CanAlaska Acquires High-Grade Nickel Deposit in Thompson Nickel Belt, Manitoba

CanAlaska Acquires High-Grade Nickel Deposit in Thompson Nickel Belt, Manitoba

Mel Deposit Contains Historical Indicated Resource Estimate of 82.5 Million Pounds Nickel at 0.875% Grade

Property Located Within 25 Kilometres of Vale's Thompson Mine and Mill Complex

CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7N) ("CanAlaska or the "Company") is pleased to announce that B. Riley Farber Inc., in its capacity as Trustee in Bankruptcy of the property, assets and undertakings of Victory Nickel Inc, has accepted CanAlaska's offer to acquire the Mel Nickel Deposit and surrounding mineral claims. The acquisition provides the Company with 100% ownership of the mineral lease that hosts the Mel Deposit, as well as ten mineral claims covering a total of 2,613 hectares in the Thompson Nickel Belt in Manitoba (Figure 1). The Mel project claims are contiguous with the Company's 100% owned Hunter and Strong projects.

CanAlaska CEO, Cory Belyk, comments, "For CanAlaska, the acquisition of the high-grade Mel nickel deposit and its surrounding exploration claims in the north Thompson Nickel Belt region compliments the Company's existing nickel assets perfectly. It provides the Company with a 100%-owned and large nickel resource in the 5th largest sulphide nickel belt in the world near Vale's Thompson operation. This acquisition further positions CanAlaska's district-scale nickel assets, now over 40,000 hectares total, as a front-runner among global nickel exploration portfolio's that will allow the Company to attract outside investment in a strengthening nickel market. New sources of nickel supply are scarce and demand is quickly growing as the world continues to electrify toward a carbon-free energy future."

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Figure 1 – Mel Project Location
 
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STRUCTURE OF THE DEAL

CanAlaska will acquire 100% of the Mel Deposit lease and surrounding claims by paying CDN$300,000 and issuing 2,000,000 common shares of CanAlaska, subject to TSX Venture Exchange approval. The shares will be subject to a statutory 4 month and a day hold period from the closing date (the "Hold Period") under applicable securities laws. In addition, the parties have agreed to voluntary resale restrictions thereafter with 25% (500,000) of the shares released from resale restrictions after the expiry of the Hold Period and the balance being released in three tranches of 500,000 on each of the dates that is 2, 4 and 6 months after the expiry date of the Hold Period. Notwithstanding the foregoing, the Trustee will have the right to sell, transfer or otherwise dispose of all (but not less than all) of the shares in a block trade at any time in its sole discretion after the expiry date of the Hold Period. CanAlaska has paid 15% of the consideration to the Trustee upon their acceptance of the offer. The balance of the purchase price will be paid and the acquisition completed upon execution of a definitive agreement and receipt of TSX Venture Exchange approval.

About the Mel Deposit and Project

The 100%-owned Mel property is located within 25 kilometres of Vale Canada Limited's processing facilities in Thompson, Manitoba. The property consists of 10 claims and one mineral lease for a total of 2,613 hectares. The mineral lease contains the Mel deposit, which has a historical indicated resource estimate of 4.3 million tonnes at 0.875% nickel for 82.5 million pounds of contained nickel and an inferred resource estimate of 1.0 million tonnes at 0.839% nickel for 18.7 million pounds of contained nickel (Table 1). The Company believes the Mel property is underexplored, with previous focus being mostly on the immediate Mel lease and deposit.

Table 1 - Historical Resource Estimate For Mel Deposit

CategoryTonnes% NickelContained Nickel (lbs)
Indicated4,279,0000.87582,520,515
Inferred1,010,0000.83918,676,476
Notes:
- See "Technical Report on the Mel Deposit, Northern Manitoba" prepared for Victory Nickel Inc. by Shahé Naccashian (P.Geo.) of Wardrop Engineering Inc. dated March 9, 2007
- Historical resource estimate calculated using a 0.5% nickel cut-off.

 

The Mel deposit was discovered by Inco in 1961 and was subsequently explored between 1961 and 1971. Between 1999 and 2004, Inco completed subsequent drill programs on the Mel project. Victory Nickel acquired the property in 2007 and completed a resource estimate (Table 1) based on 296 drillholes, 126 of which define the deposit. Subsequent work on the property and mineral lease by Victory Nickel included additional drilling in 2007 and 2011, and baseline environmental studies in 2012.

The Mel deposit strikes ~345˚ for a distance of 1,500 m, dips 70˚ - 80˚ east, and extends 46 - 183 metres from surface to a depth of 825 metres (Figure 2). The mineralization is characterized by nickel-bearing massive and stringer sulfides within and in contact with ultramafic intrusions. The sulfides are dominantly pyrrhotite with lesser amounts of pentlandite and chalcopyrite. Folded, continuous to discontinuous high-grade nickel-bearing sulfide layers up to 15 m thick (horizontal) are located within a broader mineralized zone with a thickness exceeding 30 metres. Additional drilling in 2011, intersected down-dip extensions of the deposit at depths of 165 to 350 metres, highlighted by 13.71 metres at 0.96% nickel, including 1.2 metres at 2.64% nickel in drill hole M-11-09.

The Mel property and deposit is subject to a Vale 10% net profits royalty. The Mel deposit contains a milling agreement with Vale at cash cost plus 5%, provided that the product meets Vale's specifications, and that Vale has sufficient mill capacity.

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Figure 2 – Mel Deposit Mineralized Envelope From Historical Resource Estimate
 
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The Mel deposit contains a historical resource estimation completed in compliance with the CIM Mineral Resource and Mineral Reserve definitions referred to in NI 43-101, Standards and Disclosure for Mineral Projects, at the time of publication. It also involved the preparation of a Technical Report as defined in NI 43-101, and in compliance with Form 43-101F1. The historical resource was presented in the "Technical Report on the Mel Deposit, Northern Manitoba" prepared for Victory Nickel Inc. by Shahé Naccashian (P.Geo.) of Wardrop Engineering Inc. dated March 9, 2007. The historical resource was calculated using the interpolation methods of nearest neighbour, inverse distance squared, and ordinary kriging. The methods were validated by comparison of global mean grades, visual review of coded block grades, and swath plots. Ordinary kriging methodology was selected for grade estimation on the deposit. The historical resource was completed in the local universal INCO grid (grid 11), that measures in feet. A qualified person with the Company has not done sufficient work to classify the historical estimate as current mineral resources or mineral reserves. The Company is not treating the historic estimate as current mineral reserves or mineral resources.

About CanAlaska Uranium

CanAlaska Uranium Ltd. (TSXV: CVV) (OTCQX: CVVUF) (FSE: DH7N) holds interests in approximately 300,000 hectares (750,000 acres), in Canada's Athabasca Basin - the "Saudi Arabia of Uranium." CanAlaska's strategic holdings have attracted major international mining companies. CanAlaska is currently working with Cameco and Denison at two of the Company's properties in the Eastern Athabasca Basin. CanAlaska is a project generator positioned for discovery success in the world's richest uranium district. The Company also holds properties prospective for nickel, copper, gold and diamonds. For further information visit www.canalaska.com.

The qualified technical person for this news release is Nathan Bridge, MSc., P.Geo., CanAlaska's Vice President, Exploration.

On behalf of the Board of Directors
"Cory Belyk"
Cory Belyk, P.Geo., FGC
CEO, Executive Vice President and Director
CanAlaska Uranium Ltd.

Contacts:

Cory Belyk, Executive VP and CEO
Tel: +1.604.688.3211 x 306
Email: cbelyk@canalaska.com

General Enquiry
Tel: +1.604.688.3211
Email: info@canalaska.com

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

Forward-looking information

All statements included in this press release that address activities, events or developments that the Company expects, believes or anticipates will or may occur in the future are forward-looking statements. These forward-looking statements involve numerous assumptions made by the Company based on its experience, perception of historical trends, current conditions, expected future developments and other factors it believes are appropriate in the circumstances. In addition, these statements involve substantial known and unknown risks and uncertainties that contribute to the possibility that the predictions, forecasts, projections and other forward-looking statements will prove inaccurate, certain of which are beyond the Company's control. Readers should not place undue reliance on forward-looking statements. Except as required by law, the Company does not intend to revise or update these forward-looking statements after the date hereof or revise them to reflect the occurrence of future unanticipated events.

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Baselode Defines the Significance of Massive Clay Alteration System Identified on Hook Uranium Project

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  • Five drill holes outlined an open massive hydrothermal clay alteration system measuring at least 200 m x 100 m, resembling alteration found in Athabasca high-grade uranium deposits
  • Radioactivity within the clay alteration system increases with depth and remains open
  • Drill hole HK24-010 intersected 13.4 metres of continuous radioactivity within a 200 m wide alteration system
  • New defined target areas are within 6 km of near-surface ACKIO uranium prospect

Baselode Energy Corp. (TSXV: FIND) (OTCQB: BSENF) ("Baselode" or the "Company") is pleased to provide results and findings from the exploration and discovery portion of the drill program on Hook project ("Hook") in the Athabasca Basin area of northern Saskatchewan.

"These results represent an important discovery on our Hook project. While we've already made a discovery at Hook with ACKIO, this is only a small part of the broader Hook land package. The potential on the property is substantial as Hook is an extensive project, and our discovery at ACKIO, combined with our neighbour Atha Energy's discovery in their Gemini Mineralized Zone, highlights that the region has all the geological features needed to host significant uranium deposits. More importantly, we can clearly demonstrate that this area is fertile with uranium mineralization. Large-scale alteration systems are key indicators when it comes to uranium, which tends to occur in smaller deposits relative to other minerals. We're pleased to have uncovered such a large system, exhibiting all the hallmark features needed for a new high-grade Athabasca uranium discovery," commented James Sykes, CEO, President, and Director of Baselode.

Watch this video for a detailed analysis of the two follow-up target areas and a comparison of Hook alteration systems to seven Athabasca high-grade uranium deposits that have combined over 700 million pounds of uranium.

The first alteration system the Company highlights is in the HK24-016 area, measuring more than 250 metres wide by 400 metres deep, with a core of massive clay and bleached alteration styles that measure 100 metres wide by at least 200 metres deep. These core alteration styles are important as they are the same style associated with at least three basement-hosted Athabasca high-grade uranium deposits.

The second alteration system identified in the HK24-010 area is significant due to its similarly large scale, intersecting 13 meters of continuous anomalous radioactivity within pegmatite along the margin of the fluid pathway. While assays are pending, the Company is well-funded and eager to proceed with follow-up drill plans for these high-priority exploration targets.

Hook Exploration Drill Hole Highlights

HK24-016 area

Drill holes HK24-016, HK24-017, and HK24-021 to HK24-023 were collared 5.5 kilometres southwest of ACKIO (Figure 2, Figure 3). HK24-016 intersected 140 metres of massive hydrothermal clay and bleaching alteration (the "clay alteration") within a broader 370 m thick alteration corridor (Figure 4). The drill hole intersected anomalous radioactivity associated with fracture-controlled remobilized hematite alteration within the clay alteration (Figure 5).

Both HK24-017 and HK24-021 targeted the clay alteration up-dip and down-dip, with each intersecting 30 and 145 metres of clay alteration, respectively. HK24-022 was collared 100 metres southeast of HK24-016 and intersected 60 metres of clay alteration, and HK24-023 was collared 50 metres northeast and intersected 110 metres of clay alteration. Initial observations suggests follow-up drilling is required beneath HK24-021 and to the north of HK24-023.

The clay alteration encountered within these Hook drill holes (Figure 6) share numerous similarities to massive hydrothermal clay alteration systems observed in Athabasca basement-hosted, high-grade uranium systems, such as Cameco's Millennium and Eagle Point deposits, Uranium Energy Corp's Roughrider deposits, and Denison Mines' Gryphon deposit.

The upper outer halo of the clay alteration is further identified with unique limonite liesegang banding and fracture-controlled alteration, including a distinct quartz stockwork. These are also similar outer halo alteration styles that have been observed within large-scale Athabasca uranium deposits.

HK24-010 area

Drill holes HK24-009 and HK24-010 were collared 6 kilometres northeast of ACKIO (see Figure 2, Figure 7). Details of these drill holes were initially released on July 17, 2024. HK24-010 has returned the best radioactive intersection outside of Baselode's near-surface ACKIO uranium prospect with 13.2 metres of continuous anomalous radioactivity starting at 186 metres beneath the surface hosted within a pegmatite along the western margin of a 200 m-wide, structurally-controlled, hematite and bleached alteration system. The area remains open in all directions.

Drill hole samples have been sent to Saskatchewan Research Council for uranium and multi-element analysis. Results will be released after being received and reviewed by the Company.

NOTES:

  1. cps* = "counts-per-second", as measured with a handheld RS-125 Gamma-Ray Spectrometer/Scintillometer ("RS-125"). The reader is cautioned that Baselode uses scintillometer readings as a preliminary indication for the presence of radioactive materials (uranium, thorium and/or potassium), and that scintillometer results may not be used directly to quantify or qualify uranium concentrations of the rock samples measured.
  2. The Company defines groupings of RS-125 as i) background radioactivity (50 to 200 cps), ii) above-background radioactivity (200 to 300 cps), and iii) anomalous radioactivity (300 to 1,000 cps).
  3. "Radioactivity (>300 cps)" in Table 1 is defined as drill core length with no greater than 2.0 m of consecutive drill hole length measuring less than 300 cps.
  4. All reported drill hole depths and lengths do not represent true thicknesses.

About Baselode Energy Corp.

Baselode controls 100% of approximately 238,930 hectares for exploration in the Athabasca Basin area of northern Saskatchewan, Canada. The land package is free of any option agreements or underlying royalties.

The Company discovered the ACKIO near-surface, uranium prospect in September 2021. ACKIO measures greater than 375 m along strike, greater than 150 m wide, comprised of at least 9 separate uranium Pods, with mineralization starting as shallow as 28 m and 32 m beneath the surface in Pods 1 and 7, respectively, and down to approximately 300 m depth beneath the surface with the bulk of mineralization occurring in the upper 120 m. ACKIO remains open at depth, and to the north, south and east.

Baselode's Athabasca 2.0 exploration thesis focuses on discovering near-surface, basement-hosted, high-grade uranium orebodies outside the Athabasca Basin. The exploration thesis is further complemented by the Company's preferred use of innovative and well-understood geophysical methods to map deep structural controls to identify shallow targets for diamond drilling.

QP Statement

The technical information contained in this news release has been reviewed and approved by Cameron MacKay, P.Geo., Vice-President, Exploration & Development for Baselode Energy Corp., who is considered to be a Qualified Person as defined in "National Instrument 43-101, Standards of Disclosure for Mineral Projects."

For further information, please contact:

James Sykes, CEO, President and Director
Baselode Energy Corp.
jsykes@oregroup.ca
306-221-8717
www.baselode.com

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

Certain information in this press release may contain forward-looking statements. This information is based on current expectations that are subject to significant risks and uncertainties that are difficult to predict. Actual results might differ materially from results suggested in any forward-looking statements. Baselode Energy Corp. assumes no obligation to update the forward-looking statements, or to update the reasons why actual results could differ from those reflected in the forward looking-statements unless and until required by securities laws applicable to Baselode Energy Corp. Additional information identifying risks and uncertainties is contained in the Company's filings with Canadian securities regulators, which filings are available under Baselode Energy Corp. profile at www.sedarplus.ca.

This news release does not constitute an offer to sell or a solicitation of an offer to buy any of the securities in the United States. The securities have not been and will not be registered under the United States Securities Act of 1933, as amended (the "U.S. Securities Act") or any state securities laws and may not be offered or sold within the United States or to, or for the account or benefit of, U.S. Persons unless registered under the U.S. Securities Act and applicable state securities laws, unless an exemption from such registration is available.

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FIGURE 1 - Baselode projects location map. ACKIO uranium prospect identified with yellow circle.

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FIGURE 2 - Drill holes (HK24-009 to HK24-023) location map

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FIGURE 3 - HK24-016 target area drill holes (HK24-016, HK24-017, and HK24-021 to HK24-023) location map

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FIGURE 4 - Cross-section interpretation of large hydrothermal fluid system with core massive clay and bleaching alteration (blue)

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FIGURE 5 - Fracture-controlled, hydrothermal remobilized anomalous radioactivity, HK24-016

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FIGURE 6 - Massive clay and bleaching alteration system, HK24-021. NOTE: clay has been gouged with carbon scribe to demonstrate drill core softness

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FIGURE 7 - HK24-010 target area drill holes (HK24-009 and HK24-010) location map

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MOVIE 1 - Clay alteration and bleaching identified within drill hole HK24-021

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