dick resistivity anomaly (Figure 4).

 

PGC-26-074A encountered unaltered gabbro with a broad anomalous copper-gold interval from the bedrock surface at 17.0m to 338.2m downhole, returning 0.07% Cu Eq (0.05% Cu; 0.01 g/t Au; 0.96 g/t Ag) over 321.2m. Narrow higher-grade intervals include 0.86% Cu Eq (0.56% Cu; 0.154 g/t Au; 12.5 g/t Ag) over 1.0m from 23.0m to 24.0m; 0.84% Cu Eq (0.74% Cu; 0.019 g/t Au; 7.55 g/t Ag) over 0.7m from 195.0m to 195.7m; and 0.92% Cu Eq (0.44% Cu; 0.316 g/t Au; 12.5 g/t Ag) over 0.7m from 336.6m to 337.3m. The hole also returned 0.11% Cu Eq (0.08% Cu; 0.02 g/t Au; 1.48 g/t Ag) over 24.0m from 246.0m to 270.0m. PGC-26-074A is the only hole to have tested the Western EM anomaly and did not adequately explain the EM response. Follow-up drilling is being planned from the southern side of the anomaly.

 

Figure 3. Chalcopyrite mineralization in PGC-26-074A at the Western EM anomaly at approximately 195.2m.*

 

*Core photographs in Figures 1 and 3 are selective and are not representative of the entire mineralized intervals reported for PGC-26-118 and PGC-26-074A.

 

 Figure 4. Recent drilling at Moby Dick and the Western EM anomaly over airborne EM resistivity.

 

 

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Drill Hole From (m) To (m) Length (m) Cu (%) Au (g/t) Ag (g/t) Cu Eq (%) Au Eq (g/t) Zn (%)
PGC-26-074A 17.0 338.2 321.2 0.05 0.01 0.96 0.07 0.06
Incl. 23.0 24.0 1.0 0.56 0.154 12.5 0.                                             .79
Incl. 195.0 195.7 0.7 0.74 0.019 7.55 0.84 0.77
Incl. 246.0 270.0 24.0 0.08 0.02 1.48 0.11 0.10
Incl. 336.6 337.3 0.7 0.44 0.316 12.5 0.92 0.84
PGC-26-088 32.0 52.0 20.0 0.08 0.04 4.70 0.18 0.16
With 30.4 52.0 21.6 1.26
And 164.9 177.0 12.1 0.09 0.024 0.77 0.                                             .11
And 241.9 277.3 35.4 0.06 0.026 1.80 0.11 0.10
With 240.9 251.0 10.1 0.52
PGC-26-104 NSR NSR NSR NSR NSR NSR NSR NSR
PGC-26-118 12.6 312.0 299.4 0.13 0.087 1.72 0.24 0.22
Incl. 149.0 205.5 56.5 0.                                             .184 2.00 0.43 0.39
Incl. 157.0 192.6 35.6 0.24 0.238 2.06 0.52 0.47
And incl. 292.2 312.0 19.8 0.26 0.112 4.12 0.43 0.39
And 312.0 337.7 25.7 0.05 0.047 1.02 0.11 0.10
And 377.4 385.4 8.00 0.07 0.054 0.57 0.13 0.12
And 424.0 496.7 72.7 0.12 0.084 1.65 0.23 0.21
Incl 424.0 461.0 37.0 0.17 0.121 2.32 0.33 0.30

 

Table 1. Significant assay results.

 

Target zones: PGC-26-074A, Western EM anomaly; PGC-26-088, Moby Dick East; PGC-26-104, regional target; PGC-26-118, Moby Dick.

 

1 True widths are unknown; all intervals are reported as downhole lengths.

2 See the QA/QC section for metal-equivalent assumptions and calculation methodology.

3 Intervals not listed are considered to have returned no significant assay results.

 

Moby Dick Alteration Zone

 

Hosted within the Crippleback Intrusive Suite in the southern portion of the Treasure Island Project (Figure 5), Moby Dick is a large advanced argillic alteration zone first identified in 2024. Drilling has now traced the alteration over approximately 4,000m of strike, up to 850m in width and to a depth of 500m. Its full extent remains unknown and is constrained only by drilling completed to date. Spectral analysis indicates that the advanced argillic alteration is primarily composed of montmorillonite, kaolinite and pyrophyllite.

 

As shown in Figure 4, the modelled Moby Dick alteration zone closely correlates with a low-resistivity electromagnetic (“EM”) signature.

 

Initial results from the grassroots discovery were reported on June 17, 2026 and showed broad copper-gold mineralization consistent with a copper-gold porphyry/high-sulphidation epithermal mineralizing system. Discovery hole PGC-26-058 returned 0.38% Cu Eq (0.12% Cu; 0.22 g/t Au; 1.76 g/t Ag) over 112.4m. PGC-26-068 returned 0.54% Cu Eq (0.13% Cu; 0.36 g/t Au; 1.73 g/t Ag) over 180.8m, including 1.48% Cu Eq (0.28% Cu; 1.07 g/t Au; 3.42 g/t Ag) over 49.4m.

 

Figure 5. Location of Crippleback within the Treasure Island Project.

 

Moby Dick Interpretation and Next Steps

 

As an early-stage grassroots discovery with few direct local analogues, Moby Dick is undergoing continued technical investigation to better understand its geological setting, geometry and distribution of mineralization.

 

Drilling to date has outlined broad copper-gold mineralization in three holes across approximately 100m of strike and to vertical depths of approximately 340m within an expansive advanced argillic alteration zone. In most cases, copper-gold mineralization has been confined to the alteration envelopes.

 

Three mineralization styles have been observed to date. The first consists of broad intervals containing intermittent disseminated chalcopyrite and elevated pyrite, together with fine chalcopyrite-filled fractures and locally more massive chalcopyrite over several centimetres of downhole width. The second occurs in strongly altered quartz monzonite and gabbroic intrusions containing disseminated to locally massive pyrite without visually discernible copper sulphides. The third is associated with elevated magnetite concentrations containing chalcopyrite and pyrite within granodiorite and quartz monzonite intrusions and is interpreted to be magmatic in origin. Detailed mineralogical studies are underway to further assess and categorize these styles.

 

The magnetite-chalcopyrite mineralization occurs within a traceable copper-gold core zone encountered in PGC-26-058, PGC-26-068 and PGC-26-118. This zone correlates with the central low-resistivity portion of the Moby Dick EM anomaly and is interpreted to continue beneath Crippleback Lake. The Company has contracted a barge-mounted drill to begin testing portions of the anomaly beneath Crippleback Lake in September 2026.

 

Airborne Mobile MT Survey

 

The Company has contracted Expert Geophysics of Newmarket, Ontario, to conduct an airborne Mobile MT geophysical survey over the southern portion of the Treasure Island Project. The survey follows the airborne EM program completed in early 2026, which defined a resistivity anomaly closely correlated with the Moby Dick alteration zone (Figure 4). Mobile MT is a passive EM system used to map subsurface resistivity and identify potential deeper targets associated with copper-gold porphyry and epithermal mineralization. The survey is planned to cover 4,345 line-kilometres at 100m line spacing and image subsurface resistivity to an approximate depth of 1 to 2 kilometres. The survey commenced on August 30, 2026, and is expected to take four to five weeks, with final deliverables expected approximately eight weeks after completion.

 

Visual Observations from Follow-up Drilling at Moby Dick

 

Eleven additional holes have targeted the Moby Dick alteration zone relative to discovery holes PGC-26-058 and PGC-26-068 (Figures 2 and 4). PGC-26-123 was completed approximately 200m west; PGC-26-125, 1,000m southwest; PGC-26-127 and PGC-26-132, approximately 100m east; PGC-26-133B, 500m east; PGC-26-124, 1,500m east; PGC-26-120, 1,700m east; PGC-26-128A, 1,850m east; and PGC-26-130, 2,100m east. PGC-26-131 and PGC-26-134 were drilled approximately 2,800m east of the discovery holes at the eastern end of the Moby Dick EM anomaly. The intervals of logged visible copper mineralization are summarized below.

 

 

Hole ID From (m) To (m) Description
PGC-26-120 43.7 73.2 Fine grained chalcopyrite disseminated in host rock
PGC-26-120 124.0 215.6 Fine grained chalcopyrite disseminated in host rock
PGC-26-120 223.6 224.0 Fine grained chalcopyrite stringers
PGC-26-120 236.1 249.5 Fine grained disseminated chalcopyrite blebs or stringer
PGC-26-120 313.6 314.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-120 322.0 322.5 Fine grained chalcopyrite disseminated in vein and host rock
PGC-26-120 326.8 329.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-120 357.5 367.1 Fine grained chalcopyrite disseminated in host rock
PGC-26-120 395.9 401.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-120 430.3 445.1 Fine grained chalcopyrite disseminated in host rock
PGC-26-120 477.6 478.0 Fine grained chalcopyrite disseminated in vein and host rock
PGC-26-123 32.0 32.5 Medium grained chalcopyrite in vein fill
PGC-26-123 70.0 368.4 Fine grained chalcopyrite disseminated in host rock
PGC-26-124 50.5 54.8 Medium grained chalcopyrite stringer in host rock
PGC-26-124 101.0 102.0 Fine grained chalcopyrite stringer in host rock
PGC-26-124 114.0 115.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-124 124.3 125.3 Fine grained chalcopyrite disseminated in host rock
PGC-26-124 141.0 142.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-124 158.8 159.7 Fine grained chalcopyrite stringer in vein and host rock
PGC-26-124 237.0 263.2 Fine grained chalcopyrite blebs in host rock
PGC-26-124 340.0 353.8 Fine grained chalcopyrite blebs in vein
PGC-26-124 433.0 436.0 Medium grained chalcopyrite blebs in host rock
PGC-26-125 60.0 61.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-125 65.0 67.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-125 70.0 71.0 Fine grained chalcopyrite disseminated in vein and host rock
PGC-26-125 84.0 85.0 Fine grained chalcopyrite in vein
PGC-26-125 88.0 89.0 Fine grained chalcopyrite in vein
PGC-26-125 130.0 131.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-125 146.0 147.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-125 272.0 273.0 Fine grained chalcopyrite blebs in veins
PGC-26-125 292.0 293.0 Fine grained chalcopyrite blebs in veins
PGC-26-127 149.0 150.0 Fine grained chalcopyrite blebs in host rock
PGC-26-127 319.0 320.0 Fine grained chalcopyrite blebs in host rock
PGC-26-127 387.0 395.0 Medium grained chalcopyrite in host rock
PGC-26-127 415.0 416.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-127 422.0 487.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-127 500.0 508.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-127 513.0 562.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-127 605.0 635.0 Fine grained chalcopyrite disseminated in vein and host rock
PGC-26-127 639.0 640.0 Fine grained chalcopyrite as band in vein and host rock
PGC-26-127 643.0 644.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-127 662.0 666.0 Fine grained chalcopyrite disseminated in vein and host rock
PGC-26-128A 22.0 22.4 Fine grained chalcopyrite blebs in host rock
PGC-26-128A 27.5 29.0 Fine grained chalcopyrite blebs in host rock
PGC-26-128A 35.7 35.8 Fine grained chalcopyrite blebs in veins
PGC-26-128A 179.7 179.8 Fine grained chalcopyrite blebs in vein and host rock
PGC-26-128A 188.3 188.5 Fine grained chalcopyrite blebs in vein and host rock
PGC-26-128A 219.2 219.3 Fine grained chalcopyrite blebs in vein and host rock
PGC-26-128A 274.6 278.8 Fine grained chalcopyrite blebs in veins
PGC-26-128A 328.3 328.8 Fine grained chalcopyrite disseminated in host rock
PGC-26-128A 351.0 352.0 Coarse grained chalcopyrite blebs in host rock
PGC-26-128A 396.0 397.0 Coarse grained chalcopyrite blebs in vein
PGC-26-128A 407.0 408.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-130 No notable visible copper mineralization
PGC-26-131 No notable visible copper mineralization
PGC-26-132 17.0 18.5 Fine grained chalcopyrite disseminated in host rock
PGC-26-132 241.0 242.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-132 249.0 250.0 Semi massive chalcopyrite in host rock
PGC-26-132 317.0 330.0 Fine grained chalcopyrite blebs in host rock
PGC-26-132 560.0 561.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-133B 379.5 381.1 Fine grained chalcopyrite disseminated in host rock
PGC-26-133B 423.7 427.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-133B 437.0 438.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-133B 442.0 447.0 Fine grained chalcopyrite disseminated in host rock
PGC-26-134 No notable visible copper mineralization

 

Table 2. Visual mineralization observations from follow-up drilling at Moby Dick.

 

The company cautions that visual observations of mineralization are not indicative of high assay grades, and drill core samples will be submitted to a certified laboratory for analysis. Assay values for the intervals shown will be released when available. All intervals are down hole depths and true widths are unknown.

 

 

Drill Hole Easting Northing Azimuth Dip Length (m)
PGC-26-058 562447 5398569 345 -65 602
PGC-26-068 562447 5398569 345 -44 596
PGC-26-074A 559295 5397616 155 -45 515
PGC-26-088 563983 5399338 340 -45 398
PGC-26-104 560176 5398806 310 -43 605
PGC-26-118 562352 5398577 345 -45 788
PGC-26-120 564054 5399156 340 -45 860
PGC-26-123 562240 5398610 345 -45 503
PGC-26-124 563871 5399097 340 -45 569
PGC-26-125 561551 5398180 120 -65 347
PGC-26-127 562548 5398614 345 -45 722
PGC-26-128A 564134 5399394 340 -45 683
PGC-26-130 564430 5399291 340 -45 464
PGC-26-131 564759 5400223 210 -50 275
PGC-26-132 562548 5398614 345 -60 645
PGC-26-133B 562900 5398966 315 -50 566
PGC-26-134 564760 5400223 145 -45 263

 

Table 3. Drill-hole information referenced in this release.

 

Pirate Gold Treasure Hunters Season 1 Episode 18 – Moby Dick Part 3

 

Episode 18 takes viewers into the expanding Moby Dick discovery as Pirate Gold follows up on its initial copper-gold results. VP Exploration Greg Matheson explains how PGC-26-118 expands the known volume of mineralized rock, how the broader alteration system is guiding exploration and why the team is now shifting from defining the footprint toward targeting the system’s stronger mineralized core. The episode features:

  • The multi-phased intrusive geology and magmatic fluids believed to have shaped the Moby Dick system
  • How the expanding alteration envelope is helping define the scale of the broader hydrothermal system
  • Three active drills targeting the higher-grade core, testing the system’s margins and advancing new greenfields opportunities
  • A new Mobile MT survey designed to see deeper into Crippleback and refine future drill targets
  • The arrival of a barge-mounted drill to test the interpreted continuation of Moby Dick beneath Crippleback Lake
  • Preparations to advance drilling at Clipper Brook as Pirate Gold searches for the next discovery across Crippleback

Cannot view this video? Visit:

https://www.youtube.com/watch?v=tIhp4RaQUxc

 

Subscribe to Pirate Gold’s YouTube channel for weekly episodes of Treasure Hunters and follow the drill in real time:

 

https://www.youtube.com/@PirateGoldCorp.

 

Qualified Person

 

Greg Matheson, P.Geo., VP Exploration for Pirate Gold, a “Qualified Person” under National Instrument 43-101, has reviewed and approved the scientific and technical information in this press release.

 

About Pirate Gold Corp.

 

Pirate Gold Corp. is a Newfoundland-focused exploration company advancing its 100%-owned Treasure Island Project, a district-scale property covering more than 90 km of strike along the Valentine Lake Fault Zone. Exploration is focused on the high-grade Moosehead gold system, the Moby Dick copper-gold porphyry/epithermal discovery and multiple regional targets across the Crippleback Intrusive Suite. The Company also holds a portfolio of Newfoundland gold projects, including the district-scale Fleur de Lys Project.

 

Posted September 2, 2026

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New Break Resources Ltd. (CSE: NBRK) (OTCQB: NBRKF) (FSE: O91) has received results from the last four holes of a ten-hole, 1,996 metre summer drilling program in the Zavitz gold zone at the Company's 100% owned Moray gold project. In total, New Break has completed 5,372 metres of drilling in 32 drillholes in 2026. Moray is located 49 km southeast of Timmins, Ontario and 32 km northwest of the Young-Davidson gold mine operated by Alamos Gold Inc. Select results from the final four of ten holes drilled in the summer drilling program are presented below in Table 1, while drillhole collar locations are detailed in Table 2 in Appendix A. Table 1 – Moray Summer 2026 Final Drill Results Hole ID Length (m) From (m) To (m) Width (1) (m) Au Grade (2) (g/t) NBR-26-29 322.0 77.3 78.8 1.5 0.42 and 138.0 139.1 1.1 0.38 and 162.5 173.3 10.8 (3) 1.61 and 227.4 229.0 1.6 1.21 and 231.5 232.1 0.6 1.72 NBR-26-30 250.0 37.0 38.0 1.0 0.30 and 102.8 103.5 0.7 0.60 and 121.5 122.5 1.0 0.36 and 124.5 125.5 1.0 0.33 and 128.5 129.0 0.5 0.90 and 131.0 132.0 1.0 0.36 and 169.8 174.0 4.2 2.65 and 178.0 179.5 1.5 0.77 and 183.5 186.6 3.1 1.22 and 190.0 190.5 0.5 1.06 and 191.5 192.5 1.0 1.48 and 196.0 200.5 4.5 2.53 and 203.5 204.0 0.5 2.15 and 206.5 212.0 5.5 1.57 NBR-26-31 274.0 169.0 170.5 1.5 0.37 and 184.5 186.0 1.5 0.51 and 197.0 200.0 3.0 0.94 and 201.5 202.0 0.5 0.50 and 203.5 210.0 6.5 (3) 3.12 NBR-26-32 352.0 73.5 74.0 0.5 0.44 and 174.0 174.6 0.6 0.52 and 194.0 195.0 1.0 0.66 and 199.8 203.3 3.5 2.29 and 227.3 228.0 0.7 0.97 (1) Intervals are drill intersections and do not necessarily represent true widths. (2) All intervals are presented using a cut-off grade of 0.3 g/t Au and internal dilution of no more than 1.0 metres at grades less than 0.3 g/t Au and assays are not capped (see QA/QC Procedures). (3) Drill core photos shown in Appendix B. Figure 1 – Newly Reported Drillholes NBR-26-29, 30 Figure 2 – Newly Reported Drillholes NBR-26-30, 31, 32 Note: The bottom of NBR-26-30 deviated southeast and is represented in both sections. Figure 1: Section B-B1 incorporates drillholes NBR-26-06, 07, 08, 25, 26, 27, 28, 29 and part of 30. Gold mineralization extends southeast into the syenite as exhibited in NBR-26-29. NBR-26-30 is identified in both sections A-A1 and B-B1 as the drillhole was collared along section A-A1 but deviated southeast, intersecting gold mineralization in the mafic volcanics in section B-B1. Figure 2: A-A1 incorporates drillholes NBR-26-03, 04, 05, 23, 24, 30, 31 and 32. NBR-26-31 exhibits gold mineralization both within the syenite (at the contact) and within a "flow breccia" within the hematite altered mafic volcanic at the contact. NBR-26-32 is typified by blocky faulted ground with lamprophyre dykes and gold mineralization in the hematite altered mafic volcanics in a brecciated quartz vein with angular syenitic fragments. William Love, Chief Executive Officer of New Break commented, "Ongoing drilling this summer in the Zavitz gold zone continues to deliver significant gold values, with gold mineralization intercepted in every drillhole. As depicted in Figures 1 and 2, gold mineralization has been encountered predominantly within the mafic volcanics. Importantly, drillholes NR-26-29 and NR-26-32, the deepest drilled to date, demonstrate that gold mineralization extends into the syenite to the southeast at the contact with the mafic volcanics." He further noted, "The intrusive-mafic volcanic contact in the Zavitz gold zone has a distinctive magnetic high. This could be reflective of the higher proportion of iron in these mafic volcanics, which is associated with the higher gold values. This same magnetic and IP signature has been identified elsewhere in areas also believed to be along the intrusive-mafic volcanic contact. Drilling these never before tested targets with the goal of identifying gold mineralization similar to that encountered in the Zavitz zone represents the potential for significantly expanding the Moray gold discovery. There is also the belief that the Zavitz zone could represent the first of a series of stacked mineralized gold zones, which would point to the potential for a much larger gold system at depth. We plan to test this through deeper drilling directly into the Zavitz zone." About the Moray Gold Project The Moray property is located in the heart of the Ontario Abitibi greenstone belt, 49 km southeast of Timmins surrounded by a number of significant gold producing companies and existing mills (see Figure 3). The Young-Davidson gold mine operated by Alamos Gold Inc., with its 8,000 tonne per day mill is the closest and within a short trucking distance of approximately 45 km by road from Moray. The understanding of gold mineralization at Moray continues to evolve with each round of drilling. The occurrence of gold mineralization extending into the syenite to the southeast of the Zavitz zone and in the deepest drillholes is noteworthy given the presence of syenite-hosted mineralization at Young-Davidison. More recent examination of the drill core also suggests that the gold mineralization discovered to date may resemble an intrusion related style of deposit like Agnico Eagle's Upper Beaver gold deposit east of Kirkland Lake, as opposed to a structurally hosted gold system. Both Young-Davidson and Upper Beaver host multi-million ounce gold deposits. Figure 3 – Moray Location Map: Surrounding Gold Producers and Upper Beaver Gold Project Technical Content and Qualified Person The scientific and technical information contained in this news release has been reviewed and approved by Peter C. Hubacheck, P. Geo, consulting geologist to New Break, and an independent Qualified Person as defined by National Instrument 43-101. Mr. Hubacheck certifies that this news release fairly and accurately reflects the technical information and data presented. New Break conducts its exploration activities in accordance with CIM Best Practices Guidelines. QA/QC Procedures QA/QC procedures were executed to ensure all work is conducted in accordance with best practices. All drill core was sawn in half with one half of the core prepared for shipment and the other half retained for future verification. All core is under watch from the drill site to the core processing facility. Drill core is BQTK size and sample intervals range from 0.5 metres to 1.0 metres in length. Commercially prepared certified reference material ("CRM") standards and blanks were inserted with each shipment at a rate of 1 QAQC sample in every 12 core samples. Samples from New Break's 2026 Moray drilling program were analyzed at Activation Laboratories in Timmins, Ontario, which is ISO 17025 certified, by 30-gram fire assay with atomic absorption finish. Any sample assaying greater than 10.0 g/t Au was re-assayed with fire assay gravimetric analysis. Grade composite intervals over core lengths are calculated using a weighted average grade with a cut-off grade of 0.3 g/t Au. Up to 1.0 m of internal dilution (consecutive interval below cut-off grade) are included within specific geologic domains and alteration assemblages, except as otherwise noted. The composites are constrained geologically by metasomatic alteration processes sourcing from the Fiset syenite intrusion and contact mafic volcanic rocks. Elevated gold values are coincident with hematite, silica, sericite and pyrite mineralization within structurally prepared brecciated corridors flanking the intrusion. Intervals are not true widths and no top cutting has been applied to the higher gold values. About New Break Resources Ltd. New Break is a Canadian mineral exploration company focused on its Moray gold project located 49 km southeast of Timmins, Ontario, in a well-established mining camp within proximity to existing infrastructure, and 32 km northwest of the Young-Davidson gold mine, operated by Alamos Gold Inc. Shareholders are also leveraged to exploration success in Nunavut, Canada, through New Break's 20% carried interest in the Sundog gold project and ownership of 6.0 million shares of Guardian Exploration Inc. (TSXV: GX). The Company is supported by a highly experienced team of mining professionals. Appendix A – Drillhole Data and Locations Table 2 – Moray Summer 2026 Drillhole Collar Locations Hole ID Length (m) UTM Easting UTM Northing UTM Elevation Azimuth (degrees) Dip (degrees) NBR-26-29 322.0 492703 5320285 363 220 -70 NBR-26-30 250.0 492708 5320329 363 220 -47 NBR-26-31 274.0 492708 5320329 363 220 -60 NBR-26-32 352.0 492708 5320329 363 220 -70 Total 1,198.0 Coordinates are reported in UTM Zone 17 North, with units in metres. Figure 4 – Zavitz Gold Zone – Surface Traces of 2025 and 2026 Drillholes. All of the drilling at Moray has been completed by Enviro North Exploration Inc. out of Sturgeon Falls, Ontario. Drilling in the Zavitz gold zone is shown in figure 4, with the 1,996 metres in 10 holes drilled this summer depicted in red, the 2,807 metres in 20 holes drilled from January to April 2026 shown in blue and the 1,817 metres in 8 holes drilled in 2025 shown in black. In total, 6,620 metres in 38 drillholes have been completed in the Zavitz gold zone, while New Break has completed a total of 5,372 metres in 32 drillholes of our planned 2026, 10,000 metre drilling program. Appendix B – Drill Core Photos From NBR-26-29 and NBR-26-31

New Break Resources Ltd. (CSE: NBRK) (OTCQB: NBRKF) (FSE: O91) ha... READ MORE

September 16, 2026

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