Beaver River Project
The 4502.4 ha Beaver River Project is located 40 km ESE of Uranium City in northern Saskatchewan. Uranium City is located on the north shore of Lake Athabasca, 536km NNW of LaRonge and is accessible via scheduled flights from Saskatoon, Saskatchewan and charter aircraft from Fort McMurray, Alberta. All season road access is available to Stoney Rapids then a 175km seasonal ice road to Uranium City via Fon-du-Lac. Uranium City is endowed with services such as hospital, lodging accommodations, groceries, fuel and airport.
The Beaver River claims were acquired in 2023 and have no underlying royalties or encumbrances. They are located within 2.5km of a power transmission line and accessible by float/ski equipped aircraft from Uranium City. A detailed compilation and interpretation of available data from historical work programs has begun and will lead to recommendations for future work and more information for this webpage.
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- Saskatchewan
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- Available for option: No
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- Uranium,
- Copper,
- Nickel
Project Highlights
- Chip sampling at the VIC South Occurrence returned U308 values of, 29.89% over 0.293m, 18.09% over 0.152m and 3.09% over 0.609m
- Mineralization occurs continuous over approximately 1097m
- Hosts Beaverlodge-style basement-hosted uranium mineralization
- Property contains 4 uranium mineral occurrences
- Grab samples from VIC U-Cu-Ni Occurrence returned up to 36.3%, 29.7% and 27.62% U308
Summary
The Beaver River uranium project, located 40km SE of Uranium City, Saskatchewan, hosts near surface high grade uranium mineralization.
The Uranium City projects are included in a formal Exploration Agreement between Eagle Plains and the Ya’thi Néné Lands and Resource Office (“YNLR”), representing the Athabasca Denesułiné First Nations of Hatchet Lake, Black Lake, and Fond du Lac, the Northern Hamlet of Stony Rapids, and the Northern Settlements of Uranium City, Wollaston Lake and Camsell Portage.
Beaver River Highlights
- Historical assays up to 29.89% U3O8 in trench chip samples
- Historical drill intersections include 0.18% U3O8 over 0.3m and 0.06% U3O8 over 0.61m
- Recognized mineralized trend >1km in length
- Prospective for polymetallic Beaverlodge-type uranium mineralization in E-W and NW-SE trending fault zones
Uranium City Option Agreement
Under the terms of the agreements, Xcite Uranium Inc. may earn an 80% interest in each of the Beaver River, Black Bay, Don Lake, Gulch, Lorado, and Smitty projects by completing CDN$3,200,000 in exploration expenditures, issuing 750,000 common shares of Xcite and making cash payments to Eagle Plains of CDN$55,000 over four years, for an aggregate of CDN$19,200,000 in exploration expenditures, 4,500,000 shares and $330,000 in cash to Eagle Plains. Upon Xcite fulfilling the terms of any or all of the earn-in agreements, an 80/20 joint venture will be formed, with Eagle Plains retaining a carried interest in all expenditures until delivery by Xcite or its assigns of a bankable feasibility study. During the option earn in period, XRI will be appointed as operator, and EPL will manage the exploration programs under the direction of a joint technical committee. The projects are owned 100% by EPL, who will retain an underlying 2% NSR royalty on the each of the properties.
About the Beaverlodge Uranium District
The Beaver River, Black Bay, Don Lake, Gulch, Lorado, and Smitty projects are located in the Beaverlodge District near Uranium City in the Lake Athabasca region of Saskatchewan. Occurrences of uranium mineralization are abundant in the Uranium City area and have been explored and documented since the 1940s. The Beaverlodge camp was the first uranium producer in Canada, with historic production of approximately 70.25 million pounds of U3O8 between 1950-1982, from ore grades averaging 0.23% U3O8. The two largest producers were the Eldorado Beaverlodge (Ace-Fay-Verna) mine and the Gunnar uranium mine. The Beaverlodge area has seen limited uranium focused exploration since the early 1990’s.
The Uranium City area projects have potential for both Beaverlodge-style and basement-hosted uranium mineralization.
Key features about the projects include:
- Outcropping, largely northeast-southwest-trending tectonic fabric;
- Electromagnetic conductors that have been confirmed as graphite-rich pelites within or near major faults;
- Anomalous uranium geochemistry and radioactivity associated with graphitic faults;
- Compelling property-wide evidence for hydrothermal alteration;
- Uranium mineralization with corresponding elevations in pathfinder elements.
These factors, along with the presence of a substantial uranium endowment in both basement rocks and Athabasca basin cover rocks, indicate excellent potential for economic uranium mineralization within the project. The mineralization, structures and alteration identified on the claims to date are strong indicators of the possibility of a nearby source for the uranium mineralization.
Eagle Plains’ management cautions that past results or discoveries on proximate land are not necessarily indicative of the results that may be achieved on the subject properties.
Eagle Plains - A Project Generator
Eagle Plains Resources is a project generator with several mineral exploration properties of merit that meet qualifying transaction requirements. We facilitate the listing process for capital pool companies and initial public offerings while providing technical expertise for exploration programs. Companies interested in co-operatively exploring any of our projects please contact: Chuck Downie at ccd@eagleplains.com or Andrew Wilson at abw@eagleplains.com or call 1 866 Hunt Ore (486 8673).
Details
The 4502.4ha project overlies 5 Saskatchewan Mineral Deposit Index (“SMDI”) occurrences associated with Beaverlodge-type uranium mineralization.
The polymetallic VIC U-Cu-Ni zone (SMDI 1551, 1553, and 1994) occurs along a NW-SE trending fault zone which has been traced for approximately 1 km. Mineralization occurs in fracture filling of quartz veins hosting sulphides, graphite, and pitchblende and uraninite, ore minerals of uranium. Historical assays of channel samples in this zone yield up to 29.89% U3O8 over 0.3m, 18.09% U3O8 over 0.2m and 3.09% U3O8 over 0.6m (AF 74O05-0077). The southeast zone has been tested by nine shallow drill holes, averaging 80m in length, returning assays of 0.18% U3O8 over 0.3m (AF74O05-0016) and 0.06% U3O8 over 0.61m along with anomalous copper, nickel, gold and silver (AF74O05-0051). The northwest portion of the VIC zone, identified as a priority for follow-up by Denison Mines, has yet to be tested by drilling.
Another significant mineral occurrence on the Beaver River property is the Combined Mining Uranium Showing (SMDI 1557) where northeast-trending pitchblende-bearing fractures have ben mapped over a strike length of 137.2m. Assays from trenches yielded 0.23% U3O8 over 0.5m and 1.77% U3O8 over 0.9m.
Since uranium mineralization on the Beaver River property was first noted in 1958 the property has seen a total of 1708m of diamond drilling in 26 shallow holes, with the last drilling completed in 1969 by Trans-Canada Resources. Other historical work includes prospecting, mapping, scintillometer surveys, trenching at the main showing areas, and airborne and ground-based geophysics.
An electromagnetic and magnetic VTEM survey flown by Geotech for Fission 3.0 in 2016 covered the eastern part of the Beaver River property. The survey outlined numerous areas of enhanced conductivity including areas of parallel conductors with offsets and termination points indicative of cross structure, including a high priority conductive trend located west of the Combined SMDI occurrence. Follow-up prospecting and geochemical sampling was recommended to evaluate the source of the anomalies.
The last recorded assessment work on the project was by Fission 3.0 who successfully located and resampled historic trenches at the VIC occurrence.
Management of Eagle Plains and Xcite are encouraged by the tenor of mineralization displayed in trenches and shallow historical drilling at Beaver River and the potential for additional uranium mineralization both along strike and to depth within known mineralized areas, along trends identified by historical geophysical surveys, and on any additional targets generated by 2024 work.
