(TheNewswire)

VANCOUVER, BC TheNewswire – September 9, 2025 Heritage Mining Ltd. (CSE: HML FRA: Y66) (‘ Heritage ‘ or the ‘ Company ‘) is pleased to announce a confirmed broad gold zone within a newly discovered ~74m wide quartz vein system (true width unknown) associated with a magnetic anomaly that extends for ~4km along strike length and up to 200m in width (Figure 1, 2) at its flagship Drayton Black Lake Project. Scout drilling targeted this previously unrecognized magnetic feature at Zone Three Extension, as part of the ongoing 2025 Exploration Scout Drill Program.

DBL Exploration Update Highlights

Drilling at Drayton-Black Lake (‘ DBL ‘) Zone 3 Extension prospect confirms gold mineralization over broad widths and associated with a thick quartz vein structure that is up to 74m in core length (true width unknown) as initially reported in Heritage’s press release dated May 15, 2025 and July 22, 2025.

Drill Hole HML25-013 intersected

• 0.98 g/t Au over 5.00m from 101.00m (Figure 3)

• 1.11 g/t Au over 11.09m from 115.91m

Including: 4g/t Au over 2m from 125m (Figure 3)

‘We are very pleased with the discovery of such a wide quartz vein structure. Our limited drilling has now confirmed a broad zone of gold mineralization associated with the ‘mega-quartz vein structure’.  The Company is excited by the potential this vein system exhibits, and we look forward to further communicating the next steps as well as findings on our other projects to the market in short order.’ Commented Peter Schloo, President, CEO and Director of Heritage Mining Ltd.

‘The intersection of very wide (~74m wide in core length, HML25-013) strongly deformed quartz vein in drill holes from Zone 3 Extension in the Lake of Bays Batholith was a great proof of concept for our geology/mineralization model. Multiple stages of deformation, fluid ingress, alteration, and sulphide deposition are evident within the quartz vein system. The return of assays showing a composite interval of 0.98 g/t Au over 5.00m and 1.11 g/t Au over 11.09m (including 4g/t Au over 2m from 125m) in hole HML25-013 provides further encouragement for discovery and support of our model.’ Commented Brett Davis, Structural Geologist Consultant to Heritage Mining Ltd.

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Figure 1: HML25-013, 014 Cross section with 2024 Drone Mag Survey

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Figure 2: Showing the completed and proposed holes testing the northeast-southwest trending magnetic lineament

Discussion of Results

DBL – Zone 3 Extension

The 2025 scout drill program at Zone 3 Extension targeted granite-hosted mineralised quartz-vein structures that were first discovered in the HML Zone 3 drilling program of August 2024 (Figure 2).  The recently completed drill program comprised 4 holes for a total 1105.5m.  Drilling targeted a northeast-southwest trending magnetic lineament, which appears to control the quartz veining.  Drilling is considered a technical success with two ( HML25-011 and 013 ) of the four holes intersecting a well-developed quartz vein structure, including drill hole HML25-013 that intersected a 74m wide vein structure (true width unknown).  Assays received for HML25-010, 011, 012, 13, 14.

Assay results from HML 25-013 confirm broad gold mineralization. Based on the Drone Magnetic survey, the ‘mega-quartz vein structure’ has a potential strike length of ~4km and warrants additional exploration drilling.

Internal dilution is no more then 0.20 g/t Au over a 5m interval.

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Figure 3: HML25-013 Box 29, 126.66m to 126.45m Mineralization Photo (4g/t Au over 2m from 125m interval)

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Figure 4: HML25-013 Box 24 (103.29m – 107.68m) 1.83 g/t Au from 103.5m

Assay results from HML 25-014 confirm anomalous gold values outside the quartz vein zone and inside the granite batholith providing support of a potential mineralized vein system.

HML25-014 Highlights:

• • • • 0.87 g/t Au over 0.46m from 310.82m

      • 0.63 g/t Au over 0.52m from 315.75m

Assays for HML25-010 & 011 & 14 confirm locally elevated gold values in the vein structure per press released July 22, 2025 with HML25-014 missing the structure due to dip direction.

Conclusion

The Company believes additional drilling is warranted to test along this major quartz vein structure along strike.   The Company has proposed an additional 10 holes to test along a 2km strike length of the magnetic lineament (Figure 3) the complete program proposal for the remainder of 2025 will be communicated in short order.

Qualified Person

Stephen Hughes P. Geo, Strategic Advisor for the Company, serves as a qualified person as defined by National Instrument 43-101 – Standards of Disclosure for Mineral Projects and has reviewed the scientific and technical information in this news release, approving the disclosure herein.

Technical Program

Heritage Mining adheres to a strict QA/QC protocol for handling, sampling, sample transportation and analyses.  Chain-of-custody protocols are designed to ensure security of samples until their delivery at the laboratory.

Sampling, Sub-sampling, and Laboratory Analysis for Heritage Mining Drayton Black Lake Project All drilling at the Drayton Black Lake project recovers NQ core. Drill core is systematically split in half using a diamond saw. A qualified geologist examines the drill core, marking intervals for sampling and indicating the cutting line. Sample lengths are typically 1.0 metre, adjusted to a minimum length of 0.5 metre as necessary to respect lithological and/or mineralogical contacts and to isolate narrow veins or structures that may contain higher-grade mineralization.

Technicians saw the core along the cutting lines determined by the geologist. One half of the core is retained as a witness sample, while the other half is submitted for analysis. Individual sample bags are securely sealed and placed into sealed bags, which are then clearly marked with their contents.

Heritage Mining submits samples for gold determination by PhotonAssay to ALS Canada Ltd. (‘ ALS ‘). ALS operates under a commercial contract with Heritage Mining.

Drill core samples are shipped to ALS for sample preparation at their facilities in Thunderbay Ontario. ALS is an ISO/IEC 17025:2017 accredited laboratory for the PhotonAssay method in addition to a variety of diverse metal determination methods.

Analytical Procedures

The ALS procedure for PhotonAssay involves lab applying preparation codes LOG-21 (sample logging via barcode), CRU-31 (fine crushing so that 70% passes through a 2mm screen) and SPL-32a (rotary splitting of a representative ~500g subsample)  followed by analytical code Au-PA01 which is a non-destructive gold analysis method using high-energy X-rays with a gold detection range from 0.03 ppm to 350ppm.

After gold assays are returned, Heritage then may choose to perform multi-element assays on selected samples based on the gold results. In these cases, sample preparation codes FND-05 (locate and use remaining crushed material from Au-PA01) and PUL-32m (pulverization so that >85% passes 75 µm screen) are then applied followed by analytical code ME-MS61 (multi-element ICP-MS analysis for base metals, pathfinder elements, lithophile elements and rare earth elements).

________________________________________

Quality Assurance/Quality Control (QA/QC)

The drill program design, QA/QC, and interpretation of results are performed by qualified persons employing a rigorous QA/QC program consistent with industry best practices. Standards and blanks account for a minimum of 10% of the samples, in addition to the laboratories’ internal quality assurance programs.

Quality Control data are meticulously evaluated upon receipt from the laboratories for any failures. Appropriate corrective action is taken if assay results for standards and blanks fall outside allowed tolerances. All results disclosed by Heritage Mining have successfully passed the Company’s stringent quality control protocols.

The Company does not recognize any factors of drilling, sampling, or recovery that could materially affect the accuracy or reliability of the assay data disclosed. The assay data disclosed in this press release have been verified by the Company’s Qualified Person against the original assay certificates.

Heritage Mining notes that it has not completed any economic evaluations of its Drayton-Black Lake Project, and the project does not currently have any resources or reserves.

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.

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

Copyright (c) 2025 TheNewswire – All rights reserved.

E-Power Resources Inc. (CSE: EPR) (‘E-Power’ or the ‘Company’) is pleased to report results from Phase 1 of the 2025 Exploration Program being completed on the Tetepisca Flake Graphite Property located in the North Shore region of Quebec. Highlights of results include:

• Several high grade (> 10% Cg) samples including a high grade sample of 26.4% Cg from a target area on the northern part of the property which was discvered in 2024.

• Several high grade (> 10% Cg) samples including a high grade sample of 68.7% Cg from Graphi-Centre, the Company’s highest priority target on the Tetepisca Property.

• Discovery of a new flake graphite showing which includes a high grade grab sample of 54.7% Cg located on a long conductive linear trend on the southwestern part of the property.

James Cross, President and CEO of E-Power commented: ‘Phase 1 of our 2025 Exploration Program further demonstrates the from-surface, high grade resource potential of several flake graphite targets on the property. Metallurgical testwork, detailed mineralogy, and continued geological evaluation will result in characterization of the potential deposits and prioritization for advanced evaluation and delineation. By characterizing the different resource delineation targets, we expect to be able to attract users of graphite, and companies who want to secure that link in the supply chain; those who need politically-reliable graphite sources. Those users and traders have the capital to turn it quickly into a resource, and ultimately, a secure source of easily accessible graphite.’

During June 2025, the Company completed Phase 1 of its 2025 exploration and development program on the Tetepisca Flake Graphite Property. Field work included geological and geophysical mapping and prospecting during which 44 grab samples were collected. The objectives of the field work were to:

1) Follow up and expand Flake Graphite discoveries made in 2024 located on the lesser explored northern part of the property,

2) Complete detailed geological mapping and sampling on Graphi-Centre, the Company’s highest priority flake graphite target on the Tetepisca Property,

3) Geological mapping and sampling along the Syndicate Target, a long linear airborne conductor which includes 6 historical flake graphite showings and a historical drill hole with an intercept of 12.74% Cg over 9.55 metres.

4) Collect samples of approximately 250 kg each from selected exposures for preliminary metallurgical test work fron the Graphi Centre target and from the northern claims.

Map 1 is an index map illustrating target areas explored and the locations of bulk samples collected during Phase 1 of the 2025 exploration program.

Map 1

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Northern Claims Target Area and Results

As part of the 2024 exploration program, the company completed a program of geological and geophysical prospecting and mapping on the northern part of the property. The work was focussed on evaluating selected conductors and conductor trends derived from interpretation of the Company’s airborne electomagnetic (‘EM’) survey completed in 2022 as well as historical airborne EM surveys. The 2024 prospecting work resulted in the discovery of 5 flake graphite bearing conductors all of which are characterized by numerous samples > 5% Cg and and all containing high grade samples > 20% Cg (Map 2).

During Phase 1 of the 2025 program, follow-up geological and geophysical mapping and prospecting was completed with the objective of expanding the surface exposure of the N3 and N4 targets. On the N3 target, one additional outcrop was located and stripped. Three grab samples of the exposure returned 23.1 % Cg, 23.0 % Cg, and 17.95% Cg (Map 3). The N3 target is exposed, in isolated outcrop exposures, over a distance of approximately 330 m parallel to the airborne conductive trend. Depth of overburden prohited further exposing the conductive trend.

Map 2

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Work in the area of the N4 target resulted in a significant expansion of the footprint of graphite bearing stratigraphy coincident with airborne conductive trends. Samples recovered from the north-northeast conductive trend west of the 2024 target area returned values of 26.4% Cg, 21.7% Cg, 17.95% Cg, and 7.44% Cg (Maps 2 and 3). A single sample located approximately 35 metres north of 2024 sampling returned a value of 18.05% Cg.

Flake graphite mineralization discovered on the northern claims in 2024 and 2025 is hosted by strongly deformed, high metamorphic grade, sedimentary rocks. Airborne magnetic and EM conductivity patterns indicate that the graphite bearing stratigraphy is part of a complexly folded and faulted sequence continuous from southwest of the N5 target to north, north of the N1 target, and which includes the Uatnan deposit as well as historical graphite mineralization in surface showings and in diamond driill hole intercepts (Maps 1 and 2).

Map 3

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Graphi-Centre Target Area and Results

The Graphi-Centre target area, located in the southern part of the Tetepisca Flake Graphite property, is a domain of curved magnetic and conductive lineaments interpreted as the hinge zone of complexly folded, variably magnetic and conductive stratigraphy (Map 4). The Graphi-Centre domain hosts the historical Graphi-Centre graphite occurrence and a number of historical graphite bearing to high grade graphite grab samples. During 2021, the Company completed a ground based electromagnetic survey to aid in the mapping and interpretation of airborne conductors, and in 2023 drilled 632.7 metres in 5 NQ diamond drill holes and an additional 7.45 metres of BQ core in 3 man-portable drill holes. Highlights of the drilling include 3.80 metres at a average grade of 17.85% Cg. During Phase 1 2025, the Company initiated a program of detailed geological mapping and sampling on the southern part of the Graphi-Centre target area. Fifteen samples were taken from the southern part of the Graphi-Centre target. Highlights of the mapping and sampling include a high of 64% Cg from a grab sample on the South Limb Zone and a high of 68.7% Cg from a grab sample at the western end of the North Limb Zone (Map 4).

Map 4

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Syndicate Target and Results

The Syndicate Target comprises a southeast trending linear airborne conductor approximately 12 kilometres long located in the southwest part of the property. The conductor hosts 6 historical graphite showings; 3 of which were discovered by the Company in 2019 and one of which is a historical drill hole with an intercept of 12.74 % Cg over an intersection length of 9.55 metres (Map 5). During Phase 1 2025, mapping and prospecting resulted in the discovery of an additional showing along the syndicate trend defined by 5 flake graphite bearing samples colleted over a 28 metre southeast trend length. Cg analyses of the 5 samples range from 5.07% Cg to 54.7% Cg (Map 5).

Map 5

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Summary and Next Steps

The Tetepisca Graphite district contains approximately 126 Mt Mt of Measured and Indicated flake graphite mineralization at an average grade of approximately 14% Cg in 3 deposits, one of which has advanced through feasibility containing a reserve of approximate 4.7 Mt of ore at an average grade of 27.8 % Cg. E-Power is the largest holder of mineral rights in the Tetepisca Graphite District with 234 claims covering 12,840 hectares. The E-Power property contains the stratigraphy and geophysical signatures correlated with that hosting the district resources and contains 9 recorded historical graphite showings. E-Power has added to the inventory of showings with a number of graphite discoveries property-wide including those in the northern claim group discovered in 2024.

Since entrance into the Tetepasca Graphite District in 2019, E-Power has been completing a comprehensive property-wide assessment of flake graphite resource potential. The Company is anticipating the near-term reporting of metallurigical testwork initiated during the winter of 2025 from the Captain Cosmos, Syndicate, and Graphi-West Showings. Next steps include continued field work during Phase 2, 2025 and the initiation of additional metallurgical test work and detailed mineralogy study from selected showings. The Company is advancing towards target prioritization for advanced exploration, evaluation, and resource delineation.

About the Tetepisca Property

The Tetepisca Property is located approximately 220 km north of the town of Baie-Comeau in the North Shore Region of Québec. The property consists of 234 claims covering an area of approximately 12,840 hectares within the emerging Tetepisca Graphite District (‘TGD’). The property is 100% owned by E-Power. Fifty-two claims, located in the southern part of the property, are subject to a 1.5% NSR held by a group of local prospectors; otherwise the Tetepisca property remains unencumbered. The TGD is an active graphite exploration and development district with delineated measured and indicated resources in excess of 120 Mt at an average grade of approximately 14% Cg. The Company’s Tetepisca property is strategically located over continuous bedrock conductive horizons that are known and interpreted to be due to graphite and which hold significant potential to host flake graphite resources. The intersection of graphite in our 2023 drilling and the results of our 2024 exploration program to date confirms the Company’s exploration model and provides the basis for continued exploration and evaluation.

Sources of Information and Qualified Person

1) The resource and reserve data on Maps 1 and 2 is from the following sources:

1. NI 43-101 Technical Report Mineral Resource Estimate. Lac Tétépisca Graphite Project Québec, Focus Graphite, 2022 available at the SEDAR website

3. NI 43-101 Technical Report Mineral Resource Estimate on the Lac Gueret South Property. Berkwood Resources Ltd., 2019) available at the SEDAR website

2) The historical graphite showing locations illustrated in Maps 1, 4 and 5 is from the data file of Non-metallic deposits in Quebec, available from the SIGEOM website, Ministère des Ressources Naturelles et des Forêts.

3) The historical Cg data on the Map 4 is from: Rapport des travaux de prospection, Projet Lac Guinécourt, SNRC 22K14, file GM 67766, available from the SIGEOM website, Ministère des Ressources Naturelles et des Forêts.

4) The data for the 2023 drilling program contained in Map 4 is from: Report on 2023 drilling campaign on the Tetepisca property, file GM 73883, available from the SIGEOM website, Ministère des Ressources Naturelles et des Forêts.

5) The historical drill hole intercept reported on Map 5 and discussed in the release is from file GM 68992 available from the SIGEOM website, Ministère des Ressources Naturelles et des Forêts.

6) The Cg data from 2024 appearing on Maps 4 is from the E-Power 2024 exploration program and was released October 9, 2024 and March 7, 2025.

Jamie Lavigne, P. Geo, Vice President Exploration and Director for E-Power is a Qualified Person as defined in NI 43-101 and has reviewed and approved the technical information in this press release.

About E-Power

E-Power Resources Inc. is a Québec Corporation based in Montréal and focused on battery minerals exploration in Québec. The Company is currently advancing two projects; the Tetepisca property, located in the North Shore region of the Province and the Turgeon property located in the Abitibi region adjacent to the Ontario border. The Company’s priority target is flake graphite on the Tetepsica Property. The Turgeon property is located in the prolific Abitibi gold and base metal mining district and the Company is evaluating Turgeon primarily for its copper-zinc and gold potential.

For more information about E-Power Resources Inc. please visit the Company website at: e-powerresources.com.

Notice Regarding Forward-Looking Statements:
This news release contains ‘forward-looking statements.’ Statements in this press release which are not purely historical are forward-looking statements and include any statements regarding beliefs, plans, expectations or intentions regarding the future. Actual results could differ from those projected in any forward-looking statements due to numerous factors. These forward-looking statements are made as of the date of this news release, and the Company assumes no obligation to update the forward-looking statements, or to update the reasons why actual results could differ from those projected in the forward-looking statements. Although the Company believes that the plans, expectations and intentions contained in this press release are reasonable, there can be no assurance that they will prove to be accurate.

To view the source version of this press release, please visit https://www.newsfilecorp.com/release/265515

(TheNewswire)

Vancouver, British Columbia TheNewswire – September 8, 2025 Juggernaut Exploration Ltd (JUGR.V) (OTCQB: JUGRF) (FSE: 4JE) ( the ‘Company’ or ‘Juggernaut’) is excited to announce that it has identified 4 distinct extensive drill-ready gold-rich zones that remain wide open located along the prolific 15 km Highway of Gold Corridor within the Eldorado System, including: the Gold Dome Zone where grab samples assayed up to 256.60 gt Au or 8.25 ozt Au; the Gold Swarm Zone where grab samples assayed up to 226.94 gt Au or 7.30 ozt Au; the Big Mac Zone where grab samples assayed up to 111.35 gt Au or 3.58 ozt Au; and the Whopper Zone where grab samples assayed up to 39.84 gt Au or 1.28 ozt Au on the Big One property (the ‘Property’), Golden Triangle, British Columbia . The Company expanded the high-grade gold mineralized Eldorado System that hosts the Highway of Gold with >500 widespread mineralized veins covering an area of ~9 km 2 . The Big One discovery is located in an area of recent glacial and snowpack abatement adjacent to the world-class gold-rich porphyry systems at Galore Creek. The 100% controlled Big One property covers 36,989 hectares in world-class geologic terrane with tremendous additional discovery potential.

Link to overview map with target names and all samples > 1 g/t Au

Link to overview figures Gold Dome+Big Mac, Whopper, Goldswarm

Dan Stuart, President and CEO of Juggernaut Exploration states: ‘The initial results from this year’s exploration season on the Big One property with grab assays up to 256.60 g/t Au or 8.25 oz/t Au from the newly discovered Gold Dome Zone clearly demonstrate the high-grade nature of this emerging district-scale gold system. With over 500 widespread veins and shears discovered in a very short period of time over 15 km with a vertical relief exceeding 1 km that remains open, shows that the Eldorado System is district scale with tremendous untapped growth potential. The Eldorado gold system and Highway of Gold Corridor are showing the right ingredients to quickly become the next big discovery in the Golden Triangle. We look forward to unlocking the full potential of this discovery with the drill bit with much anticipation. The entire team believes we are only seeing the tip of the iceberg and the best is yet to come.’

Manuele Lazzarotto, PhD, Chief Geologist of Juggernaut Exploration states: ‘I am happy to report on behalf of the entire team that the successful 2025 systematic exploration program was just wrapped up on August 29th and all goals have been accomplished on time and on budget. The excellent results with many grab samples with multi-ounce gold assays from 4 extremely gold-rich extensive drill-ready zones within the 15 km Highway of Gold Corridor, namely the Gold Swarm Zone, Big Mac Zone, Gold Dome Zone and  Whopper Zone, which some say appears to be a lot like the high-grade seen at Brucejack, or epithermal/porphyry related or related to a magmatic intrusive. It’s early days but these are all possible geological model outcomes. All of this is a clear testament that we appear to have discovered a new gold-rich, polymetallic-rich district-scale system at Big One. Over 500 mineralized veins many with remarkable gold content have been confirmed on surface and we look forward to testing the subsurface with the planned inaugural drill program. The team is eager to start planning the upcoming fully funded drill campaign designed to test these 4 extensive zones once all the data collected this season has been received, compiled and interpreted.’

The Eldorado system consists of a vast area of ~9 km 2 of recently exposed bedrock that hosts the 15 km Highway of Gold Corridor containing >500 widespread polymetallic quartz-sulphide veins and shears as well as extensive propylitic alteration within a vertical relief of 1 km. The polymetallic veins contain semi-massive to massive chalcopyrite, sphalerite and galena with grades up to 256.60 g/t Au or 8.25 oz/t Au that remain wide open, visually and geochemically reminiscent of the high-grade veins observed at Brucejack. Grab samples collected during the 2024 season assayed up to 2084 g/t Ag and 7.9% Cu. 2025 assay results reported in this news release only comprise gold values. Results for silver, copper, lead and zinc will be reported once analyses are completed and the data has been reviewed and compiled. Four gold-rich polymetallic mineralized zones have been identified and are planned to be tested during the inaugural drill program.

Initial highlights from the 2025 exploration season:

• The Big Mac Zone measures ~1 km by ~1 km and consists of multiple large veins with shear zones that are up to 10 meters wide and exposed on surface for 400 meters with vertical reliefs of up to 360 m where they are covered by snow and ice and remain wide open. A channel cut from the Big Mac Zone that assayed 6.63 g/t Au over 3.58 meters, including 17.45 g/t Au over 1.35 m and 47.18 g/t Au or 1.52 oz/t Au over 0.47 m, true width, was collected 5 meters to the east of a grab sample that assayed up to 111.35 g/t Au. A second channel cut assayed 3.60 g/t Au over 1.45 meters, including 10.17 g/t Au over 0.50 meters located 270 m on strike to the west of the 111.35 g/t Au sample. A grab sample, located 450 m to the west, assayed 55.5 g/t Au or 1.78 oz/t Au from a difficult-to-access secondary vein located in the nearby cliffs. 14 out of 26 samples (54%) from the Big Mac Zone assayed 1 g/t Au. The Big Mac Zone is drill-ready.

Link to video , Link to image gallery

Table 1: Big Mac Zone samples >1 g/t Au

• The Whopper Zone is a ~2 km by ~2 km area that consists of multiple veins up to 5 meters wide and extensive shear zones up to 50 meters wide that are exposed on surface for 500 meters with vertical reliefs of up to 780 meters. Channel cuts from the Whopper Zone assayed up to 39.84 g/t Au or 1.28 oz/t Au over 0.50 m within a larger interval that assayed 6.71 g/t Au over 3.06 meters. Multiple grab collected upslope of the channel cut along a 5 meter wide vein hosted in an 8 meter wide shear zone along 50 meters of exposed vein assayed up to 13.12 g/t Au. The shear zones are difficult to sample due to the exposed cliffs and comprise numerous lenses of semi-massive to massive galena, chalcopyrite, sphalerite and pyrite contained in quartz veins and stockwork and remain open on either side, where they are covered by snow and ice. 32 samples out of 158 (20%) assayed 1 g/t Au. Multiple targets in the Whopper zone are drill-ready

Link to video , Link to image gallery

Table 1: Whopper Zone samples >1 g/t Au

• The Gold Swarm Zone contains clusters of shear zones and veins up to 4.5 meters wide with grab samples that assayed up to 226.94 g/t Au or 7.30 oz/t Au and a channel cut that assayed 4.02 g/t Au over 4.36 m containing substantial amounts of semi-massive to massive chalcopyrite, galena and sphalerite. The zone has been recently exposed by glacial retreat and covers an area of ~1 km by ~1 km and extends over a vertical relief of 440 m and remains open in all directions. 27 samples out of 44 (61%) assayed 1 g/t Au. The Gold Swarm Zone is drill-ready.

Link to video

Table 1: Gold Swarm Zone samples >1 g/t Au

• The Gold Dome Zone is a ~3 km by ~1.5 km zone that consists of clusters of multiple extensive gold-rich shear zones, veins, and stockwork that are up to 4 meters wide and exposed on surface for 1 km with a vertical relief of ~600 m and remain open. Grab samples assayed up to 256.60 g/t Au or 8.25 oz/t Au and a channel cut assayed 5.45 g/t Au over 2.77 meters from a vein exposed on surface in the adjacent difficult to reach cliff face for ~200 meters. The mineralized veins contain seams of semi-massive galena, sphalerite, chalcopyrite and pyrite. 46 samples out of 191 (24%) assayed 1 g/t Au. Multiple targets in the Gold Dome Zone are drill ready.

Link to video , Link to image gallery

Table 1: Gold Dome Zone samples >1 g/t Au

• A total of 421 rock samples were collected during the 2025 exploration season along the 15 km Highway of Gold: 272 grab/float samples and 149 channel samples. Preliminary assay results for samples reported in this news release only comprise gold. Assay results only comprise gold values. Results for silver, copper, lead and zinc will be reported once analyses are completed and the data has been reviewed and compiled. Based on assay results reported from the 2024 season on samples that are visually similar to the samples reported today, the previously reported 2024 samples assayed up to 2084 g/t Ag and 7.9% Cu, shows there is strong potential for considerable added value once full assays are received.

• Detailed geological and structural mapping has been completed on the reported drill targets in order to better understand the full geometry of these high-grade gold-bearing shears and veins and will be instrumental in designing the drill plan for the upcoming maiden drill program.

• A high-resolution UAV photogrammetry survey was completed over an area of 52 km on the Eldorado System encompassing the entire 15 km Highway of Gold with all four of the confirmed drill targets. The data will be used to support modelling and better understand the high-grade gold mineralization recently discovered.

• A property wide LiDAR survey covering an area of 385 km has been conducted and will be used to augment information obtained from the mapping as well as plan the upcoming inaugural drill campaign.

• The polymetallic veins, alteration signature, geochemical path finder element signature, and geophysical anomalies strongly indicate the presence of a common buried gold-silver-copper rich porphyry feeder source or similar magmatic source at depth responsible for the extensive high-grade veining confirmed on surface.

• Four extensive drill-ready Zones have been confirmed on the 15 km Highway of Gold Corridor and are planned to be tested in the inaugural drill program and include: the Gold Dome Zone where grab samples assayed up to 256.60 g/t Au or 8.25 oz/t Au; the Gold Swarm Zone where grab samples assayed up to 226.94 g/t Au or 7.30 oz/t Au; the Big Mac Zone where grab samples assayed up to 111.35 g/t Au or 3.58 oz/t Au; and the Whopper Zone where grab samples assayed up to 39.84 g/t Au or 1.28 oz/t Au.

The Big One property is situated in a region that is well known for hosting world class precious metal and porphyry deposits, several of which occur near the property including the multiple porphyry systems at Galore Creek (12,159 million pounds of copper, 9.438 million ounces of gold, 174.086 million ounces of silver), the world’s largest known gold reserve at KSM (47.3 million ounces of gold, 160 million ounces of silver, 7.32 billion pounds of copper) and the polymetallic copper project at Shaft Creek (5 billion pounds of copper, 3.7 million ounces of gold, 16.4 million ounces of silver), as well as the Brucejack high-grade epithermal gold deposit (14 million ounces of gold, 91.8 million ounces of silver), and the structurally controlled high-grade hydrothermal gold-silver zones at Trophy and Sphal Creek. The property geology is favorable to host these types of deposits as confirmed by the presence of extensive areas of propylitic alteration, untested geophysical anomalies, strong silt, soil and rock geochemistry including path finder elements directly related to porphyry systems, key structures and textures, porphyry-style mineralization, and high-grade polymetallic veins, that have been discovered within the Big One claims.

Property Location Map

The Big One property can be accessed year-round via helicopter from the Glenora/Telegraph Creek Road at the Barrington Mine (33 km to the north-northeast) as well as the Galore Creek Road (15 km to the southeast). The Canadian government committed $20 M to extend/improve the Galore Creek Road to within 15 km of the Big One property. The property is 2 km west of the Scud River airstrip used in the early days of Galore Creek.

A Notice of Work application (drill permit application) has been submitted to the British Columbia Ministry of Mining and Critical Minerals in preparation for the inaugural drill program. The Big One property exploration qualifies for the Critical Mineral Exploration Tax Credit (CMETC).

The Company would like to extend a special thanks to the Tahltan First Nation, the local community and service providers for supporting our efforts and contributing to the success of this year’s program. We look forward to continuing to work with the Tahltan First Nation and all local stakeholders, and businesses, while we move forward to unlocking the full potential of this amazing new discovery. WORKING TOGETHER WE SUCCEED!

About Juggernaut Exploration Ltd.

Juggernaut Exploration Ltd. is an explorer and generator of precious metals projects in the prolific Golden Triangle of northwestern British Columbia. Its projects are in world-class geological settings and geopolitical safe jurisdictions amenable to Tier 1 mining in Canada. Juggernaut is a member and active supporter of CASERM, an organization representing a collaborative venture between the Colorado School of Mines and Virginia Tech. Juggernaut’s key strategic cornerstone shareholder is Crescat Capital.

For more information, please contact:

Juggernaut Exploration Ltd.

Dan Stuart

President, Director and Chief Executive Officer

Tel: (604)-559-8028

www.juggernautexploration.com

Qualified Person

Rein Turna, P. Geo is the qualified person as defined by National Instrument 43-101, for Juggernaut Exploration projects, and supervised the preparation of, and has reviewed and approved, the technical information in this release.

Other

The reader is cautioned that grab samples are spot samples which are typically, but not exclusively, constrained to mineralization. Grab samples are selective in nature and collected to determine the presence or absence of mineralization and are not intended to be representative of the material sampled.

Grab, channels, chip and talus samples were collected by foot with helicopter assistance. Prospective areas included, but were not limited to, proximity to MINFile locations, placer creek occurrences, regional soil anomalies, and potential gossans based on high-resolution satellite imagery. The rock grab and chip samples were extracted using a rock hammer, or hammer and chisel to expose fresh surfaces and to liberate a sample of anywhere between 0.5 to 5.0 kilograms. All sample sites were flagged with biodegradable flagging tape and marked with the sample number. All sample sites were recorded using hand-held GPS units (accuracy 3-10 meters) and sample ID, easting, northing, elevation, type of sample (outcrop, subcrop, float, talus, chip, grab, etc.) and a description of the rock were recorded on all-weather paper. Samples are then inserted in a clean plastic bag with a sample tag for transport and shipping to the geochemistry lab. QA/QC samples including blanks, certified reference materials, and duplicate samples are inserted regularly into the sample sequence at a rate of 10%.

All samples are transported in rice bags sealed with numbered security tags. The rice bags are transported from the core shacks to the MSALABS facilities in Terrace, BC. MSALABS is certified with both AC89-IAS and ISO/IEC Standard 17025:2017. The core samples undergo preparation via drying, crushing to ~70% of the material passing a 2 mm sieve and riffle splitting. The sample splits are weighed and transferred into three plastic jars, each containing between 300 g and 500 g of crushed sample material. A 250 g split is pulverized to ensure at least 85% of the material passes through a 75 µm sieve. The crushed samples are transported to the MSALABS PhotonAssayTM facility in Prince George, where gold concentrations are quantified via photon assay analysis (method CPA-Au1). Samples that result in gold concentrations ≥5 ppm are analyzed to extinction. Photon assay uses high-energy X-rays (photons) to excite atomic nuclei within the jarred samples, inducing the emission of secondary gamma rays, which are measured to quantify gold concentrations. The assays from all jars are combined on a weight-averaged basis. Multielement analyses are carried at the MSALABS facilities in Surrey, BC, where 250 g of pulverized splits are analyzed via ICF6xx and IMS-230 methods. The IMS-230 method uses 4-acid digestion (a combination of hydrochloric, nitric, perchloric and hydrofluoric acids) followed by inductively coupled plasma emission spectrometry to quantify concentrations of 48 elements. Samples with over-limit results for Ag, Cu, Pb and Zn undergo ore-grade analysis via the ICF-6xx method (where ‘xx’ denotes the target metal). This method employs 4-acid digestion followed by inductively coupled plasma emission spectrometry.

NEITHER THE TSX VENTURE EXCHANGE NOR ITS REGULATION SERVICES PROVIDER (AS THAT TERM IS DEFINED IN THE POLICIES OF THE TSX VENTURE EXCHANGE) ACCEPTS RESPONSIBILITY FOR THE ADEQUACY OR ACCURACY OF THIS RELEASE.

FORWARD LOOKING STATEMENT

Certain disclosure in this release may constitute forward-looking statements that are subject to numerous risks and uncertainties relating to Juggernaut’s operations that may cause future results to differ materially from those expressed or implied by those forward-looking statements, including its ability to complete the contemplated private placement. Readers are cautioned not to place undue reliance on these statements.

NOT FOR DISSEMINATION IN THE UNITED STATES OR TO U.S. PERSONS OR FOR DISTRIBUTION TO U.S. NEWSWIRE SERVICES. THIS PRESS RELEASE DOES NOT CONSTITUTE AN OFFER TO SELL OR AN INVITATION TO PURCHASE ANY SECURITIES DESCRIBED IN IT.

Copyright (c) 2025 TheNewswire – All rights reserved.

Sun Summit Minerals Corp. (TSXV: SMN,OTC:SMREF) (OTCQB: SMREF) (‘Sun Summit’ or the ‘Company’) is pleased to report results from its first drill hole completed in 2025 at the JD Project, Toodoggone Mining District, north-central British Columbia.

Hole CZ-25-007 returned one of strongest intervals of consistent and near-surface gold mineralization drilled to date at the Creek Zone: 78.0 meters of 3.72 g/t gold starting at 30.0 meters down hole. This interval of near-surface gold mineralization is in an area previously untested by drilling and is interpreted to represent a parallel trend of mineralization north of the Creek Zone where it remains open to the northwest. Follow-up drilling is planned for this season.

Highlights:

• Hole CZ-25-007 intersected a significant zone of near-surface, continuous gold mineralization punctuated with high-grade veins:
  • 78.0 meters of 3.72 g/t gold from 30.0 meters down hole, including
  • 12.0 meters of 8.55 g/t gold, and including
  • 19.1 meters of 7.50 g/t gold
  • The 78.0 meter interval contains multiple high-grade veins, some with fine visible gold, that returned 31.84 g/t gold over 1.0 meters, 54.40 g/t gold over 1.0 meters, 67.80 g/t gold over 0.90 meters and 98.80 g/t gold over 0.5 meters. These intervals clearly demonstrate the high-grade gold mineralization potential of the Creek Zone.
• Establishes a new zone of high-grade and disseminated mineralization: The upper 78.0 meter interval is in an area not previously tested by drilling and may represent a parallel zone of mineralization north of the main series of Creek Zone high-grade veins.
• Follow-up drilling planned: Based on the exceptional results from CZ-25-007, additional step-out holes are planned for this season to test the down-dip and northwest strike extent.
• Additional assay results pending: Assays from the remaining ten holes (3,340 meters) drilled at the Creek zone are pending.

‘The first hole of this year’s drill program at our JD Project in the significant Toodoggone District, represents the best hole drilled to date at the Creek Zone,’ said Niel Marotta, CEO of Sun Summit Minerals. ‘The hole intersected significant mineralization from 30 meters downhole. This interval is punctuated with multiple high-grade zones which supports the high-grade gold potential of the Creek Zone, typical of many Toodoggone gold deposits. We have planned additional holes to test the strike extent of this new zone of mineralization and are excited to move the drill rig back to the area in the coming weeks.’

Table 1. Assay Results^1,2

1. Intervals are downhole core lengths. True widths are unknown.
2. Calculations are uncut and length-weighted using a 0.10 g/t gold cut-off.
3. Grades have not been capped in the length-weighted averaging.

Drill Hole CZ-25-007

Hole CZ-25-007 was collared 75 meters to the north of hole CZ-24-004 (122.53 metres of 2.11 g/t gold including 4.04 metres of 46.78 g/t gold, see October 2, 2024 news release) and stepped out 100 meters west of hole CZ-24-005 (57.95 meters of 2.69 g/t gold including 19.50 meters of 7.31 g/t gold, see October 16, 2024 news release, Figure 1). The upper interval of strong disseminated and high-grade vein-hosted gold mineralization in CZ-25-007 (e.g., 78.0 meters 3.72 g/t gold, Table 1) is approximately 120 metes to the northwest of the upper interval in CZ-24-005 (Figure 2). Together, these intercepts may represent a new zone of mineralization that trends parallel to the main steeply-dipping northwest-striking vein-sets (e.g., 22.0 m of 11.7 g/t Au including 4.0 m of 61.2 g/t Au, in hole CZ97-008¹). Further drilling is warranted to test the strike- and dip- extent of this parallel zone.

The upper interval in CZ-25-007 contains multiple high-grade veins and breccias (31.84 g/t gold over 1.0 meters, 54.40 g/t gold over 1.0 meters, 67.80 g/t gold over 0.90 meters and 98.80 g/t gold over 0.5 meters) within the broad zone of disseminated gold mineralization (Figure 3). Many of these higher-grade intervals contain fine visible gold (Figure 4). These intervals demonstrate the high-grade mineralization potential of the Creek Zone and support the strong prospectivity of the Creek Zone to the northwest in an area lacking drilling.

Hole CZ-25-007 intersected a bedded sequence of intermediate volcanic and volcaniclastic rocks interpreted to be a sequence within the McClair Member of the Early Jurassic Toodoggone formation. Higher-grade gold mineralization is hosted in epithermal-related and locally banded quartz-carbonate veins, veinlets and sulfide-cemented breccias with locally strong potassium feldspar alteration halos (Figure 3). Vein-hosted sulfides include pyrite, sphalerite, ± chalcopyrite and galena with some veins containing visible gold. Bulk-tonnage mineralization is associated with selectively pervasive sericite-chlorite-hematite alteration with disseminated pyrite, proximal to vein-associated potassic alteration (Figure 3).

Drill Program

Drilling in 2025 at the Creek Zone was designed to investigate the lateral and vertical extent of high-grade and bulk-tonnage gold mineralization (Figures 1 and 2). Over 3,700 meters across 11 drill holes at Creek have so far been completed. These holes were designed to systematically test the vein-controlling structures on 50 to 100 meter pierce-points covering a strike-length of over 800 meters and a down-dip extent of over 200 meters (Figures 1 and 2). Based on the result of CZ-25-007 step-out holes to the northwest are planned this season.

Assays from the remaining drill holes, as well as surface sampling results are pending and will be released as they are received and reviewed.

Figure 1. Plan map showing drill collar location of CZ-25-007 and additional drill holes with pending results. Selected highlights from the 2024 drill program at the Creek Zone are also shown (see October 2^nd, 2024 and October 16^th, 2024 news releases). See references 1 and 2 for sources of historical drill data.

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https://images.newsfilecorp.com/files/6142/265410_d618af9264737880_001full.jpg

Figure 2. Oblique view through the Creek Zone drill holes showing downhole assays for all drill holes including CZ-25-007 and holes with pending results. Selected highlights from the 2024 drill program at the Creek Zone are also shown (see October 2^nd, 2024 and October 16^th, 2024 news releases). See references 1 and 2 for sources of historical drill data.

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https://images.newsfilecorp.com/files/6142/265410_d618af9264737880_002full.jpg

Figure 3. Core photos of CZ-25-007, A. Box photos showing core from 24.99 m to 80.0 m downhole which includes four high-grade intervals of 31.84 g/t Au over 1.0 m, 54.40 g/t Au over 1.0 m, 67.80 g/t Au over 0.94 m and 98.80 g/t Au over 0.50 m collectively within a broader interval of 49.0 m of 5.57 g/t Au. Individual down hole gold assay results are annotated at the sample depths.

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https://images.newsfilecorp.com/files/6142/265410_d618af9264737880_003full.jpg

Figure 4. Core photos from CZ-25-007 showing zones of high-grade mineralization, A. sulfide-cemented hydrothermal breccia at 59.9 m down hole (67.80 g/t gold over 0.94 m) with visible gold B. example of visible gold at 59.9 m down hole, C. high-grade vein at 37.0 m down hole (31.84 g/t gold over 1.0 m) with specks of visible gold, D. example of visible gold at 37.0 m down hole. Abbreviations, qtz = quartz, carb = carbonate, epi = epidote, sph = sphalerite, cpy = chalcopyrite.

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https://images.newsfilecorp.com/files/6142/265410_d618af9264737880_004full.jpg

Figure 5. Map of the Toodoggone District showing the location of the JD Project in relation to other development and exploration projects. Data sourced from Thesis, TDG and Centerra’s corporate websites. The QP has been unable to verify the information and that the information is not necessarily indicative to the mineralization on the property that is the subject of the disclosure.

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Table 2. Drill Collar Location

Coordinates are in UTM NAD83 Zone 9N

Quality Assurance and Quality Control

All drill core sample assay and analytical results have been monitored through the Company’s quality assurance and quality control program (QA/QC). Drill core was sawn in half at Sun Summit’s dedicated and secure core logging and processing facility at the JD exploration camp.

Half of the drill core was sampled and shipped by a bonded courier in sealed and secured woven polyester bags to the ALS Global preparation facilities in Kamloops, BC. Core samples were prepared using ALS standard preparation procedure PREP-31A which involves crushing the sample to 70% less than 2mm, followed by a riffle split of 250g, and then a pulverised split to better than 85% passing 75 microns.

Following sample preparation, the pulps were sent to the ALS Global analytical laboratory in North Vancouver, B.C. for analysis. ALS Global is registered to ISO/IEC 17025:2017 accreditations for laboratory procedures.

Drill core samples were analyzed for 48 elements by ICP-MS on a 0.25-gram aliquot using a four-acid digestion (method ME-MS61). This method is considered a ‘ultra trace element’ analytical method with low detection limits on key pathfinder elements such as Ag, As, Sb, Se and Tl.

Gold was analyzed by fire assay on a 30-gram aliquot with an AES finish (inductively coupled plasma atomic emission spectroscopy – method Au-ICP21). Samples that returned >10 parts per million (ppm) gold were re-analyzed by fire assay using a gravimetric finish on a 30-gram aliquot (method Au-GRA21).

Overlimit samples (e.g. Ag, Cu, Pb & Zn) were re-analyzed using an ore-grade, four-acid digestion and ICP-AES finish. Over limits for key elements: samples with >100 ppm silver, >10,000 ppm Cu, >10,000 ppm Pb and >10,000 ppm Zn. In addition to ALS Global laboratory QA/QC protocols, Sun Summit implements a rigorous internal QA/QC program that includes the insertion of duplicates, certified reference materials (standards prepared by an independent lab) and blanks into the sample stream. A total of 38 QA/QC samples, including 21 standards, were inserted in the field, representing 14.2% of the overall sample stream. There were no significant issues identified in either the internal or external QA/QC samples.

National Instrument 43-101 Disclosure

This news release has been reviewed and approved by Sun Summit’s Vice President Exploration, Ken MacDonald, P. Geo., a ‘Qualified Person’ as defined in National Instrument 43-101 Standards of Disclosure for Mineral Projects of the Canadian Securities Administrators. Some technical information contained in this release is historical in nature and has been compiled from public sources believed to be accurate. The historical technical information has not been verified by Sun Summit and may in some instances be unverifiable dependent on the existence of historical drill core and grab samples.

Community Engagement

Sun Summit is engaging with First Nations on whose territory our projects are located and is discussing their interests and identifying contract and work opportunities, as well as opportunities to support community initiatives. The Company looks forward to continuing to work with local and regional First Nations with ongoing exploration.

About the JD Project

The JD Project is located in the Toodoggone mining district in north-central British Columbia, a highly prospective deposit-rich mineral trend. The project covers an area of over 15,000 hectares and is in close proximity to active exploration and development projects, such as Thesis Gold’s Lawyers and Ranch projects, TDG Gold’s Baker-Shasta projects, Amarc Resource’s AuRORA project, Centerra’s Gold’s Kemess East and Underground projects, as well as the past-producing Kemess open pit copper-gold mine (Figure 5).

The project is 450 kilometres northwest of the city of Prince George, and 25 kilometres north of the Sturdee airstrip. It is proximal to existing infrastructure in place to support the past-producing Kemess mine, including roads and a hydroelectric power line.

The JD Project is in a favourable geological environment characterized by both high-grade epithermal gold and silver mineralization, as well as porphyry-related copper and gold mineralization. Some historical exploration, including drilling, geochemistry and geophysics, has been carried out on the property, however the project area is largely underexplored.

About Sun Summit

Sun Summit Minerals (TSXV: SMN,OTC:SMREF) (OTCQB: SMREF) is a mineral exploration company focused on the discovery, expansion and advancement of district scale gold and copper assets in British Columbia. The Company’s diverse portfolio includes the JD and Theory projects in the Toodoggone region of north-central B.C., and the Buck Project in central B.C.

Further details are available at www.sunsummitminerals.com.

References

1. Hawkins, P.A. (1998), 1997 Exploration Report on the Creek Zone for Antares Mining and Exploration Corporation and AGC Americas Gold Corporation, JD Property, Toodoggone River Area, Omineca Mining Division, Internal Report #98-065-1.

Link to Figures

Figure 1: https://wp-sunsummitminerals-2024.s3.ca-central-1.amazonaws.com/media/2025/09/SMN_JD_CZ007_20250903_Figure_1-scaled.jpg

Figure 2: https://wp-sunsummitminerals-2024.s3.ca-central-1.amazonaws.com/media/2025/09/SMN_JD_CZ007_20250903_Maps_Figure-2-scaled.jpg

Figure 3: https://wp-sunsummitminerals-2024.s3.ca-central-1.amazonaws.com/media/2025/09/JD_CZ_CZ007_V1_CorePhotos_V2_Figure_3-scaled.jpg

Figure 4: https://wp-sunsummitminerals-2024.s3.ca-central-1.amazonaws.com/media/2025/09/JD_CZ_CZ007_V1_CorePhotos_V2_Figure_4-scaled.jpg

Figure 5: https://wp-sunsummitminerals-2024.s3.ca-central-1.amazonaws.com/media/2025/09/SMN_JD_CZ007_20250903_V4_Figure-5.jpg

On behalf of the board of directors

Niel Marotta
Chief Executive Officer & Director
info@sunsummitminerals.com

Forward-Looking Information

Statements contained in this news release that are not historical facts may be forward-looking statements, which involve risks, uncertainties and other factors that could cause actual results to differ materially from those expressed or implied by such forward-looking statements. In addition, the forward-looking statements require management to make assumptions and are subject to inherent risks and uncertainties. There is significant risk that the forward-looking statements will not prove to be accurate, that the management’s assumptions may not be correct and that actual results may differ materially from such forward-looking statements. Accordingly, readers should not place undue reliance on the forward-looking statements. Generally forward-looking statements can be identified by the use of terminology such as ‘anticipate’, ‘will’, ‘expect’, ‘may’, ‘continue’, ‘could’, ‘estimate’, ‘forecast’, ‘plan’, ‘potential’ and similar expressions. Forward-looking statements contained in this press release may include, but are not limited to, the timing of and size and scope of the drill program at the JD property; the Company’s exploration plans, expectations and forecasts. These forward-looking statements are based on a number of assumptions which may prove to be incorrect which, without limiting the generality of the following, include: the Company’s ability to complete the drill program as currently contemplated; risks inherent in exploration activities; volatility and sensitivity to market prices; volatility and sensitivity to capital market fluctuations; and fluctuations in metal prices. The forward-looking statements contained in this news release are made as of the date hereof or the dates specifically referenced in this press release, where applicable. Except as required by applicable securities laws and regulation, Sun Summit disclaims any intention or obligation to update or revise any forward-looking statement, whether as a result of new information, future events or otherwise, except as required by applicable securities laws. All forward-looking statements contained in this press release are expressly qualified by this cautionary statement.

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

To view the source version of this press release, please visit https://www.newsfilecorp.com/release/265410