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Vancouver, British Columbia TheNewswire – November 13th, 2025 Prismo Metals Inc. (‘ Prismo ‘ or the ‘ Company ‘) (CSE: PRIZ,OTC:PMOMF) (OTCQB: PMOMF) is pleased to announce that further to its news release dated October 20, 2025 (the ‘ Initial News Release ‘), the Company has upsized and closed its previously announced non-brokered private placement of units of the Company (‘ Units ‘) at an issue price of $0.10 per Unit (the ‘Private Placement’ ). Due to strong investor demand, the Private Placement was increased from 12,500,000 Units to the issuance of 17,450,000 Units for gross proceeds of $1,745,000.

The Company also announced it has amended the terms of the warrants forming part of the Units (the ‘ Amendmen t’). As announced in the Initial News Release, each Unit was to consist of one common share of the Company (a ‘ Share ‘) and one-half of one common share purchase warrant of the Company (each whole warrant, a ‘ Warrant ‘). Each Warrant was to entitle the holder to purchase one Share for a period of thirty-six (36) months from the date of issuance at an exercise price of $0.175, subject to an acceleration expiry clause (the ‘ Acceleration Clause ‘), whereby if the Shares closed at or above $0.25 for ten (10) consecutive trading days on the Canadian Securities Exchange, the Company would have the right to accelerate the expiry date of the Warrants by issuing a news release announcing the accelerated Warrant term, pursuant to which the Warrants would expire on the 30 th calendar day after the date of such news release. As a result of the Amendment, each issued Unit now consists of one Share and one full Warrant, with each Warrant entitling the holder to purchase one Share for a period of thirty-six (36) months from the date of issuance at an exercise price of $0.175, without the Acceleration Clause.

The Company intends to use the net proceeds from the Private Placement primarily for drilling at its Silver King project and for general corporate purposes. There may be circumstances, however, where, for sound business reasons, a reallocation of funds may be necessary. The Company expects to accept additional subscriptions of Units in the coming days for an approximate amount of $125,000.

In connection with the closing of the Private Placement, the Company issued an aggregate of 919,960 finder’s warrants (the ‘Finder’s Warrants’ ) and paid finder’s commissions of $ 92,398 to certain qualified finders. Each Finder’s Warrant is exercisable for a period of twenty-four (24) months from the date of issuance to purchase one Share at a price of $0.10. In addition, the Company paid a cash fee of $15,000 to a financial advisor.

All securities issued or issuable in connection with the Private Placement are subject to a four-month hold period from the closing date under applicable Canadian securities laws, in addition to such other restrictions as may apply under applicable securities laws of jurisdictions outside Canada.

Multilateral Instrument 61-101

The Company has issued an aggregate of 303,275 Units pursuant to the Private Placement to certain ‘related parties’ of the Company (the ‘ Interested Parties ‘), in each case constituting, to that extent, a ‘related party transaction’ as defined under Multilateral Instrument 61-101 – Protection of Minority Securityholders in Special Transactions (‘ MI 61-101 ‘). The Company is exempt from the requirements to obtain a formal valuation and minority shareholder approval in connection with the participation of the Interested Parties in the Private Placement in reliance on sections 5.5(a) and 5.7(1)(a) of MI 61-101, as neither the fair market value of the Private Placement nor the securities issued in connection therewith, in so far as the Private Placement involves the Interested Parties, exceeds 25% of the Company’s market capitalization. The Company did not file a material change report more than 21 days before the expected closing of the Private Placement as the details of the Private Placement and the participation therein by the Interested Parties therein were not settled until recently and the Company wishes to close on an expedited basis for sound business reasons.

About Prismo Metals Inc.

Prismo (CSE: PRIZ,OTC:PMOMF) is mining exploration company focused on three silver projects (Palos Verdes, Silver King and Ripsey) and a copper project in Arizona (Hot Breccia).

Please follow @PrismoMetals on , , , Instagram , and

Prismo Metals Inc.

1100 – 1111 Melville St., Vancouver, British Columbia V6E 3V6

Contact:

Alain Lambert, Chief Executive Officer alain.lambert@prismometals.com

Gordon Aldcorn, President gordon.aldcorn@prismometals.com

Neither the Canadian Securities Exchange nor its Market Regulator (as that term is defined in the policies of the Canadian Securities Exchange) accepts responsibility for the adequacy or accuracy of this release.

Cautionary Note Regarding Forward-Looking Information

This release includes certain statements and information that may constitute forward-looking information within the meaning of applicable Canadian securities laws. Forward-looking statements relate to future events or future performance and reflect the expectations or beliefs of management of the Company regarding future events. Generally, forward-looking statements and information can be identified by the use of forward-looking terminology such as ‘intends’ or ‘anticipates’, or variations of such words and phrases or statements that certain actions, events or results ‘may’, ‘could’, ‘should’, ‘would’ or ‘occur’. This information and these statements, referred to herein as ‘forward‐looking statements’, are not historical facts, are made as of the date of this news release and include without limitation, statements regarding discussions of future plans, estimates and forecasts and statements as to management’s expectations and intentions with respect to, among other things, the intended use of any proceeds raised under the Private Placement.

These forward‐looking statements involve numerous risks and uncertainties and actual results might differ materially from results suggested in any forward-looking statements. These risks and uncertainties include, among other things, the potential inability of the Company to utilize the anticipated proceeds of the Private Placement as anticipated; and those risks set out in the Company’s public disclosure record on SEDAR+ ( www.sedarplus.com ) under the Company’s issuer profile .

Although management of the Company has attem pted to identify important factors that could cause actual results to differ materially from those contained in forward-looking statements or forward-looking information, there may be other factors that cause results not to be as anticipated, estimated or intended. There can be no assurance that such statements will prove to be accurate, as actual results and future events could differ materially from those anticipated in such statements. Accordingly, readers should not place undue reliance on forward-looking statements and forward-looking information. Readers are cautioned that reliance on such information may not be appropriate for other purposes. The Company does not undertake to update any forward-looking statement, forward-looking information or financial out-look that are incorporated by reference herein, except in accordance with applicable securities laws. We seek safe harbor.

Copyright (c) 2025 TheNewswire – All rights reserved.

Discovery of uranium mineralization in ideal geological setting, supported by regional radiometric anomaly, confirms large Rossing-style target

ReeXploration Inc. (TSXV: REE) (FSE: K2I0) (‘ReeXploration’ or the ‘Company’) is pleased to announce the identification of a significant new uranium exploration target at its Eureka Project (‘Eureka’ or the ‘Project’), located in the Erongo mining district, central Namibia. This new uranium target supports the Company’s broader focus on advancing critical-mineral opportunities in stable, mining-friendly jurisdictions.

HIGHLIGHTS:

• New Large-Scale Uranium Target Identified: Immediately southwest of the Eureka Dome, which hosts the Company’s rare earth element (‘REE’) resource and numerous REE targets.
• Strong Regional Radiometric Anomaly: Airborne data defines a 6.5 x 3.5 km zone characterized by high uranium and low thorium responses.
• Evidence of Widespread Uranium Mineralization: Uranium reported in shallow overburden samples from historical exploration, verified by recent scintillometer readings up to 1,500 counts per second (‘cps’).
• Uranium Discovered in Weathered Leucogranites: Field reconnaissance confirmed elevated uranium in occasionally outcropping leucogranites (‘alaskites’), with portable XRF semiquantitative values up to 853 ppm U.
• Along Trend of Namibia’s ‘Alaskite Alley’: Lies within the same structural corridor that hosts major uranium deposits — Rössing, Husab, Etango, Omaholo, and Norasa — which collectively contain more than 1 billion pounds of U₃O₈.
• Geological Setting Matches Rössing-Style Models: Key discovery criteria evident, including 1) proximity to the Welwitschia Lineament, 2) position on the flanks of a major basement dome, and 3) leucogranites intruded into reactive calc-silicate host rocks.

‘This uranium target, which is almost entirely covered by thin overburden, represents a promising exploration opportunity within one of the world’s most prolific uranium belts,’ commented Tolene Kruger, Senior Geologist for ReeXploration. ‘The geology, structural setting, and early results are consistent with the deposit models that led to the discovery of the major leucogranite-hosted uranium deposits within Namibia.’

Christopher Drysdale, Interim CEO for ReeXploration, added ‘The identification of this new target highlights the strong technical work completed by our exploration team and the expanded potential of the Eureka Project. As we continue to advance with our REE resource growth plan within the Eureka Dome, this extensive target immediately outside the Dome adds significant exploration upside and optionality for our shareholders, in one of the world’s most established critical minerals mining jurisdictions. We are looking forward to advancing exploration on our numerous REE targets and this newly identified uranium target, consistent with our strategy to discover significant critical mineral resources that contribute to secure, responsible supply chains.’

Expanded Discovery Potential – Large-Scale Rössing-Style Target

The identification of this target underscores the exceptional potential of the Eureka Project, which now includes a growing pipeline of REE targets alongside this newly recognized uranium opportunity. Review and field validation of government airborne radiometric data revealed extensive uranium anomalies situated off the southwestern margin of the Eureka Dome, which is host to the Company’s REE mineral resources and exploration targets. The government airborne radiometric data shows large-scale uranium anomalies 6.5 x 3.5 kilometres in extent with high uranium and low thorium – characteristic signature for Rössing-style targets (Figure 1).

Figure 1: Company license holding showing REE targets within the Eureka Dome, and high uranium anomalies outlined in red on uranium radiometric (government airborne radiometrics) backdrop. Insert: Thorium radiometric backdrop showing low thorium relative to the uranium anomalies.

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https://images.newsfilecorp.com/files/6102/274096_b3f40910c437995f_001full.jpg

Located Along Trend of Namibia’s Renowned Alaskite Alley

The new uranium target at Eureka is situated along trend of Namibia’s ‘Alaskite Alley’, a structural corridor within Namibia’s Central Zone of the Damara Belt that hosts multiple giant uranium deposits hosted within leucogranites, including Rössing, Husab, Etango, Omaholo and Norasa (Figure 2).

Figure 2: Regional satellite view showing the position of the uranium anomalies southwest of the Eureka Dome, and their proximity to the Welwitschia Lineament and other large uranium deposits in Alaskite Alley.

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https://images.newsfilecorp.com/files/6102/274096_b3f40910c437995f_002full.jpg

Key Geological Criteria Consistent with Major Uranium Deposits

The target exhibits all the key geological criteria consistent with the major uranium deposit models, including (Figure 3):

• Proximity to the Welwitschia Lineament – a major crustal-scale structure, central to ‘Alaskite Alley’, interpreted to have played a key role in localizing uranium-bearing leucogranite intrusions throughout the district.

• The Welwitschia Lineament is located immediately east of the new uranium target at Eureka.

• An Older Basement Dome – that provides the structural architecture for the emplacement of uranium-rich leucogranites around dome margins.

• The Eureka Dome is mapped as the same formation as the Rössing Dome (Etusis Formation).

• Reactive Contact Rocks – typically calc-silicate lithologies (metasediments) which act as chemical traps promoting uranium precipitation.

• Calc-silicates are mapped flanking the Eureka Dome (Arandis Formation).

• The Presence of Leucogranites – late-stage magmatic intrusions which host uranium mineralization in Rössing-style deposits.

• Significant leucogranites are interpreted to exist below the thin overburden at Eureka as sheeted dykes intercalated between calc-silicates, as evidenced by occasional weathered leucogranite outcrop.

Figure 3: Comparison between the major uranium deposits in Alaskite Alley and the airborne uranium anomalies southwest of the Eureka Dome.

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Initial Field Reconnaissance Supports Potential for Rössing-Style Deposit

Field spectrometer prospecting conducted by the Company has confirmed the regional scale of the airborne radiometric uranium anomalies. The anomalies relate to widespread uranium mineralization occurring within thin overburden, which is best visible where drainages have incised a regionally occurring gypcrete/calcrete horizon with anomalous values ranging from 300 to 1,500 counts per second (‘cps’) (Figure 4).

Figure 4: Photographs taken during reconnaissance field work and ground spectrometer survey within the anomalous areas.

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The uranium mineralization within the overburden is potentially indicative of extensive uranium mineralization within the underlying leucogranites, supported by (Figure 5):

1. Discovery of secondary uranium mineralization (carnotite) within weathered/leached leucogranites— pXRF semiquantitative values of up to 853 ppm U.

2. Abundant ‘smokey’ or irradiated quartz within the leucogranites.

3. Spectrometer evidence of uranium enrichment of weathered leucogranites where in contact with chemically-reactive calc-silicates.

Figure 5: Mineralized leucogranite found during reconnaissance field work and the ground spectrometer survey.

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Historical Work Focused on Shallow Overburden Mineralization

Although the target is on trend with Namibia’s Alaskite Alley, its position farther north, together with the thin overburden and the presence of calc-silicates belonging to the Arandis rather than the Khan Formation, likely contributed to the lack of focused historical exploration. Despite the highly favorable geological setting, the target appears to remain largely untested.

Historical uranium exploration at Eureka—outside of the main Eureka Dome and then held under EPL 3637—was primarily directed toward near-surface secondary uranium (carnotite) mineralization hosted within calcrete and gypcrete horizons. While historical work confirmed the presence of leucogranites intruding calc-silicate rocks, these potential bedrock sources were evidently not systematically drill-tested at any depth.

The work completed in 2009 consisted mainly of shallow pitting and percussion drilling (<5 m depth) designed to evaluate surface uranium enrichment in the search for calcrete-hosted (paleochannel-type) uranium deposits such as Langer Heinrich, leaving the primary leucogranite targets effectively untested. Across the broader Eureka license area, historical work included 100 prospecting pits (to 1.8 m depth, averaging 1.3 m) and 139 rotary air-blast (RAB) drill holes totaling only 803 m (i.e. average depth of only 5.8 m). Visible carnotite mineralization was reported in several pits, with uranium values up to 192 ppm U₃O₈ over 1.18 m, confirming uranium enrichment within the overburden and weathered bedrock. Preliminary, non-NI 43-101-compliant historical estimates indicated approximately 600,000 lbs U₃O₈ at 70 ppm within the overburden gycretes and calcretes (see Technical Disclosure below in reference to this historical resource estimate).

Despite best efforts, the Company has been unable to locate additional drill data or records. The summary descriptions provided in the available report suggest that systematic testing of deeper bedrock targets was never completed. This provides a significant opportunity to evaluate the potential for Rössing-style, leucogranite-hosted uranium mineralization beneath the thin overburden.

Drill Testing Warranted Below the Weathering Profile

Given the apparent shallow nature of the historical drilling, any testing of the underlying leucogranite units would have been very limited or non-existent, with exploration evidently focused on surface and near-surface mineralization within the overburden. The highly weathered nature of the limited leucogranite outcrop indicates that leaching has occurred near-surface, and as a result, leucogranites found at surface would not be expected to be mineralized other than possible secondary mineralization (carnotite) — as discovered from initial field reconnaissance. Drilling below the weathering profile is required to test for primary leucogranite-hosted mineralization (uraninite), typical of Rössing-style deposits.

Technical Disclosure

The historical exploration results and historical resource estimate summarized herein are considered historical in nature and have not been verified by the Company’s Qualified Person as defined under National Instrument 43-101 – Standards of Disclosure for Mineral Projects (‘NI 43-101’). These results, including the historical resource estimate, are sourced from Wartha, R.R. (2009). 2009 Annual Technical Report – EPL 3637 (Ancash Investment (Pty) Ltd.), prepared for Valencia Uranium (Pty) Ltd., December 18, 2009. The approximate historical resource estimate was calculated using an area of 1.5 million m² and an average mineralized thickness of 1 to 2 metres within the overburden gycretes and calcretes providing approximately 3.9 million tonnes of mineralization at 70 ppm, totaling in 600,000 lbs of U₃O₈. The historical resource categories used in the estimate do not conform to the current CIM Definition Standards and should not be compared directly to current mineral resource categories. The Company is not aware of any more recent mineral resource estimates for the Property. A Qualified Person has not completed sufficient work to verify the historical estimate or to classify it as a current mineral resource, and the Company is not treating the historical estimate as a current mineral resource. To verify and upgrade the historical estimate, additional work will be required, including data verification, review of historical drilling and sampling QA/QC, updated geological modeling, and completion of a new mineral resource estimate in accordance with NI 43-101 and CIM Definition Standards.

Field analysis of rock samples was carried out using a calibrated SciAps X-555 portable X-Ray Fluorescence (pXRF) analyzer. The instrument is capable of detecting uranium providing a rapid, preliminary, and semi-quantitative indication of uranium concentrations which is considered sufficiently reliable for initial reporting of initial field reconnaissance results. Samples are expected to be verified through uranium assay at an accredited laboratory.

Counts per second (‘cps’) results were collected using an RS-125 handheld gamma-ray spectrometer. The RS-125 measures natural radioactivity from potassium (K), uranium (U), and thorium (Th), providing real-time counts-per-second (cps) readings that assist in identifying zones of elevated radioactivity and guiding geological mapping and sampling programs. The cps measurements are qualitative in nature and should not be interpreted as equivalent to uranium concentrations obtained through laboratory analysis.

Qualified Person

Tolene Kruger, BSc. (Hons), M.Sc., is a consulting geologist and has reviewed and approved the scientific and technical information in this news release. Mrs. Kruger is registered as Professional Natural Scientist (Pr.Sci.Nat.) with the South African Council for Natural Science Professions (SACNASP, Reg. No.: 148182), and a Qualified Person for the purposes of National Instrument 43-101 – Standards of Disclosure for Mineral Projects. Ms. Kruger is not independent of the Company under NI 43-101.

About ReeXploration Inc.

ReeXploration (TSXV: REE) (FSE: K2I0) is a Canadian exploration company positioned to help meet surging global demand for secure, responsible supplies of critical minerals essential to the clean energy transition, advanced technologies and national defense. The company’s flagship Eureka Project in central Namibia hosts rare earth element (REE) mineralization in monazite, rich in NdPr magnet metals, with bench-scale testing confirming production of a clean, Western-standard concentrate. Supported by a Namibia-based technical team and guided by global critical minerals experts, ReeXploration is advancing discovery-led growth for rare earth elements (REEs) and other critical minerals, building a credible, ESG-aligned platform positioned to benefit from the global race to diversify and secure responsible supply chains.

Caution Regarding Forward-Looking Information

This press release may contain forward-looking information. This information is based on current expectations and assumptions (including assumptions relating to general economic and market conditions) that are subject to significant risks and uncertainties that are difficult to predict. Actual results may differ materially from results suggested in any forward-looking information. ReeXploration does not assume any obligation to update forward-looking information in this release, or to update the reasons why actual results could differ from those reflected in the forward-looking information unless and until required by securities laws applicable to ReeXploration. Additional information identifying risks and uncertainties is contained in the filings made by ReeXploration with Canadian securities regulators, which filings are available at www.sedarplus.ca.

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in 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/274096

Osisko Metals Incorporated (the ‘ Company or ‘ Osisko Metals ‘) ( TSX: OM,OTC:OMZNF ; OTCQX: OMZNF ; FRANKFURT: 0B51 ) is pleased to announce new drill results from the Gaspé Copper Project, located in the Gaspé Peninsula of Eastern Québec.

New analytical results are presented below (see Table 1), including 35 mineralized intercepts from ten new drill holes. Infill intercepts are located inside the 2024 MRE model ( see November 14, 2024 news release ), and are focused on upgrading inferred mineral resources to measured or indicated categories, as applicable. Expansion intercepts are located outside the 2024 MRE model and may potentially lead to additional resources that will be classified appropriately within the next MRE update. Some of the reported intercepts have contiguous shallower infill as well as deeper expansion (noted on Table 1 below as ‘Both’). Maps showing hole locations are available at www.osiskometals.com .

Highlights:

• Drill hole 30-1128
  • 330.6 metres averaging 0.46% Cu (0.49% CuEq – expansion)
• Drill hole 30-1115
  • 33.0 metres averaging 1.28% Cu (1.36% CuEq – expansion)
• Drill hole 30-1117
  • 779.0 metres averaging 0.26% Cu (0.34% CuEq – infill and expansion)
• Drill hole 30-1118
  • 555.9 metres averaging 0.20% Cu (0.26% CuEq – infill)
• Drill hole 30-1123
  • 313.5 metres averaging 0.23% Cu (0.28% CuEq – infill and expansion)
  • 220.5 metres averaging 0.20% Cu (0.30% CuEq – expansion)
• Drill hole 30-1125
  • 293.0 metres averaging 0.23% Cu (0.30% CuEq – expansion)
• Drill hole 30-1126
  • 804.0 metres averaging 0.24% Cu (0.31% CuEq – infill and expansion)
• Drill hole 30-1130
  • 347.7 metres averaging 0.24% Cu (0.29% CuEq – infill)
• Drill hole 30-1131
  • 714.0 metres averaging 0.21% Cu (0.27% CuEq – both)

Table 1: Infill and Expansion Drilling Results

* See explanatory notes below on copper equivalent values and Quality Assurance/Quality Controls.
** ‘Both’ indicates drill holes that have contiguous shallower infill as well as deeper expansion intercepts.

Discussion

Drill hole 30-1115, located on the eastern margin of the 2024 MRE model, did not intersect significant mineralization to a depth of 499 metres, but cut relatively high grades of 33.0 metres averaging 1.28 % Cu, 8.89 g/t Ag within the C Zone skarn horizon (expansion), as well as 56.1 metres averaging 0.59 % Cu and 3.52 g/t Ag, above the E Zone skarn horizon. The hole ended in an E zone stope where massive sulfides and high-grade skarns were previously mined.

Drill hole 30-1117, located on the western flank of Copper Mountain, cut three mineralized intervals including 779.0 metres averaging 0.26 % Cu, 1.68 g/t Ag and 0.019% Mo (which includes 312.5 metres of depth expansion), extending mineralization in this area to a vertical depth of 991 metres.

Drill hole 30-1118, located near the southern lip of the Copper Mountain open pit, cut two mineralized intervals including 555.9 metres averaging 0.20 % Cu, 1.00 g/t Ag and 0.008% Mo (infill) as well as a deeper intersection of 151.5 metres averaging 0.11 % Cu, 0.77 g/t Ag and 0.027% Mo (expansion), extending mineralization in this area to a vertical depth of 776 metres.

Drill hole 30-1123, located on the southern flank of Copper Mountain, cut three mineralized intersections, 14 to 36 metres thick and distributed in ‘layer cake’ fashion from surface to a vertical depth of 137 metres, followed by 313.5 metres averaging 0.23 % Cu, 1.84 g/t Ag and 0.012% Mo (infill and expansion) and then by 220.5 metres averaging 0.20 % Cu, 1.63 g/t Ag and 0.024% Mo (expansion), extending mineralization in this area to a vertical depth of 774 metres.

Drill hole 30-1125, located approximately 200 metres south of 30-1118, near Copper Brook, cut five mineralized intersections, 30 to 293 metres thick and distributed in ‘layer cake’ fashion from surface to a vertical depth of 936 metres, including 184.2 metres averaging 0.20 % C and 0.97 g/t Ag (infill) as well as 293.0 metres averaging 0.23 % Cu, 1.26 g/t Ag and 0.019% Mo (expansion).

Drill hole 30-1126, located on the western flank of Copper Mountain, cut two mineralized intervals including 804.0 metres averaging 0.24 % Cu, 1.48 g/t Ag and 0.016% Mo (which includes 399.4 metres of depth expansion), extending mineralization in this area to a vertical depth of 1033 metres.

Drill hole 30-1127, located near the eastern margin of the 2024 MRE model, cut eight intersections of mineralization, 17 to 45 metres thick and distributed in ‘layer cake’ fashion from surface to a vertical depth of 891 metres, confirming the near limit of the 2024 MRE model at this location.

Drill hole 30-1128, located 100 metres south of the southern margin of the 2024 MRE model, cut four mineralized intersections, all expansion outside the current resource model, including 115.5 metres averaging 0.44 % Cu and 3.67 g/t Ag within (and above) the B Zone skarn horizon, as well as 330.6 metres averaging 0.46 % Cu and 4.33 g/t Ag from the top of the C Zone skarn to well below (120 metres) the E zone horizon. This latter intersection included a high-grade interval of 14.5 metres averaging 2.51 % Cu and 24.9 g/t Ag, located in a mineralized vein/massive sulfide zone about 20 metres above the E Zone horizon. This is a new mineralized zone not previously identified at Gaspé Copper and its extent is presently unknown.

Drill hole 30-1130, located on top of Copper Mountain near the center of the 2024 MRE model, cut two significant mineralized intervals including 347.7 metres averaging 0.24 % Cu, 2.14 g/t Ag and 0.010% Mo, followed by 277.5 metres averaging 0.26% Cu, 1.51 g/t Ag and 0.023% Mo, extending mineralization in this area to a vertical depth of 874 metres.

Drill hole 30-1131, located near the southern lip of the Copper Mountain open pit adjacent to 30-1118, was drilled at a 78-degree dip towards the north and it intersected 741 metres of continuous mineralization from surface, averaging 0.21 % Cu, 1.11 g/t Ag and 0.015% Mo (infill). This hole confirmed mineralization in this area to a vertical depth of 725 metres, ending in the porphyry intrusion core of the Copper Mountain deposit.

Mineralization at Gaspé Copper is of porphyry copper/skarn type and occurs as disseminations and stockworks of chalcopyrite with pyrite or pyrrhotite and minor bornite and molybdenite. One prograde and at least five retrograde vein/stockwork mineralizing events have been recognized at Copper Mountain, which overprint earlier, bedding replacement skarn and porcellanite-hosted mineralization throughout the Gaspé Copper system. Porcellanite is a historical mining term used to describe bleached, pale green to white potassic-altered hornfels. Subvertical stockwork mineralization dominates at Copper Mountain whereas prograde bedding-parallel mineralization, that is mostly stratigraphically controlled, dominates in the area of lower Copper Mountain, Needle Mountain, Needle East, and Copper Brook. High molybdenum grades (up to 0.5% Mo) were locally obtained in both the C Zone and E Zone skarns away from Copper Mountain.

The 2022 to 2024 Osisko Metals drill programs were focused on defining open-pit resources within the Copper Mountain stockwork mineralization ( see May 6, 2024 MRE press release ). Extending the resource model south of Copper Mountain into the poorly-drilled prograde skarn/porcellanite portion of the system subsequently led to a significantly increased resource, mostly in the Inferred category ( see November 14, 2024 MRE press release ).

The current drill program is designed to convert the November 2024 MRE to Measured and Indicated categories, as well as test the expansion of the system deeper into the stratigraphy and laterally to the south and southwest towards Needle East and Needle Mountain respectively. The November 2024 MRE was limited at depth to the base of the L1 skarn horizon (C Zone), and all mineralized intersections below this horizon represent potential depth extensions to the deposit, to be included in the next scheduled MRE update in Q1 2026.

Most holes are being drilled sub-vertically into the altered calcareous stratigraphy which dips 20 to 25 degrees to the north. The L1 (C Zone) the L2 (E Zone) skarn/marble horizons were intersected in most holes, as well as intervening porcellanites that host the bulk of the disseminated copper mineralization.

Table 2: Drill hole locations

Explanatory note regarding copper-equivalent grades

Copper Equivalent grades are expressed for purposes of simplicity and are calculated taking into account: 1) metal grades; 2) estimated long-term prices of metals: US$4.25/lb copper, $20.00/lb molybdenum, and US$24/oz silver; 3) estimated recoveries of 92%, 70%, and 70% for Cu, Mo, and Ag respectively; and 4) net smelter return value of metals as percentage of the price, estimated at 86.5%, 90.7%, and 75.0% for Cu, Mo, and Ag respectively.

Qualified Person

The scientific and technical content of this news release has been reviewed and approved by Mr. Bernard-Olivier Martel, P. Geo. (OGQ 492), an independent ‘qualified person’ as defined by National Instrument 43-101 – Standards of Disclosure for Mineral Projects (‘NI 43-101’).

Quality Assurance / Quality Control

Mineralized intervals reported herein are calculated using an average 0.12% CuEq lower cut-off over contiguous 20-metre intersections (shorter intervals as the case may be at the upper and lower limits of reported intervals). Intervals of 10 metres or less are not reported unless indicating significantly higher grades .   True widths are estimated at 90 – 92% of the reported core length intervals.

Osisko Metals adheres to a strict QA/QC program for core handling, sampling, sample transportation and analyses, including insertion of blanks and standards in the sample stream. Drill core is drilled in HQ or NQ diameter and securely transported to its core processing facility on site, where it is logged, cut and sampled. Samples selected for assay are sealed and shipped to ALS Canada Ltd.’s preparation facility in Sudbury. Sample preparation details (code PREP-31DH) are available on the ALS Canada website. Pulps are analyzed at the ALS Canada Ltd. facility in North Vancouver, BC. All samples are analyzed by four acid digestion followed by both ICP-AES and ICP-MS for Cu, Mo and Ag.

About Osisko Metals

Osisko Metals Incorporated is a Canadian exploration and development company creating value in the critical metals sector, with a focus on copper and zinc. The Company acquired a 100% interest in the past-producing Gaspé Copper mine from Glencore Canada Corporation in July 2023. The Gaspé Copper mine is located near Murdochville in Québec ‘ s Gaspé Peninsula. The Company is currently focused on resource expansion of the Gaspé Copper system, with current Indicated Mineral Resources of 824 Mt averaging 0.34% CuEq and Inferred Mineral Resources of 670 Mt averaging 0.38% CuEq (in compliance with NI 43-101). For more information, see Osisko Metals’ November 14, 2024 news release entitled ‘Osisko Metals Announces Significant Increase in Mineral Resource at Gaspé Copper’. Gaspé Copper hosts the largest undeveloped copper resource in eastern North America, strategically located near existing infrastructure in the mining-friendly province of Québec.

In addition to the Gaspé Copper project, the Company is working with Appian Capital Advisory LLP through the Pine Point Mining Limited joint venture to advance one of Canada ‘ s largest past-producing zinc mining camps, the Pine Point project, located in the Northwest Territories. The current mineral resource estimate for the Pine Point project consists of Indicated Mineral Resources of 49.5 Mt averaging 5.52% ZnEq and Inferred Mineral Resources of 8.3 Mt averaging 5.64% ZnEq (in compliance with NI 43-101). For more information, see Osisko Metals ‘ June 25, 2024 news release entitled ‘Osisko Metals releases Pine Point mineral resource estimate: 49.5 million tonnes of indicated resources at 5.52% ZnEq’. The Pine Point project is located on the south shore of Great Slave Lake, NWT, close to infrastructure, with paved road access, an electrical substation and 100 kilometres of viable haul roads.

For further information on this news release, visit www.osiskometals.com or contact:

Don Njegovan, President
Email: info@osiskometals.com
Phone: (416) 500-4129

Cautionary Statement on Forward-Looking Information

This news release contains ‘forward-looking information’ within the meaning of applicable Canadian securities legislation based on expectations, estimates and projections as at the date of this news release. Any statement that involves predictions, expectations, interpretations, beliefs, plans, projections, objectives, assumptions, future events or performance (often, but not always, using phrases such as ‘expects’, or ‘does not expect’, ‘is expected’, ‘interpreted’, ‘management’s view’, ‘anticipates’ or ‘does not anticipate’, ‘plans’, ‘budget’, ‘scheduled’, ‘forecasts’, ‘estimates’, ‘potential’, ‘feasibility’, ‘believes’ or ‘intends’ or variations of such words and phrases or stating that certain actions, events or results ‘may’ or ‘could’, ‘would’, ‘might’ or ‘will’ be taken, occur or be achieved) are not statements of historical fact and may be forward-looking information and are intended to identify forward-looking information. This news release contains forward-looking information pertaining to, among other things: the tax treatment of the FT Units; the timing of incurring the Qualifying Expenditures and the renunciation of the Qualifying Expenditures; the ability to advance Gaspé Copper to a construction decision (if at all); the ability to increase the Company’s trading liquidity and enhance its capital markets presence; the potential re-rating of the Company; the ability for the Company to unlock the full potential of its assets and achieve success; the ability for the Company to create value for its shareholders; the advancement of the Pine Point project; the anticipated resource expansion of the Gaspé Copper system and Gaspé Copper hosting the largest undeveloped copper resource in eastern North America.

Forward-looking information is not a guarantee of future performance and is based upon a number of estimates and assumptions of management, in light of management’s experience and perception of trends, current conditions and expected developments, as well as other factors that management believes to be relevant and reasonable in the circumstances, including, without limitation, assumptions about: the ability of exploration results, including drilling, to accurately predict mineralization; errors in geological modelling; insufficient data; equity and debt capital markets; future spot prices of copper and zinc; the timing and results of exploration and drilling programs; the accuracy of mineral resource estimates; production costs; political and regulatory stability; the receipt of governmental and third party approvals; licenses and permits being received on favourable terms; sustained labour stability; stability in financial and capital markets; availability of mining equipment and positive relations with local communities and groups. Forward-looking information involves risks, uncertainties and other factors that could cause actual events, results, performance, prospects and opportunities to differ materially from those expressed or implied by such forward-looking information. Factors that could cause actual results to differ materially from such forward-looking information are set out in the Company’s public disclosure record on SEDAR+ (www.sedarplus.ca) under Osisko Metals’ issuer profile. Although the Company believes that the assumptions and factors used in preparing the forward-looking information in this news release are reasonable, undue reliance should not be placed on such information, which only applies as of the date of this news release, and no assurance can be given that such events will occur in the disclosed time frames or at all. The Company disclaims any intention or obligation to update or revise any forward- looking information, whether as a result of new information, future events or otherwise, other than as required by law.

Neither the TSX Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Exchange) accept responsibility for the adequacy or accuracy of this news release. No stock exchange, securities commission, or other regulatory authority has approved or disapproved the information contained herein.

Photos accompanying this announcement are available at:
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Questcorp Mining Inc. (CSE: QQQ,OTC:QQCMF) (OTCQB: QQCMF) (FSE: D910) (the ‘Company’ or ‘Questcorp’) is pleased to announce that Sorbie Bornholm LP (‘Sorbie’), a UK Investment Fund, has undertaken an initial investment in Questcorp Mining Inc. (CSE: QQQ,OTC:QQCMF) (OTCQB: QQCMF) (FSE: D910) (‘Questcorp’ or the ‘Company’). The gross amount of the investment is CAD$2,000,000. The funds will go toward advancing Questcorp’s ongoing exploration and development programs at its flagship La Union Gold and Silver Project in Sonora, Mexico, and its North Island Copper Property on Vancouver Island, British Columbia, and for general working capital purposes.

Reflecting on the new partnership, President & CEO, Saf Dhillon, commented:

‘We are incredibly pleased to have secured this strategic investment from Sorbie Bornholm, a respected international institutional investor. This financing provides us with the flexibility to accelerate exploration across our key assets in Mexico and British Columbia. We view Sorbie’s participation as a strong vote of confidence in Questcorp’s team, vision, and long-term potential to deliver value through discovery and development.’

Whitney Kofford, Managing Director of Sorbie Bornholm LP, added:

‘We are delighted to welcome Questcorp Mining Inc. as a new partner and portfolio company. Our decision to invest reflects our enormous confidence in Questcorp’s leadership. And in turn, by entering into a Sharing Agreement, Questcorp’s leadership signals strong conviction in their ability to execute and grow value for all stakeholders. Sorbie’s Sharing Agreement is designed to align interests towards growth and provide companies with consistent capital that rewards operational success and share price appreciation. We trust Questcorp will use the capital support to systematically unlock long-term value for all shareholders, and we look forward to sharing in their great upside potential.’

About Sorbie Bornholm

Sorbie Bornholm LP is a global investment firm that provides funding for ongoing business objectives to listed micro, small and mid-cap growth companies. We focus on public equity investments in companies that are looking to expand and on management teams with a clear growth strategy. Our extensive experience allows us to invest in most industries in order to provide supportive, longer-term capital that rewards company growth.

Since 2000, Sorbie Bornholm LP founder Greg Kofford has perfected the ‘Sorbie-Strategy’, utilizing a sharing agreement that supports management and rewards growth. This unique approach has now been used in over 50 investments – with many of those resulting in the companies receiving more cash than the original offering proceeds – without having to issue any additional shares.

Sorbie Bornholm’s core values drive who we are and how we invest. We are committed to developing long-term relationships with select listed public companies and their brokers & advisers. We focus on providing supportive, longer-term capital that rewards growth. We invest to make a difference, to become a valued partner and to be a shareholder of choice. It’s important to us that we succeed together.

To see if the Sorbie-Strategy is right for your company, please contact Sorbie Bornholm:

Whitney Kofford, Managing Director
+1-801-554-5889
whitney@sorbiebornholm.com https://sorbiebornholm.co.uk/

About Questcorp Mining Inc.

Questcorp Mining Inc. is engaged in the business of the acquisition and exploration of mineral properties in North America, with the objective of locating and developing economic precious and base metals properties of merit. The Company holds an option to acquire an undivided 100% interest in and to mineral claims totaling 1,168.09 hectares comprising the North Island Copper Property, on Vancouver Island, British Columbia, subject to a royalty obligation. The Company also holds an option to acquire an undivided 100% interest in and to mineral claims totaling 2,520.2 hectares comprising the La Union Project located in Sonora, Mexico, subject to a royalty obligation.

This news release includes certain ‘forward-looking statements’ under applicable Canadian securities legislation. Forward-looking statements include, but are not limited to, statements with respect to the intended use of proceeds from the Offering. Forward-looking statements are necessarily based upon a number of estimates and assumptions that, while considered reasonable, are subject to known and unknown risks, uncertainties, and other factors which may cause the actual results and future events to differ materially from those expressed or implied by such forward-looking statements. Such factors include, but are not limited to: the ability of Riverside to secure geophysical contractors to undertake orientation surveys and follow up detailed survey to confirm and enhance the drill targets as contemplated or at all, general business, economic, competitive, political and social uncertainties, uncertain capital markets; and delay or failure to receive board or regulatory approvals. There can be no assurance that the geophysical surveys will be completed as contemplated or at all and that such statements will prove to be accurate, as actual results and future events could differ materially from those anticipated in such statements. Accordingly, readers should not place undue reliance on forward-looking statements. The Company disclaims any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or otherwise, except as required by law.

To view the source version of this press release, please visit https://www.newsfilecorp.com/release/273793

(TheNewswire)

Vancouver, British Columbia TheNewswire – November 10, 2025 Juggernaut Exploration Ltd (JUGR.V) (OTCPK: JUGRF) (FSE: 4JE) ( the ‘Company’ or ‘Juggernaut’) is excited to announce that detailed mapping and sampling have confirmed that the gold-rich Big Mac Zone, Whopper Zone and Gold Dome Zone all form part of the 22 Km 2 district-scale Eldorado System that remains wide open where grab samples assayed up to 263.70 gt AuEq or 8.48 ozt AuEq and channel cuts assayed up to 4.89 gt AuEq over 5.21 m from >400 mineralized veins that are up to 10 m wide hosted in shear zones up to 50 m wide, and are exposed on surface for >1 km with >1 km of vertical relief, remains open and is drill ready on the Big One property (the ‘Property’), Golden Triangle, British Columbia. In addition, based on excellent assay results, the Company has acquired additional claims and expanded the Gold Swarm discovery area of strong gold potential from 1 km 2 to 3 km 2 and 700 m of vertical relief and remains open, effectively tripling this area of strong gold potential, where grab samples assayed up to 231.81 gt AuEq or 7.45 ozt AuEq and channel cuts assayed up to 4.51 gt AuEq over 4.36 m that remains open and is drill ready. The Big One discovery is located in an area of recent glacial and snowpack abatement adjacent to the Tier 1 gold-rich porphyry systems, the likes of Galore Creek. The 100% controlled Big One property covers 39,271 hectares of geological terrane with tremendous additional discovery potential.

Link to map with samples > 1 g/t AuEq

Big One Gold Rich District Scale System Highlights:

• The district-scale Eldorado System covers an area ~half the size of the Island of Manhattan (22 km ) that remains wide open where grab samples assayed up to 263.70 g/t AuEq or 8.48 oz/t AuEq and channel cuts assayed up to 4.89 g/t AuEq over 5.21 m from 400 mineralized veins that remain open and are up to 10 m wide, the equivalent to ~3-story building, hosted in shear zones up to 50 m wide, comparable to a 15-story building, and are exposed on surface for 500 m, or 5 football fields, with 1 km of vertical relief, the height of 2.5 Empire State Buildings.

Link to Gold Dome Figure

Link to Whopper Zone Figure

• The Gold Swarm Area of strong gold potential has been expanded from 1 km to 3 km , equivalent to more than the downtown core of Vancouver B.C, with 700 m of vertical relief and remains wide open, with 100 veins up to 4.5 m wide, the equivalent of a 1.5-story building, and exposed on surface for 200 m equivalent to 2 football fields and remain open containing grab samples that assayed up to 231.81 g/t AuEq or 7.45 oz/t AuEq a nd channel cuts that assayed up to 4.51 g/t AuEq over 4.36 m. The Gold Swarm Area is drill ready.

Link to Goldswarm Figure

• 41% (219 samples out of 527) collected within the Eldorado System in 2024 and 2025 assayed 1 g/t AuEq; 65% (28 samples out of 43) collected withing the Gold Swarm Zone in 2024 and 2025 assayed 1 g/t AuEq.

• Gold samples up to 256.60 g/t or 8.25 oz/t, silver samples up 2810 g/t or 90.34 oz/t, and copper samples up to 14.40 % were collected on Big One.

• Detailed mapping has confirmed common orientations as well as similar geochemical signatures and textures of the gold-mineralized veins along the 15 km Highway of Gold corridor surrounding the snowcap of Deeker Glacier, strongly indicating that the gold-rich mineralization found throughout is all part of one huge district-scale gold system that remains wide open.

• The polymetallic veins, alteration signature, geochemical pathfinder element signature, and geophysical anomalies strongly indicate the presence of a large common buried gold-silver-copper rich porphyry feeder source or similar magmatic source or sources at depth responsible for the extensive high-grade veining confirmed on surface over 22 km

• The company recently received a 5-year property-wide advanced exploration drill permit.

• Detailed geological and structural mapping has been completed on the reported drill targets in order to define 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 km2 on the Eldorado System and Gold Swarm Zone encompassing all of the maiden drill targets. The data will be used to support modelling and define targeting 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.

• Multiple drill-ready targets have been confirmed and are planned to be tested in the fully funded inaugural drill program and include but are not limited to: the 22 km Eldorado System hosting the Gold Dome Zone where grab samples assayed up to 263.70 g/t AuEq or 8.48 oz/t AuEq; the Big Mac Zone where grab samples assayed up to 113.92 g/t AuEq or 3.66 oz/t AuEq; the Whopper Zone where grab samples assayed up to 43.94 g/t AuEq or 1.41 oz/t AuEq; and the Gold Swarm Area where grab samples assayed up to 231.81 g/t AuEq or 7.45 oz/t AuEq.

• Juggernaut is working in consultation with the Tahltan First Nation and the local community and is committed to maintaining respectful and collaborative relationships. As we advance exploration on our project, we will continue working closely with the Tahltan First Nation and all the local stakeholders and regulatory agencies to ensure our activities create long-term value and reflect community priorities.

Dan Stuart, President and CEO of Juggernaut Exploration states: ‘With a district-scale discovery of this magnitude host to so many large gold-rich veins and shears exposed on surface that rise above the valley floor for >1 km we are likely only seeing the tip of the iceberg on this mountain of gold. We look forward to the fully funded maiden drill program on this remarkable gold discovery with much anticipation. The best is yet to come!’

Manuele Lazzarotto, PhD, Chief Geologist of Juggernaut Exploration, states: ‘With the advanced exploration permit in hand, we look forward to unlocking the full potential of the Big One gold discovery in the third dimension during the inaugural drill program. Once we receive, compile, and interpret all the deliverables from the detailed and regional mapping, UAV orthophotos survey, and LiDAR survey, the same team responsible for the Tier 1 Surebet gold discovery will design and execute the maiden drill program. Obvious opportunities with the scale and grades seen on Big One are extremely rare, and we have clearly barely begun to scratch the surface. The team looks forward to testing this remarkable discovery at depth.’

Table 1: Samples from 2024-2025 with assays >1 g/t AuEq

The Big One property is situated in a region that is well known for hosting Tier 1 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.

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.

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 and Chief Executive Officer

Tel: (604)-559-8028

www.juggernautexploration.com

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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.

FORWARD LOOKING STATEMENT

Certain disclosures 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.

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