Proven Probable
Register for the Rule Symposium Here: https://registration.allintheloop.net/register/event/rick-rule-symposium-2025-ccha?via=ProvenAndProbable
F3 Uranium
Website: https://f3uranium.com/
TSX.V: FUU | OTCQB: FUUFF
Press Release: https://f3uranium.com/f3-hits-anomalous-radioactivity-12km-south-of-jr-zone-on-broach-property/
Corporate Presentation: https://f3uranium.com/corporate/
Contact: ir@f3uranium.com +1 778-484-8030
20.0m Composite Mineralization at JR Zone with 2.25m high grade Radioactivity
Kelowna, British Columbia–(Newsfile Corp. – March 18, 2025) – F3 Uranium Corp (TSXV: FUU) (OTCQB: FUUFF) (“F3” or “the Company“) is pleased to release initial scintillometer results from the ongoing winter drill programs at the PLN and Broach Properties including drilling at JR Zone, B1, and the PW Area. At Broach Lake a new prospective area “PW” is emerging, where exploration drillhole PLN25-202 encountered six distinct zones of anomalous radioactivity, with readings ranging between 300 cps and 720 cps over a 90m downhole interval. At JR Zone, PLN25-200 returned mineralization over 20.0m, including 2.25m of high grade (>10,000 cps) containing 0.68m of off-scale mineralization (>65,535 cps).
2025 Handheld Spectrometer Highlights:
PLN: JR Zone
PLN25-198 (line 090S):
PLN25-200 (line 045S):
Broach Lake: PW Area
PLN25-202 (line 11325S):
B1 Conductor:
PLN25-196 (line 2835S):
Sam Hartmann, Vice President Exploration, commented:
“The ‘PW’ area, situated on the Broach Property approximately 12 kilometers south of the JR Zone, lies just within the Athabasca Basin and represents a region with minimal historical exploration and drilling activity. No previously defined conductors had been identified in this area, largely due to the presence of a thick layer of conductive Cretaceous mudstone from the Manville Group, which locally reaches thicknesses of nearly 100 meters. Recognizing the potential of this challenging but underexplored region, we conducted a specifically designed MLTDEM ground survey (see NR February 11) which has just been completed by Abitibi Geophysics. This approach successfully delineated a number of basement-hosted conductors on the survey lines interpreted so far with lines L3200N to L4400N still outstanding (see Map 2), overcoming the interference posed by the conductive mudstones. Drillhole PLN25-202 was collared based on an initial interpretation and conductor model on L1600N, and intersected strongly altered basement lithologies, encountering six distinct radioactive intercepts across a 90-meter downhole interval. Data from this drillhole was subsequently re-integrated back into the electromagnetic (EM) model – which resulted in a lateral shift of the conductor model by approximately 100 meters. This adjustment suggests that PLN25-202 overshot the intended target yet – still encountered significant alteration and structures along with radioactivity. A follow-up drillhole is scheduled and planned to step back by approximately 100 meters to better intersect the refined target, which lies in a distinct circular gravity anomaly. While the PW Area is still in its early stages of exploration, we are highly encouraged by these strong initial results, and intend to conduct further drilling in the area before shifting focus back to the JR Zone toward the conclusion of the winter season.”
Map 1. Patterson Lake North – JR Zone 2025 Scintillometer Results
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/8110/244920_f088d21f648b2b38_002full.jpg
Map 2. Broach Lake – PW Area 2025 Scintillometer Results
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/8110/244920_f088d21f648b2b38_003full.jpg
Table 1. Drill Hole Summary and Handheld Spectrometer Results
| Collar Information | * Hand-held Spectrometer Results On Mineralized Drillcore (>300 cps / >0.5m minimum) | |||||||||||
| Hole ID | Section Line | Easting | Northing | Elevation | Az | Dip | From (m) | To (m) | Interval (m) | Max CPS | Athabasca Unconformity Depth (m) | Total Drillhole Depth (m) |
| PLN25-196 | 2835S | 589265.0 | 6408368.2 | 537.9 | 54.1 | -67.3 | 366.50 | 367.00 | 0.50 | 390 | 178.4 | 497 |
| PLN25-197 | 030S | 587776.2 | 6410760.2 | 546.4 | 55.1 | -70.7 | 206.50 | 207.00 | 0.50 | 880 | 189.7 | 251 |
| 207.00 | 207.50 | 0.50 | 7,600 | |||||||||
| 207.50 | 208.00 | 0.50 | 9,700 | |||||||||
| 208.00 | 208.50 | 0.50 | 5,100 | |||||||||
| 208.50 | 209.00 | 0.50 | 510 | |||||||||
| 209.00 | 209.50 | 0.50 | 360 | |||||||||
| 209.50 | 210.00 | 0.50 | 390 | |||||||||
| 210.00 | 210.50 | 0.50 | 350 | |||||||||
| 210.50 | 211.00 | 0.50 | 530 | |||||||||
| 211.00 | 211.50 | 0.50 | 1,100 | |||||||||
| PLN25-198 | 090S | 587842.9 | 6410645.2 | 546.0 | 9.4 | -64.9 | 214.50 | 215.00 | 0.50 | 330 | 191.7 | 299 |
| 215.00 | 215.50 | 0.50 | 460 | |||||||||
| 215.50 | 217.50 | 2.00 | <300 | |||||||||
| 217.50 | 218.00 | 0.50 | 3,400 | |||||||||
| 218.00 | 218.50 | 0.50 | 2,200 | |||||||||
| 218.50 | 219.00 | 0.50 | 330 | |||||||||
| 219.00 | 219.50 | 0.50 | 340 | |||||||||
| 219.50 | 220.00 | 0.50 | 570 | |||||||||
| 220.00 | 220.50 | 0.50 | 450 | |||||||||
| 220.50 | 220.65 | 0.15 | 8,600 | |||||||||
| 220.65 | 220.85 | 0.20 | 22,100 | |||||||||
| 220.85 | 221.00 | 0.15 | 7,700 | |||||||||
| 221.00 | 221.50 | 0.50 | 8,100 | |||||||||
| 221.50 | 222.00 | 0.50 | 2,500 | |||||||||
| 222.00 | 222.50 | 0.50 | 4,900 | |||||||||
| 222.50 | 223.00 | 0.50 | 2,200 | |||||||||
| 228.50 | 229.00 | 0.50 | 310 | |||||||||
| 229.00 | 229.50 | 0.50 | <300 | |||||||||
| 229.50 | 230.00 | 0.50 | 450 | |||||||||
| PLN25-199 | 010N | 587693.2 | 6410748.1 | 545.2 | 54.9 | -65.7 | 232.00 | 232.50 | 0.50 | 360 | 197.7 | 269 |
| 242.00 | 242.50 | 0.50 | 1,000 | |||||||||
| 242.50 | 243.00 | 0.50 | 2,900 | |||||||||
| 243.00 | 243.50 | 0.50 | 1,100 | |||||||||
| PLN25-200 | 045S | 587730.9 | 6410712.4 | 545.2 | 53.4 | -65.5 | 229.00 | 229.50 | 0.50 | 330 | ||
| 229.50 | 230.00 | 0.50 | 360 | |||||||||
| 233.00 | 233.50 | 0.50 | 660 | |||||||||
| 233.50 | 234.00 | 0.50 | 720 | |||||||||
| 234.00 | 234.50 | 0.50 | 1,900 | |||||||||
| 234.50 | 235.00 | 0.50 | 4,900 | |||||||||
| 235.00 | 235.50 | 0.50 | 660 | |||||||||
| 235.50 | 236.00 | 0.50 | 9,600 | |||||||||
| 236.00 | 236.50 | 0.50 | 62,200 | |||||||||
| 236.50 | 237.00 | 0.50 | 13,400 | |||||||||
| 237.00 | 237.50 | 0.50 | 9,200 | |||||||||
| 237.50 | 237.65 | 0.15 | 58,200 | |||||||||
| 237.65 | 238.00 | 0.35 | >65,535 | |||||||||
| 238.00 | 238.33 | 0.33 | >65,535 | |||||||||
| 238.33 | 238.50 | 0.17 | 61,000 | |||||||||
| 238.50 | 238.75 | 0.25 | 22,300 | |||||||||
| 238.75 | 239.00 | 0.25 | 8,600 | |||||||||
| 239.00 | 239.50 | 0.50 | 8,400 | |||||||||
| 239.50 | 240.00 | 0.50 | 2,800 | |||||||||
| 240.00 | 240.50 | 0.50 | 5,700 | |||||||||
| 240.50 | 241.00 | 0.50 | 3,000 | |||||||||
| 241.00 | 241.50 | 0.50 | 5,400 | |||||||||
| 241.50 | 242.00 | 0.50 | 5,200 | |||||||||
| 242.00 | 242.50 | 0.50 | 5,100 | |||||||||
| 242.50 | 243.00 | 0.50 | 470 | |||||||||
| 243.00 | 244.00 | 1.00 | <300 | |||||||||
| 244.00 | 244.50 | 0.50 | 320 | |||||||||
| 244.50 | 246.50 | 2.00 | <300 | |||||||||
| 246.50 | 247.00 | 0.50 | 2,100 | |||||||||
| 247.00 | 247.50 | 0.50 | 740 | |||||||||
| 247.50 | 248.00 | 0.50 | 1,100 | |||||||||
| 248.00 | 248.50 | 0.50 | 480 | |||||||||
| 248.50 | 249.00 | 0.50 | <300 | |||||||||
| 249.00 | 249.50 | 0.50 | 330 | |||||||||
| 249.50 | 250.00 | 0.50 | 740 | |||||||||
| 250.00 | 251.00 | 1.00 | <300 | |||||||||
| 251.00 | 251.50 | 0.50 | 1,300 | |||||||||
| 251.50 | 252.00 | 0.50 | 2,100 | |||||||||
| PLN25-201 | 12510S | 590064.4 | 6397263.8 | 568.9 | 45.9 | -70.2 | PW Exploration; no radioactivity >300 cps | n.a. | 437 | |||
| PLN25-202 | 11325S | 589352.6 | 6397967.0 | 583.2 | 45.9 | -63.3 | 272.50 | 273.00 | 0.50 | 330 | 171.6 | 464.5 |
| 275.50 | 276.00 | 0.50 | 300 | |||||||||
| 296.00 | 296.50 | 0.50 | 330 | |||||||||
| 321.00 | 321.50 | 0.50 | 320 | |||||||||
| 359.50 | 360.00 | 0.50 | 320 | |||||||||
| 362.50 | 363.00 | 0.50 | 720 | |||||||||
Handheld spectrometer composite parameters:
1: Minimum Thickness of 0.5m
2: CPS Cut-Off of 300 counts per second
3: Maximum Internal Dilution of 2.0m
Image 1: Anomalous Radioactivity in PLN25-202
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/8110/244920_f088d21f648b2b38_004full.jpg
The natural gamma radiation detected in the drill core, as detailed in this news release, was measured in counts per second (cps) using a handheld Radiation Solutions RS-125 spectrometer. The Company designates readings exceeding 300 cps on the handheld spectrometer (occasionally referred to as a scintillometer in industry parlance; this colloquial usage stems from historical naming conventions and the shared functionality of detecting gamma radiation with a scintillometer)—as “anomalous”, readings above 10,000 cps as “high-grade”, and readings surpassing 65,535 cps as “off-scale”. However, readers are cautioned that spectrometer or scintillometer measurements often do not directly or consistently correlate with the uranium grades of the rock samples and should be regarded solely as a preliminary indicator of the presence of radioactive materials.
Samples from the drill core are split into half sections on site. Where possible, samples are standardized at 0.5m down-hole intervals. One-half of the split sample is sent to SRC Geoanalytical Laboratories (an SCC ISO/IEC 17025: 2005 Accredited Facility) in Saskatoon, SK while the other half remains on site for reference. Analysis includes a 63 element suite including boron by ICP-OES, uranium by ICP-MS and gold analysis by ICP-OES and/or AAS.
The Company considers uranium mineralization with assay results of greater than 1.0 weight % U3O8 as “high grade” and results greater than 20.0 weight % U3O8 as “ultra-high grade”.
All depth measurements reported are down-hole and true thicknesses are yet to be determined.
About the Patterson Lake North Project:
The Company’s 42,961-hectare 100% owned Patterson Lake North Project (PLN) is located just within the south-western edge of the Athabasca Basin in proximity to Paladin’s Triple R and NexGen Energy’s Arrow high-grade uranium deposits, an area poised to become the next major area of development for new uranium operations in northern Saskatchewan. The PLN Project consists of the 4,074-hectare Patterson Lake North Property, the 19,864-hectare Minto Property, and the 19,022-hectare Broach Property. All three properties comprising the PLN Project are accessed by Provincial Highway 955; the new JR Zone uranium discovery on the PLN property is located 23km northwest of Paladin’s Triple R deposit.
Qualified Person:
The technical information in this news release has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and approved on behalf of the company by Raymond Ashley, P.Geo., President & COO of F3 Uranium Corp, a Qualified Person. Mr. Ashley has verified the data disclosed.
About F3 Uranium Corp.:
F3 Uranium is a uranium exploration company, focusing on the recently discovered high-grade JR Zone on its Patterson Lake North (PLN) Project in the Western Athabasca Basin. F3 Uranium currently has 3 properties in the Athabasca Basin: Patterson Lake North, Minto, and Broach. The western side of the Athabasca Basin, Saskatchewan, is home to some of the world’s largest high grade uranium deposits including Paladin’s Triple R and Nexgen’s Arrow.
Forward-Looking Statements
This news release contains certain forward-looking statements within the meaning of applicable securities laws. All statements that are not historical facts, including without limitation, statements regarding future estimates, plans, programs, forecasts, projections, objectives, assumptions, expectations or beliefs of future performance, including statements regarding the suitability of the Properties for mining exploration, future payments, issuance of shares and work commitment funds, entry into of a definitive option agreement respecting the Properties, are “forward-looking statements.” These forward-looking statements reflect the expectations or beliefs of management of the Company based on information currently available to it. Forward-Looking statements are subject to a number of risks and uncertainties, including those detailed from time to time in filings made by the Company with securities regulatory authorities, which may cause actual outcomes to differ materially from those discussed in the forward-looking statements. These factors should be considered carefully and readers are cautioned not to place undue reliance on such forward-looking statements. The forward-looking statements and information contained in this news release are made as of the date hereof and the Company undertakes no obligation to update publicly or revise any forward-looking statements or information, whether as a result of new information, future events or otherwise, unless so required by applicable securities laws.
The TSX Venture Exchange and the Canadian Securities Exchange have not reviewed, approved or disapproved the contents of this press release, and do not accept responsibility for the adequacy or accuracy of this release.
F3 Uranium Corp.
750-1620 Dickson Avenue
Kelowna, BC V1Y9Y2
Contact Information
Investor Relations
Telephone: 778 484 8030
Email: ir@f3uranium.com
ON BEHALF OF THE BOARD
“Dev Randhawa”
Dev Randhawa, CEO
To view the source version of this press release, please visit https://www.newsfilecorp.com/release/244920
~Confirms receipt of the Interim Order, files Meeting Materials, and announces another round of Blue Jay financing~
Vancouver, British Columbia–(Newsfile Corp. – February 28, 2025) – Riverside Resources Inc. (TSXV: RRI) (OTCQB: RVSDF) (FSE: 5YY) (“Riverside” or the “Company”) is pleased to announce that its management information circular (the “Information Circular“), form of proxy and letter of transmittal, (together with the Information Circular, the “Meeting Materials“) in respect of its annual and special meeting (the “Meeting“) of Riverside shareholders (the “Riverside Shareholders“) to approve various matters in connection with the previously announced plan of arrangement (the “Arrangement“) on January 28, 2025 involving Blue Jay Gold Corp. (“Blue Jay“) are being filed today on Riverside’s SEDAR+ profile at www.sedarplus.ca. and provided on Riverside’s website at www.rivres.com. Riverside is using the notice and access provisions under applicable securities laws to provide Riverside Shareholders with easy electronic access to the Information Circular and other Meeting Materials.
If the Arrangement is approved at the Meeting, Riverside will distribute its common shares (each, a “Blue Jay Share“) in Blue Jay to the Riverside Shareholders by way of a statutory plan of arrangement (the “Plan of Arrangement“) under section 288 of the Business Corporations Act (British Columbia) (the “Transaction“). Following the Arrangement, Riverside Shareholders will hold shares in two reporting issuers: Riverside and Blue Jay. Blue Jay is expected to make an application to list the Blue Jay Shares on the TSX Venture Exchange (“TSXV“).
Blue Jay currently holds all right and title to the Pichette-Clist Gold Project, the Oakes Gold Project and the Duc Gold Project in Northwestern, Ontario (the “Ontario Properties“).
Information about the Meeting and Receipt of Interim Court Order
On February 14, 2025, Riverside obtained an interim order (the “Interim Order“) from the British Columbia Supreme Court (the “Court“) in connection with the Arrangement, authorizing the calling and holding of the Meeting and other matters related to the conduct of the Meeting. At the Meeting, the Riverside Shareholders will be asked to consider and, if deemed advisable, pass a special resolution (the “Arrangement Resolution“) to approve Arrangement, in accordance with the terms of an arrangement agreement (the “Arrangement Agreement“) entered into by the Company and Blue Jay on January 27, 2025.
The Meeting is scheduled to be held on March 31, 2025 at 11:00 A.M. (Vancouver time) at Suite 550, 800 West Pender Street, Vancouver, British Columbia. At the Meeting, Riverside Shareholders will be asked to approve the Arrangement Resolution.
The Meeting Materials contain important information regarding the Transaction, how Riverside Shareholders can participate and vote at the Meeting, the background that led to the Transaction and the reasons for the unanimous determinations of the board of directors of the Company (the “Riverside Board“) that the Transaction is in the best interests of the Company and is fair to Riverside Shareholders. Shareholders should carefully review all of the Meeting Materials as they contain important information concerning the Transaction and the rights and entitlements of Shareholders thereunder.
Reasons for the Arrangement
Riverside believes that the Arrangement is in the best interests of Riverside for numerous reasons, including:
In the course of its deliberations, the Riverside Board also identified and considered a variety of risks and potentially negative factors, including, but not limited to, the risks factors set out in the Information Circular and the documents incorporated by reference therein.
The foregoing discussion summarizes the material information and factors considered by the Riverside Board in their consideration of the Plan of Arrangement. The Riverside Board collectively reached its unanimous decision with respect to the Plan of Arrangement in light of the factors described above and other factors that each member of the Riverside Board felt were appropriate. In view of the wide variety of factors and the quality and amount of information considered, the Riverside Board did not find it useful or practicable to, and did not make specific assessments of, quantify, rank or otherwise assign relative weights to the specific factors considered in reaching its determination. Individual members of the Riverside Board may have given different weight to different factors.
Recommendation of the Directors
After careful consideration, the Riverside Board, after receiving legal, tax and financial advice, has unanimously determined that the Arrangement is in the best interests of Riverside and is fair to the Shareholders. Accordingly, the Riverside Board unanimously recommends that Shareholders vote FOR the Arrangement Resolution.
In order to become effective, the Arrangement must be approved by at least 66⅔% of the votes cast by the Riverside Shareholders present or represented by proxy at the Meeting. Subject to obtaining approval of the Transaction at the Meeting, and the satisfaction of the other customary conditions to completion of the Transaction contained in the Arrangement Agreement, including final approval of the Court and certain regulatory approvals, all as more particular described in the Meeting Materials, the Transaction is expected to close in the second quarter of 2025.
Filing of New Technical Report
Riverside also announces today that it will file a new technical report under National Instrument 43-101 – Standards of Disclosure for Mineral Projects titled, “Technical Report on the Pichette-Clist Property, Jellicoe Area, Northwestern Ontario” prepared by Locke B. Goldsmith, P. Eng, P.Geo, dated January 29, 2025. The Pichette-Clist Property will be Blue Jay’s material property once the Arrangement is effective. Such report will be available on Riverside’s SEDAR+ profile at https://www.sedarplus.ca/.
Blue Jay to Complete Another Round of Financing
In anticipation of making an application to list the Blue Jay Shares on the TSXV and in order to satisfy the TSXV listing requirements, Blue Jay expects to complete two further rounds of financing in connection with the Arrangement, being (a) a private placement of 2,000,000 Blue Jay Shares at an issue price of $0.40 per Blue Jay Share for gross proceeds of $800,000; and (b) a private placement of 2,000,000 Blue Jay Shares at an issue price of $0.50 for total gross proceeds of $1,000,000 and 1,428,571 Blue Jay Shares issued as “flow-through shares” (the “Flow Through Shares”) within the meaning of the Income Tax Act at an issue price of $0.70 per Flow Through Share. Each such private placement is subject to the approval by the TSXV.
About Riverside Resources Inc.
Riverside is a well-funded exploration company driven by value generation and discovery. The Company has over $4M in cash, no debt and less than 75M shares outstanding with a strong portfolio of gold-silver and copper assets and royalties in North America. Riverside has extensive experience and knowledge operating in Mexico and Canada and leverages its large database to generate a portfolio of prospective mineral properties. In addition to Riverside’s own exploration spending, the Company also strives to diversify risk by securing joint-venture and spin-out partnerships to advance multiple assets simultaneously and create more chances for discovery. Riverside has properties available for option, with information available on the Company’s website at www.rivres.com.
ON BEHALF OF RIVERSIDE RESOURCES INC.
“John-Mark Staude”
Dr. John-Mark Staude, President & CEO
For additional information contact:
| John-Mark Staude President, CEO Riverside Resources Inc. info@rivres.com Phone: (778) 327-6671 Fax: (778) 327-6675 Web: www.rivres.com | Eric Negraeff Investor Relations Riverside Resources Inc. Phone: (778) 327-6671 TF: (877) RIV-RES1 Web: www.rivres.com |
Certain statements in this press release may be considered forward-looking information. These statements can be identified by the use of forward-looking terminology (e.g., “expect”,” estimates”, “intends”, “anticipates”, “believes”, “plans”). Such information involves known and unknown risks — including the availability of funds, the results of financing and exploration activities, the interpretation of exploration results and other geological data, or unanticipated costs and expenses and other risks identified by Riverside in its public securities filings that may cause actual events to differ materially from current expectations. Readers are cautioned not to place undue reliance on these forward-looking statements, which speak only as of the date of this press release.
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/242747
Vancouver, British Columbia–(Newsfile Corp. – February 27, 2025) – Riverside Resources Inc. (TSXV: RRI) (OTCQB: RVSDF) (FSE: 5YY) (“Riverside” or the “Company”) is pleased to provide an update on its exploration progress in Canada and Mexico and further progress on the proposed spinout of Blue Jay Gold. In follow-up to the Company’s earlier press release this month, which provided updates on drilling and the 2025 exploration program at the Cecilia project, as well as ongoing collaboration with Fortuna Mining, Riverside is highlighting recent technical results from its gold and copper assets in Mexico, as well as the gold and rare earth element (REE) projects in British Columbia in this news release ahead of presenting at the Prospector Developer Association of Canada conference where the Company once again has booth and will be meeting investors and potential corporate partners.
Exploration Highlights:
CANADA
MEXICO
“We are excited to see our projects advancing, both through partnerships and our own exploration efforts,” commented John-Mark Staude, CEO of Riverside Resources. “As we attend PDAC in Toronto, we look forward to meeting with industry peers and showcasing our portfolio of gold, copper, silver and rare earth projects. Riverside holds royalties on several assets and also owns 100% of drill-permitted projects that are ready for turnkey exploration with existing and potential new partners. Additionally, we’re pleased with the progress of our proposed transaction, with Blue Jay Gold shares expected to spin out to Riverside shareholders in the first half of 2025. Alongside this, we anticipate strong exploration and discovery potential at Cecilia and other partner-backed projects in the coming months.”
Royalties
Fresnillo PLC continues drilling and resource refinement at the Tajitos project, evaluating its potential for future mine development. The newly elected President of Mexico, Claudia Sheinbaum, has expressed support for mining development, which could positively impact the progress of major projects like Tajitos Gold Project.
The Tajitos project is strategically located in northwest Sonora, Mexico, benefiting from excellent road infrastructure and access to power. The terrain is relatively flat, with no residential settlements on-site. Additionally, private ranch land where the project is located has been acquired and consolidated by Fresnillo, further facilitating potential mine construction and operations. Riverside holds a 2% net smelter royalty (NSR) on a portion of the Tajitos project, providing a strong future revenue opportunity for Riverside.
Riverside also holds a 2% NSR on the Sugarloaf Peak gold project, operated by Arizona Metals, as well as a diverse portfolio of additional royalties. More details on Riverside’s royalty assets can be found on the company’s website at www.rivres.com.
PDAC 2025
The Riverside team is pleased to invite investors, industry professionals, and stakeholders to visit us at PDAC 2025 in Toronto. Riverside’s President and CEO, John-Mark Staude, along with key team members, will be available at booth #2413A on Sunday, March 2, and Monday, March 3, from 10 AM to 5 PM or contact us at the information below.
This event provides an excellent opportunity to connect with the Riverside team, gain insights into the company’s exploration and development plans for 2025, and discuss the latest progress across our gold, copper, and silver projects in Mexico and Canada.
Additionally, Geordie Mark, CEO of Blue Jay Gold, will be attending PDAC. Blue Jay Gold, Riverside’s latest spinout, represents a compelling growth opportunity, and this will be a great chance to meet with Geordie and learn more about the company’s strategy and outlook.
Canada
Riverside continues to advance exploration at its Deer Park gold project in British Columbia, where recent fieldwork has provided strong sampling results, positive geological indicators, and structural features similar to those found in the Rossland Camp, one of BC’s largest historical gold producers. With high-grade, multi-element ores and well-developed infrastructure, Rossland has demonstrated significant mineral potential, and Riverside has outlined compelling targets for further exploration.
For Rare Earth Elements (REEs), Riverside has made notable progress at its Revel and Taft projects. At Revel, the carbonatite-style system extends over 7 kilometers along strike, with varying widths, and remains unexplored by drilling. The project is part of BC’s broader REE carbonatite belt, with extensive exposures of carbonatite mineralization. Additionally, Mount Grace, a district-scale carbonatite project staked and advanced by Riverside, has been previously studied by the British Columbia Geological Survey for its rare earth content and is now progressing with further exploration at Revel.
At the Taft Project, fieldwork conducted over the past summer included sampling and mapping, identifying both rare earth elements and gold mineralization. Taft is well-located near Salmon Arm, BC, with good road access and lower-elevation terrain, making it well-positioned for the resumption of exploration activities in early spring.
Mexico
Riverside continues to advance exploration across its gold and copper portfolio in Mexico, with significant progress at the Cuarentas, Ariel, and Union projects, among others.
At Cuarentas, the company has identified four priority target areas for drill testing. The project is drill-permitted and located on private ranch land, providing a clear path for further exploration and potentially rapid development including the existence of past mine and mill operations. With a history of high-grade mining and well-defined structural corridors, Cuarentas presents a strong opportunity for resource expansion. Riverside has made significant progress in target definition, using geochemistry, geophysics, remote sensing and geological mapping to refine drill targets.
At Ariel, Riverside is targeting a porphyry copper system characterized by large lithocaps, extensive alteration zones, breccia pipes, and veining-all indicators of a strong, undrilled porphyry copper discovery. Previous work has included mapping and geochemical sampling, particularly around former turquoise mining operations, which serve as surface indicators of deeper copper mineralization.
At the Union project in Sonora, Riverside controls three major mining areas within a large landholding. The project hosts high-grade gold potential in carbonate replacement deposits (CRDs), similar to those found in the Hermosa-Taylor deposit in Arizona, which South32 is actively developing. Union shares the same Paleozoic limestone host rocks, with an alteration halo of manganese, gold, and base metals suggesting the potential presence of a deeper porphyry copper system. CRD-style deposits in the region have historically led to significant copper discoveries, and Union remains a high-priority target for future exploration campaigns.
Other projects in Riverside’s portfolio include the Suaqui Verde project, which is currently under option to Southern Empire, and the neighboring Suaqui Grande copper project, which Riverside retains 100% ownership of. The company remains well-positioned, advancing its key assets while maintaining a strong royalty portfolio through option agreements.
Exploration efforts for H1 2025 continue across multiple projects, with further results expected from Cecilia and other key targets. Riverside also remains actively engaged in joint venture discussions, welcoming potential partnerships to advance its exploration programs. The company will be attending PDAC in Toronto, where it will be available for meetings and discussions. Further details on Riverside’s projects can be found on its website at www.rivres.com.
Qualified Person & QA/QC:
The scientific and technical data contained in this news release was reviewed and approved by Freeman Smith, P.Geo, a non-independent qualified person to Riverside Resources, who is responsible for ensuring that the geologic information provided within this news release is accurate and who acts as a “qualified person” under National Instrument 43-101 Standards of Disclosure for Mineral Projects.
About Riverside Resources Inc.
Riverside is a well-funded exploration company driven by value generation and discovery. The Company has over $4M in cash, no debt and less than 75M shares outstanding with a strong portfolio of gold-silver and copper assets and royalties in North America. Riverside has extensive experience and knowledge operating in Mexico and Canada and leverages its large database to generate a portfolio of prospective mineral properties. In addition to Riverside’s own exploration spending, the Company also strives to diversify risk by securing joint-venture and spin-out partnerships to advance multiple assets simultaneously and create more chances for discovery. Riverside has properties available for option, with information available on the Company’s website at www.rivres.com.
ON BEHALF OF RIVERSIDE RESOURCES INC.
“John-Mark Staude”
Dr. John-Mark Staude, President & CEO
For additional information contact:
| John-Mark Staude President, CEO Riverside Resources Inc. info@rivres.com Phone: (778) 327-6671 Fax: (778) 327-6675 Web: www.rivres.com | Eric Negraeff Investor Relations Riverside Resources Inc. Phone: (778) 327-6671 TF: (877) RIV-RES1 Web: www.rivres.com |
Certain statements in this press release may be considered forward-looking information. These statements can be identified by the use of forward-looking terminology (e.g., “expect”,” estimates”, “intends”, “anticipates”, “believes”, “plans”). Such information involves known and unknown risks — including the availability of funds, the results of financing and exploration activities, the interpretation of exploration results and other geological data, or unanticipated costs and expenses and other risks identified by Riverside in its public securities filings that may cause actual events to differ materially from current expectations. Readers are cautioned not to place undue reliance on these forward-looking statements, which speak only as of the date of this press release.
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/242583
As one of the lesser known but vital precious metals, Platinum has a long history of being used for jewelry and ornamentation, reaching back to the ancient Egyptian empire, having been discovered on a coffin unearthed in Thebes, estimated to be from the 7th century BC.
Platinum is a metal that represents power, prestige and a sense of great accomplishment. It has come to symbolize a high level of status in society, as evidenced by top-tier credit cards and membership programs using its name.
But Platinum has value beyond just being a status symbol. Modern-day uses of Platinum include being a key element in catalytic converters for vehicles, as it converts car exhaust gasses into less harmful substances, as a catalyst in the chemical industry and even in the creation of life-saving anti-cancer drugs.
Platinum was dubbed ‘platina’ or ‘little silver’ by the Spanish Conquistadors, and the truth is, it’s so much more than meets the eye.
But that’s just scratching the surface. On today’s episode, we explore this exclusive metal that befuddled miners and scientists alike when it was first discovered. Dubbed “platina” or “little silver” by the Spanish Conquistadors, the truth is, it’s so much more than meets the eye. Time to dig into Platinum on Commodity Culture.
Platinum is a gray-white precious metal and one of a group of six elements known as the Platinum Group Metals (PGM). The other metals in the group are iridium, osmium, palladium, rhodium and ruthenium. Platinum is the most common of the group and sees the most use.
Platinum’s atomic number is 78; it has an atomic mass of 195 units, a melting point of 1768 Degrees Celsius, and is resistant to corrosion, stable at high temperatures and has stable electrical properties.
The name Platinum comes from the Spanish word “platina,” basically translating to “little silver.” This somewhat derogatory word was coined by Spanish Conquistadors in the 16th century, as they had no idea of Platinum’s uses or true value and considered it an annoyance that interfered with their attempts to mine gold.
In those times, it was widely believed that “platina” was young gold and that, given time, it would turn yellow as it matured, but until then, better to toss it aside and get back to mining for the real thing.
Platinum is rarely found on its own; it is often deposited alongside gold, copper, iron, nickel, and the other Platinum Group Metals. When discovered, Platinum can be quite inconspicuous at first glance, with nuggets having a dull gray or black hue. One thing that can help identify platinum is its incredible heft when held and if iron is also present in the alloy, it will be slightly magnetic.
Some of the first known Platinum jewelry was crafted by the ancient indigenous peoples of Ecuador, with estimates placing their culture several centuries before the Spanish conquest of South America in 1492. It was particularly in the province of Esmeraldas where some of the most striking pieces were found, leading anthropologist William Farabee to declare:
“The native Indian workers of Esmeraldas were metallurgists of marked ability; they were the only people who manufactured Platinum jewelry.”
Considering Platinum is far more difficult to forge and manipulate than gold or silver, the method these ancient peoples used to work such a problematic metal was incredible and a testament to their dedication to their craft.
Platinum fragments were coated with gold dust, then heated by blowpipe on pieces of wood charcoal. The molten gold then caused the platinum to sinter, meaning it coalesced into a porous mass through heating, which allowed it to be forged.
Being the rarest of all the precious metals, along with its incredible strength as the hardest among them, has led Platinum to be one of the preferred forms of jewelry throughout the ages. In addition, it is highly resistant to scratches and other blemishes and does not wear away easily.
Platinum, along with the other Platinum Group Metals, has strong catalytic properties – meaning it can accelerate or trigger a chemical process without becoming permanently changed or consumed.
For this reason, Platinum is employed widely in the manufacturing of catalytic converters for use in exhaust systems in internal combustion vehicles. Platinum in exhaust systems helps curb vehicle pollution and contributes to enhanced air quality. Catalytic converters represent a whopping 50% of Platinum demand each year.
Due to its high melting point, Platinum is indispensable in chemical laboratories for electrodes and for crucibles and dishes in which materials can be heated to high temperatures.
In addition, Platinum is used in the chemicals industry as a catalyst to produce nitric acid, benzene and silicone. It is also used as a catalyst to improve the efficiency of fuel cells and for electrical contacts and sparking points, as it resists both the high temperatures and the chemical attack of electric arcs.
Platinum finds use in the electronics sector in the manufacturing of computer hard disks and thermocouples and is used to make optical fibers and LCD screens, turbine blades, spark plugs, pacemakers and, like other precious metals, is used widely in dentistry. Crowns, bridges, pins and other dental equipment, and fillings all employ Platinum as a key component.
Platinum is used as a catalyst in creating nitric acid, an essential ingredient in fertilizers, connecting Platinum to the creation of our food supply. But one of its more impactful uses to humanity is in the creation of chemotherapy drugs used to treat cancer, of which Platinum compounds are an important building block.
I’m willing to bet you didn’t think Platinum was such an essential element in our day-to-day lives, but the truth is, it’s a metal that is as practical as it is prestigious.
Next up, let’s explore the mining methods used to extract Platinum from the earth.
Being one of the rarest metals on earth, Platinum is rarely found on its own but is generally found alongside Platinum Group Metals, nickel, iron, gold and other metals. Although pure Platinum deposits have been discovered, they are the exception rather than the rule.
One of the earliest Platinum mining methods is placer mining. Like gold, Platinum particles can accumulate in alluvial sands in rivers and streams. Placer deposits are minerals concentrated in streams and riverbeds from rock eroded from its source and further ground into pieces as it is washed away by the water.
Most of the world’s placer Platinum is found in Russia and back in the 19th century, alluvial deposits located in the Ural Mountains were heavily mined by both small-scale family operations and more official mining operations.
Placer mining for Platinum was also common in South America, especially in the Río de la Plata, or the River of Silver, located between Argentina and Uruguay.
Placer mining involves using dredges to scoop Platinum-bearing sand or gravel from riverbeds and washing it until Platinum grains or nuggets are captured and separated from the surrounding material.
In today’s world, most Platinum deposits are located underground and are mined very similarly to gold, silver and other underground metal deposits, namely with strategically placed explosives.
Miners drill holes into the mine walls and pack explosives into them before detonating the rock, blasting it into small pieces and hauling it up to the surface to be loaded onto trucks, which then take it to a facility to be processed.
Most platinum mining in the modern era is done in South Africa, which accounts for a whopping 80% of world platinum production.
The story of the man who first identified Platinum and began to make it known to the greater world is no less fantastic than the element itself, involving an adventure across continents, a capture and daring escape on the high seas, and a scientific discovery that would begin Platinum’s journey to becoming the dynamic metal we know it as today.
Antonio de Ulloa of Spain was only 19 years of age when he was promoted to the rank of frigate lieutenant and sent on what would be a life-altering expedition to Quito in Ecuador, led by French geographers Charles Marie de la Condamine and Pierre Bouguer.
Antonio departed Spain in May of 1735, not knowing he wouldn’t see his motherland again for more than a decade. The mission was a monumental one: To help determine whether the earth was flat, as was popularly believed throughout most of human history up until that point, or whether it was a sphere, as suggested by Sir Isaac Newton.
To this end, it was necessary to measure the length of a degree of latitude at the equator, of which Quito was the closest city, and again at somewhere as near as possible to one of the poles. An expedition to the far north of Sweden was also dispatched for this purpose, but our story shall leave that journey to the pages of history.
As Antonio accompanied the geographers in Ecuador, their task proved epic indeed and with great struggle, they finally completed their work around 1745. Over the course of this decade, Antonio had plenty of time to explore the territory and the people there, recording his more interesting observations in various papers he carried with him.
As the expedition finally departed back to Spain, their mission accomplished, Antonio must have been filled with strong emotions as he was, at long last, headed home. Fate, however, had other plans in store for him.
As they made their way, sailing around Cape Horn, they were chased down north of the Azores by an English privateer and their ship was captured. However, they managed an escape and as luck seemed to be on their side, they evaded their captors and seemed to leave danger behind.
However, higher powers seemed intent on testing their wills and as they reached Louisbourg in Nova Scotia, their vessel was once again captured, this time by a British naval vessel and escape was out of the question. Antonio and his companions were taken to London and imprisoned, while the Admiralty confiscated nearly a decade’s worth of notes from Antonio’s time spent in Ecuador. Things looked grim for our frigate lieutenant as he sat in a cell awaiting his fate.
But this opened a window and good fortune came in the form of the President of the Royal Society, Martin Folkes, who came to know Antonio and his story and befriended him. The Royal Society was a group of natural philosophers and physicians, and not only did Martin free Antonio from his chains, but he also got all his papers returned to him and even made him a Fellow of the Royal Society in 1746. He was then allowed to return to Spain.
Finally, after his long mission, Antonio set to work compiling an account of his adventures, which he published in 1748, first in Spanish and then translated into several other languages.
For our subject today, one passage, in particular, stands out:
“In the district of Choco are many mines of lavadero or wash gold. Several of the mines have been abandoned on account of the Platina, a substance of such resistance, that when struck on an anvil of steel, it is not easy to be separated; nor is it calcinable, so that the metal enclosed within this obdurate body could only be extracted with infinite labor and charge.”
Shortly after releasing his book, Antonio was tasked with a new mission by the King of Spain, King Ferdinand VI, to travel throughout Europe and study scientific developments across the continent.
Antonio’s travels brought him to Sweden in the autumn of 1751 and he was welcomed with open arms by Swedish scientists. Shortly after his arrival, he was duly elected to the Royal Swedish Academy of Sciences in October of the same year. During his time there, he met with mathematician and chemist H.T. Scheffer. Scheffer was a former mine and metal works manager and an assayer at the mint and so had a vested interest in metals.
There is no official record of what exactly was said in that meeting, but shortly after that in November of 1751, Scheffer produced a paper titled, “The White Gold, or 7th Metal, called in Spain’ Platina del pinto’ Little Silver of Pinto, its Nature Described,” and submitted it to the Academy.
Scheffer was already familiar with Platinum before encountering Antonio, as he had received samples of it just a year earlier in 1750 from the West Indies, but his time with Antonio undoubtedly influenced his writing. In his paper, he came to the following conclusions about Platinum:
“That this is a metal hard but malleable, but of the hardness of malleable iron.
“That it is a precious metal of durability, like gold and silver.
“That it is not any of the six old metals, since first it is wholly and entirely a precious metal, containing nothing of copper, tin, lead, or iron, because it allows nothing to be taken from it. It is not silver, nor is it gold; but it is a seventh metal among those which are known up till now in all lands.”
In addition, he recommended a potential practical application for Platinum when he wrote:
“This metal is the most suitable of all to make telescope mirrors because it resists as well as gold the vapors of the air, it is very heavy, very dense, colorless and much heavier than ordinary gold, which is rendered unsuitable for this particular use by lacking these two latter properties.”
Although attempts were made in the years that followed, Platinum never found its place in the telescopes of the era, although Scheffer would be delighted to know the metal did eventually find use in the construction of x-ray telescopes centuries later. Nonetheless, Scheffer’s paper sparked the imaginations of scientists around the world, and a flurry of research into Platinum began, leading it to establish itself as the multifaceted metal that we know in the modern era.
Although the recent trend toward electrifying vehicles seemingly puts Platinum’s use in traditional gasoline-powered catalytic converters at risk, we need to step back and look at the bigger picture.
In the coming years, autocatalyst demand for Platinum is likely to rise as recent legislation to curb pollution from gasoline and diesel engines is boosting the demand for cleaner emissions, which is Platinum’s forte.
Either way, Platinum will have a role to play in a carbon-neutral future, as it is needed for hydrogen-powered fuel cell electric vehicles. These use a propulsion system similar to that of electric vehicles, where energy stored as hydrogen is converted to electricity by the fuel cell, and these vehicles are already becoming available in California and a few other places.
Platinum is also playing a role in the greater energy economy, as Platinum-based fuel cells are a cost-effective, clean and reliable off-grid power source that is currently seeing use in some remote areas, such as rural South Africa.
These fuel cells can help provide greater energy access to communities that might not normally be able to get a steady source of electricity. This includes electricity for schools, improving the quality of education and providing the ability to pump water for irrigation, facilitating agriculture.
Platinum’s other myriad uses also aren’t going away, and for this reason, Platinum will remain an essential metal to our modern civilization for as long as we can extract it from the earth.
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Jesse Day is not an employee or an affiliate of Sprott Asset Management LP. The opinions, estimates and projections (“information”) contained within this content are solely those of the presenter and are subject to change without notice. Sprott Asset Management LP makes every effort to ensure that the information has been derived from sources believed to be reliable and accurate. However, Sprott Asset Management LP assumes no responsibility for any losses or damages, whether direct or indirect, which arise out of the use of this information. Sprott Asset Management LP is not under any obligation to update or keep current the information contained herein. The information should not be regarded by recipients as a substitute for the exercise of their own judgment. Please contact your own personal advisor on your particular circumstances. Views expressed regarding a particular company, security, industry or market sector should not be considered an indication of trading intent of any investment funds managed by Sprott Asset Management LP. These views are not to be considered as investment advice nor should they be considered a recommendation to buy or sell.
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Kelowna, British Columbia–(Newsfile Corp. – February 12, 2025) – F3 Uranium Corp (TSXV: FUU) (OTCQB: FUUFF) (“F3” or “the Company“) is pleased to announce that persistent prospective geological characteristics were intersected in the last eight drill holes of the 2024 program focused on continued exploration and expansion of the B1 conductor and A1 extension, as well as further testing of the Harrison Fault area. Geochemistry and assay results from 25 drill holes from 2024 JR Zone and exploration drilling are still outstanding and will be incorporated into the 2025 drill planning and released as they come available.
B1 Conductor:
PLN24-188 tested the B1 conductor 120m north of PLN24-168 (currently the southernmost hole to intersect B1); the drillhole was lost in unconsolidated sand. Retested with hole PLN24-195 which intersected strong bleaching, clay and hematite alteration. PLN24-190 on line 3360S targeted between strong boron anomalies intersected in both PLN24-122 and PLN24-135. The hole intersected strong sandstone dissolution, graphitic faulting in basement and up to 420cps at 568.5m within a hematite altered fault zone. PLN24-193 attempted to test the Athabasca Sandstone above the B1 conductor in an area devoid of previous drilling. The hole intersected strong sandstone alteration and sulfides in the sandstone.
A1 Extension south of Harrison Fault:
PLN24-189 tested the A1 extension on line 3450S approximately 200m along strike south of radioactivity intersected in PLN24-187. The hole intersected 360cps at a depth of 419m and a strongly hematite, clay and sericite rich fault zone from 503.4-537.1m, interpreted to be the continuation of the A1 structure, extending the fault zone to nearly 620m south of Harrison Fault. PLN24-191 was abandoned prior to target depth due to excessive drillhole deviation.
Harrison Fault Area:
PLN24-192 tested the basement wedge along the Harrison Fault between holes PLN24-146 and PLN24-162. The hole successfully intersected the wedge and strong associated alteration, with the lower Athabasca Sandstone displaying strong alteration and dravite breccias (See Image 1). PLN24-194 was planned 100m northeast of hole PLN24-142, testing the Harrison Fault further to the northwest. The hole successfully intersected the fault zone from 266-335.5m containing strong graphite and sulphide alteration. The intersection of the Harrison Fault and the A1 and B1 conductors continues to display very encouraging alteration and large-scale complex structures supported by strong geochemistry, such as in drillhole PLN24-152. The area remains a high priority exploration target.
Map 1. Patterson Lake North, 2024 Scintillometer Results
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/8110/240184_d88abf7e443e3af9_002full.jpg
Table 1. Drill Hole Summary and Handheld Spectrometer Results
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https://images.newsfilecorp.com/files/8110/240184_d88abf7e443e3af9_003full.jpg
Handheld spectrometer composite parameters:
1: Minimum Thickness of 0.5m
2: CPS Cut-Off of 300 counts per second
3: Maximum Internal Dilution of 2.0m
Image 1: Brecciated Athabasca Sandstone in PLN24-192
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https://images.newsfilecorp.com/files/8110/240184_d88abf7e443e3af9_004full.jpg
Natural gamma radiation in the drill core that is reported in this news release was measured in counts per second (cps) using a handheld Radiation Solutions RS-125 scintillometer. The Company considers greater than 300 cps on the handheld spectrometer as anomalous, >10,000 cps as high grade and greater than 65,535 cps as off-scale. The reader is cautioned that scintillometer readings are not directly or uniformly related to uranium grades of the rock sample measured and should be used only as a preliminary indication of the presence of radioactive materials.
Samples from the drill core are split into half sections on site. Where possible, samples are standardized at 0.5m down-hole intervals. One-half of the split sample is sent to SRC Geoanalytical Laboratories (an SCC ISO/IEC 17025: 2005 Accredited Facility) in Saskatoon, SK while the other half remains on site for reference. Analysis includes a 63 element suite including boron by ICP-OES, uranium by ICP-MS and gold analysis by ICP-OES and/or AAS.
The Company considers uranium mineralization with assay results of greater than 1.0 weight % U3O8 as “high grade” and results greater than 20.0 weight % U3O8 as “ultra-high grade”.
All depth measurements reported are down-hole and true thicknesses are yet to be determined.
About the Patterson Lake North Property:
The Company’s 42,961-hectare 100% owned Patterson Lake North Project (PLN) is located just within the south-western edge of the Athabasca Basin in proximity to Paladin’s Triple R and NexGen Energy’s Arrow high-grade uranium deposits, an area poised to become the next major area of development for new uranium operations in northern Saskatchewan. The PLN Project consists of the 4,074-hectare Patterson Lake North Property, the 19,864-hectare Minto Property, and the 19,022-hectare Broach Property. All three properties comprising the PLN Project are accessed by Provincial Highway 955; the new JR Zone uranium discovery on the PLN property is located 23km northwest of Paladin’s Triple R deposit.
Qualified Person:
The technical information in this news release has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and approved on behalf of the company by Raymond Ashley, P.Geo., President & COO of F3 Uranium Corp, a Qualified Person. Mr. Ashley has verified the data disclosed.
About F3 Uranium Corp.:
F3 Uranium is a uranium exploration company, focusing on the recently discovered high-grade JR Zone on its Patterson Lake North (PLN) Project in the Western Athabasca Basin. F3 Uranium currently has 3 properties in the Athabasca Basin: Patterson Lake North, Minto, and Broach. The western side of the Athabasca Basin, Saskatchewan, is home to some of the world’s largest high grade uranium deposits including Triple R and Arrow and poised to become the next major area of high grade uranium operations in the world.
Forward-Looking Statements
This news release contains certain forward-looking statements within the meaning of applicable securities laws. All statements that are not historical facts, including without limitation, statements regarding future estimates, plans, programs, forecasts, projections, objectives, assumptions, expectations or beliefs of future performance, including statements regarding the suitability of the Properties for mining exploration, future payments, issuance of shares and work commitment funds, entry into of a definitive option agreement respecting the Properties, are “forward-looking statements.” These forward-looking statements reflect the expectations or beliefs of management of the Company based on information currently available to it. Forward-looking statements are subject to a number of risks and uncertainties, including those detailed from time to time in filings made by the Company with securities regulatory authorities, which may cause actual outcomes to differ materially from those discussed in the forward-looking statements. These factors should be considered carefully and readers are cautioned not to place undue reliance on such forward-looking statements. The forward-looking statements and information contained in this news release are made as of the date hereof and the Company undertakes no obligation to update publicly or revise any forward-looking statements or information, whether as a result of new information, future events or otherwise, unless so required by applicable securities laws.
The TSX Venture Exchange and the Canadian Securities Exchange have not reviewed, approved or disapproved the contents of this press release, and do not accept responsibility for the adequacy or accuracy of this release.
F3 Uranium Corp.
750-1620 Dickson Avenue
Kelowna, BC V1Y9Y2
Contact Information
Investor Relations
Telephone: 778 484 8030
Email: ir@f3uranium.com
ON BEHALF OF THE BOARD
“Dev Randhawa”
Dev Randhawa, CEO
To view the source version of this press release, please visit https://www.newsfilecorp.com/release/240184
Kelowna, British Columbia–(Newsfile Corp. – February 11, 2025) – F3 Uranium Corp (TSXV: FUU) (OTCQB: FUUFF) (“F3” or “the Company“) is pleased to announce that ground geophysical exploration programs have commenced on the Broach and Minto Properties. A total of 55 line km of Moving Loop TDEM ground EM will be undertaken on two grids of interest testing suspected conductive corridors previously identified by airborne surveys, and both parallel to the A1 conductor system which hosts the high grade JR Zone on the PLN property.
Minto Property: A4 Grid
14 line-km of MLTDEM ground geophysics testing an approximately 7,200m long conductive corridor identified by airborne MobileMT which was flown by F3 in 2023. F3 has one hole drilled on this grid in 2014; PLN14-021 intersected up to 44ppm uranium in basement, and 698ppm boron directly above the Athabasca Unconformity at 413m. Anomalous geochemistry and proximity to the Harrison fault in a corridor parallel to the A1 conductor make this grid a strong exploration target area.
Broach Property: PW Grid
41 line-km of MLTDEM ground geophysics covering a suspected conductive trend, approximately 12km south of, and parallel to the JR Zone. This particular area of the Broach property hosts thick discontinuous layers of conductive mudstones and these flat lying conductive units hampered the effectiveness of a previously flown airborne EM (VTEMmax) survey flown in 2014. Ground based geophysics is anticipated to effectively penetrate the conductive cover allowing for drill target generation. Due to its location near the interpreted Athabasca Basin boundary and the historic difficulty of exploring under conductive cover, this large area remains underexplored.
Sam Hartmann, Vice President Exploration, commented:
“We are excited with the prospect of upgrading the Broach and Minto properties to the drilling stage with this round of ground EM, which we anticipate assisting in reducing broader airborne conductivity responses to more precise conductor models for drill testing. At the A4 grid, where some historic ground EM coverage prompted us to drill a single hole in 2014, this new ground EM will give us an improved conductor model, in a strategic location near the projected confluence of the Harrison Fault with the A4 conductive corridor. At the PW grid, we are aiming to generate a conductivity model in an area where no previous airborne EM conductors have been clearly identified, near the margins of the Athabasca Basin in an area of very limited historical drilling. Identifying ground conductors near the present day margins of the basin is something that we are specifically interested in. Additionally, recent re-modelling of historic ground EM surveys south of Broach Lake has resulted in an additional target; the northeast trending BRS conductor. This suspected structure sits along favorable MT conductivity, and we look forward to upgrading the BRS conductor to the drilling stage as well with ground EM surveying.”
Map 1. Broach and Minto Properties, 2025 Exploration
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https://images.newsfilecorp.com/files/8110/240183_e1a7c21b142cbb01_002full.jpg
About the Patterson Lake North Project:
The Company’s 42,961-hectare 100% owned Patterson Lake North Project (PLN) is located just within the south-western edge of the Athabasca Basin in proximity to Fission Uranium’s Triple R and NexGen Energy’s Arrow high-grade world class uranium deposits which is poised to become the next major area of development for new uranium operations in northern Saskatchewan. The PLN Project consists of the 4,074-hectare Patterson Lake North Property, the 19,864-hectare Minto Property, and the 19,022-hectare Broach Property. All three properties comprising the PLN Project are accessed by Provincial Highway 955; the new JR Zone uranium discovery on the PLN property is located 23km northwest of Fission Uranium’s Triple R deposit.
Qualified Person:
The technical information in this news release has been prepared in accordance with the Canadian regulatory requirements set out in National Instrument 43-101 and approved on behalf of the company by Raymond Ashley, P.Geo., President & COO of F3 Uranium Corp, a Qualified Person. Mr. Ashley has verified the data disclosed.
About F3 Uranium Corp.:
F3 Uranium is a uranium exploration company, focusing on the recently discovered high-grade JR Zone on its Patterson Lake North (PLN) Project in the Western Athabasca Basin. F3 Uranium currently has 3 properties in the Athabasca Basin: Patterson Lake North, Minto, and Broach. The western side of the Athabasca Basin, Saskatchewan, is home to some of the world’s largest high grade uranium deposits including Triple R and Arrow and poised to become the next major area of high grade uranium operations in the world.
Forward Looking Statements
This news release contains certain forward-looking statements within the meaning of applicable securities laws. All statements that are not historical facts, including without limitation, statements regarding future estimates, plans, programs, forecasts, projections, objectives, assumptions, expectations or beliefs of future performance, including statements regarding the suitability of the Properties for mining exploration, future payments, issuance of shares and work commitment funds, entry into of a definitive option agreement respecting the Properties, are “forward-looking statements.” These forward-looking statements reflect the expectations or beliefs of management of the Company based on information currently available to it. Forward-looking statements are subject to a number of risks and uncertainties, including those detailed from time to time in filings made by the Company with securities regulatory authorities, which may cause actual outcomes to differ materially from those discussed in the forward-looking statements. These factors should be considered carefully and readers are cautioned not to place undue reliance on such forward-looking statements. The forward-looking statements and information contained in this news release are made as of the date hereof and the Company undertakes no obligation to update publicly or revise any forward-looking statements or information, whether as a result of new information, future events or otherwise, unless so required by applicable securities laws.
The TSX Venture Exchange and the Canadian Securities Exchange have not reviewed, approved or disapproved the contents of this press release, and do not accept responsibility for the adequacy or accuracy of this release.
F3 Uranium Corp.
750-1620 Dickson Avenue
Kelowna, BC V1Y9Y2
Contact Information
Investor Relations
Telephone: 778 484 8030
Email: ir@f3uranium.com
ON BEHALF OF THE BOARD
“Dev Randhawa”
Dev Randhawa, CEO
To view the source version of this press release, please visit https://www.newsfilecorp.com/release/240183
In this episode of ‘Proven and Probable,’ we engage with Bob Moriarty, a distinguished commentator on geopolitical and economic affairs. Bob’s extensive experience includes serving as a Marine F-4B pilot during the Vietnam War, where he flew over 820 combat missions and became one of the most highly decorated pilots of the conflict.
We delve into the recent tragic collision between an American Airlines plane and a military helicopter near Washington, D.C., exploring Bob’s insights on the incident, the National Transportation Safety Board’s investigative approach, and media coverage.
The discussion also covers U.S. tariff policies, international responses, and the current state of gold and precious metals, providing a comprehensive analysis of these pressing issues.
Join us for an in-depth conversation that offers clarity and depth on these complex topics.
Vancouver, British Columbia–(Newsfile Corp. – February 5, 2025) – Riverside Resources Inc. (TSXV: RRI) (OTCQB: RVSDF) (FSE: 5YY) (“Riverside” or the “Company”), is pleased to announce that the next stage of exploration is now progressing, following the successful completion of the joint Q4 2024 drilling program at the Cecilia Gold Project in Sonora, Mexico. The drill program was conducted in partnership with Fortuna Mining, which continues to advance their earn-in option on the project (See news release: March 13, 2024). Riverside, acting as the operator, completed an initial five-hole, 2,250-meter drilling campaign designed to test four distinct target areas generally with one geological evaluation drill hole per target to seek scale and evidence of a potentially strong hydrothermal system which would set up for a follow up 2025 exploration program which has now begun. The drilling in Q4 hit favorable indicators as outlined below and continued to develop the district scale targets both at Cerro Magallanes and on the broader >60 km sq property package with vast areas to expand.
The drill program announced in September (See press release: September 10, 2024), where Riverside outlined its goals to define and expand key targets at Cecilia. The latest program hit gold mineralization in each target area and broader epithermal alteration consistent with target styles like the nearby Mercedes Mine Sonora and Oatman Gold District Arizona. At Magallanes Hill, two holes were drilled at the San Jose target, followed by one hole on the eastern flank, referred to as the East Target. Additionally, two holes were drilled in the Mesa area to the south: one testing the Mayra Vein concept and the final hole drilled eastward to intersect the Mesa Fault, a significant structural target.
“We are encouraged by the results of the Q4 2024 drilling program, which focused on testing geological features with limited previous drilling, just one or two holes in each area, and yielded positive indicators while also uncovering some unexpected geologic surprises,” said John-Mark Staude, President and CEO of Riverside Resources. “This program not only confirmed earlier gold intercepts but also expanded the scale of exploration with significant step-outs and new target areas. The ongoing work underscores our commitment to unlocking new opportunities and delivering sustained value to our stakeholders.”
Highlights of the Drill Program:
San Jose Vein System (North Breccia): Two holes were drilled to extend testing of this structure, building upon results from previous drilling and assay work. The San Jose system has shown significant mineralization potential, as highlighted in prior programs including samples returning values of up to 48.3 g/t Au over 0.75 m at surface (See press release: January 28, 2021). Drilling to depths of 500 to 800 meters successfully intersected the San Jose structure in both holes, confirming the continuity of this extensive vein system. Notably, hole CED24-010 returned an intercept of 3.41 g/t Au over 4 meters, starting at a depth of 76 meters, with an additional lower intercept including 0.39 g/t Au over 5.25m starting at 319m identified along the projected extension of the San Jose vein which topographically is over 500m below the Magallanes peak and previous drill intercepts in the upper part of the San Jose vein system. These results are illustrated in the cross-section below.
East Target: A single hole was drilled perpendicular to known mineralization identified in surface samples and previous drilling by Cambior (1996). This hole crossed through thick zones of alteration, adding valuable geological data for this target and confirming that Cecilia has strong feeder zones for gold. The hole intersected at least 6 gold bearing intervals with one being 0.38 g/t Au over 1.75m starting from 149.25m. This hole was drilled eastward in order to constrain the dip as past drill holes had been drilled westward. The single new hole intercepted multiple veins for this part of the eastern Magallanes system as shown on the map below and on the Company website
Mesa Ranch Area (Mayra Vein): The 2024 program was the first time the Mayra Vein has been tested with this the first drill to be conducted on the broader Cecilia project, which encompasses over a dozen identified targets. This hole was intended to test the northwest trending epithermal veins related with felsic dikes that potentially feed toward and likely cut the Puma Dome. These district-scale targets from the Mesa Ranch area have potential along strike for further exploration. Core drill hole CED24-011 intersected multiple vein zones, including an interval of 0.21 g/t Au over 2 meters starting at 281 meters. The gold-bearing interval featured quartz veining and oxides whose projection aligns with surface-sampled veins that extend over 700 meters along strike, further highlighting the potential and continued interest in these vein systems.
South Mesa Fault Zone (Mesa South): The final hole of the program focused on the extensive South Mesa Fault; a 10 km-long structure comparable to fault-controlled gold systems like those in Nevada’s Midas District. Drill hole CED24-012 intersected the fault at 110m and comprises a 5m thick interval of sheared brecciated rock which can be projected to surface and followed along strike. Surface samples returned gold values of over 2 g/t gold along the surface projection of this fault. Plans are in place for additional exploration of the Mesa South region for the first half of 2025, which will include tracking the Mesa fault’s continuity along strike.
The table below summarizes the locations and depths for the five holes completed in this first drilling round with Fortuna Mining.
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6101/239658_ceciliatable.jpg
The drilling location map below shows the 5 holes (3 drill pads) which correlate with the drill hole descriptive table above. Drill hole CED24-008 at Magallanes was deeper than any previous drilling. Figure 1 shows the drill traces as they intersected the down dip projection of the veins.
Figure 1– Geology map and location of the five 2024 drill holes shown in red. The straight and thin black lines near Magallanes are drill holes from previous campaigns. This new program stepped out to test the East Target (CED24-009) and the Mayras and South Mesa with single holes.
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6101/239658_0363d2fe54345ab7_003full.jpg
The cross-section figure below highlights hole CED24-010 from the drill program, which demonstrates the intersections of multiple vein structures. These structures are now interpreted to potentially extend over 800 meters vertically, suggesting they could be part of a significant epithermal system. Further exploration is planned for 2025, including an MT (Magneto-telluric) geophysical survey to refine our targeting of the system. Based on the results of these surveys, additional drilling may be undertaken to further evaluate the system’s potential. The Project includes numerous untested targets throughout the 60 km sq land package.
Figure 2: Cross section of the Magallanes Dome showing the volcanic units and structures
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/6101/239658_0363d2fe54345ab7_004full.jpg
This drill program advanced the understanding of the Cecilia system’s geology, confirming significant low-sulfidation epithermal features in the Cerro Magallanes area. Data from the drilling suggests the mineralization system is tilted southeast, supported by surface mapping, geochemical analysis, and structural modeling.
The Cecilia Gold Project continues to demonstrate significant potential. Fortuna Mining’s technical expertise and funding have enabled systematic exploration, with the partnership potentially targeting a larger follow-up program in 2025. The drilling positively demonstrated scale and alterations consistent with a mineralized system worthy of more advanced drilling in addition to continued target testing.
Stock Option Grant:
On February 4th, 2025, the Company granted 1,450,000 incentive stock options (the “Options”) to certain Directors, Officers and Consultants of the Company. The Options are exercisable at $0.13 per share for a period of 5 years from the date of grant. Options granted to individuals in their capacity as a director vest in 3 equal instalments over 18 months. Options granted to Officers and Consultants vest in 4 equal instalments over 12 months. The Options were granted pursuant to the Company’s shareholder approved stock option plan and are subject to the policies of the TSX Venture Exchange and any applicable regulatory hold periods.
Qualified Person & QA/QC:
The scientific and technical data contained in this news release pertaining to the Cecilia Project was reviewed and approved by Freeman Smith, P.Geo, a non-independent qualified person to Riverside Resources who is responsible for ensuring that the information provided in this news release is accurate and who acts as a “qualified person” under National Instrument 43-101 Standards of Disclosure for Mineral Projects.
Drill core samples were sealed with zip straps and picked up by Bureau Veritas at site who took custody and drove samples to the Bureau Veritas Laboratories in Hermosillo, Mexico for fire assaying for gold. The rejects remained with Bureau Veritas in Mexico while the pulps were transported to Bureau Veritas’ laboratory under their custody to Vancouver, BC, Canada and analyzed for 45 elements using their ICP/ES-MS analysis. A QA/QC program was implemented as part of the sampling procedures for the exploration program. Standards, duplicates and blanks were inserted into the sample stream prior to being sent to the laboratory. The QA/QC analysis was completed with results fitting well with standards, blanks and duplicates not varying beyond normal statistical variance.
About Riverside Resources Inc.:
Riverside is a well-funded exploration company driven by value generation and discovery. The Company has over $4M in cash, no debt and less than 75M shares outstanding with a strong portfolio of gold-silver and copper assets and royalties in North America. Riverside has extensive experience and knowledge operating in Mexico and Canada and leverages its large database to generate a portfolio of prospective mineral properties. In addition to Riverside’s own exploration spending, the Company also strives to diversify risk by securing joint-venture and spin-out partnerships to advance multiple assets simultaneously and create more chances for discovery. Riverside has properties available for option, with information available on the Company’s website at www.rivres.com.
ON BEHALF OF RIVERSIDE RESOURCES INC.
“John-Mark Staude”
Dr. John-Mark Staude, President & CEO
For additional information contact:
| John-Mark Staude President, CEO Riverside Resources Inc. info@rivres.com Phone: (778) 327-6671 Fax: (778) 327-6675 Web: www.rivres.com | Eric Negraeff Investor Relations Riverside Resources Inc. Phone: (778) 327-6671 TF: (877) RIV-RES1 Web: www.rivres.com |
Certain statements in this press release may be considered forward-looking information. These statements can be identified by the use of forward-looking terminology (e.g., “expect”,” estimates”, “intends”, “anticipates”, “believes”, “plans”). Such information involves known and unknown risks — including the availability of funds, the results of financing and exploration activities, the interpretation of exploration results and other geological data, or unanticipated costs and expenses and other risks identified by Riverside in its public securities filings that may cause actual events to differ materially from current expectations. Readers are cautioned not to place undue reliance on these forward-looking statements, which speak only as of the date of this press release.
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/239658
Vancouver, British Columbia–(Newsfile Corp. – February 4, 2025) – EMX Royalty Corporation (NYSE American: EMX) (TSXV: EMX) (the “Company” or “EMX”) congratulates EMX board member, Mr. Chris Wright, on his confirmation as U.S. Secretary of Energy under President Donald Trump. Mr. Wright was confirmed as Secretary on February 3, 2025 in a bipartisan vote in the U.S. Senate and will now join the Cabinet of the United States in Washington, D.C. Mr. Wright is known for his innovations and entrepreneurial contributions to the energy sector, but also for his focus on humanitarian efforts such as co-founding the Bettering Human Lives Foundation. He has been a spirited contributor at EMX board meetings and management discussions. As a consequence of his confirmation, Mr. Wright will step down from the board of EMX. The Company sincerely thanks Mr. Wright for his contributions at EMX and is excited to observe his future role in leading and shaping the energy policy of the United States.
About EMX – EMX is a precious and base metals royalty company. EMX’s investors are provided with discovery, development, and commodity price optionality, while limiting exposure to risks inherent to operating companies. The Company’s common shares are listed on the NYSE American Exchange and TSX Venture Exchange under the symbol “EMX”. Please see www.EMXroyalty.com for more information.
For further information contact:
David M. Cole
President and CEO
Phone: (303) 973-8585
Dave@EMXroyalty.com
Isabel Belger
Investor Relations
Phone: +49 178 4909039
IBelger@EMXroyalty.com
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
Forward-Looking Statements
This news release may contain “forward looking statements” that reflect the Company’s current expectations and projections about its future results. These forward-looking statements may include statements regarding perceived merit of properties, exploration results and budgets, mineral reserves and resource estimates, work programs, capital expenditures, timelines, strategic plans, market prices for precious and base metal, or other statements that are not statements of fact. When used in this news release, words such as “estimate,” “intend,” “expect,” “anticipate,” “will”, “believe”, “potential” and similar expressions are intended to identify forward-looking statements, which, by their very nature, are not guarantees of the Company’s future operational or financial performance, and are subject to risks and uncertainties and other factors that could cause the Company’s actual results, performance, prospects or opportunities to differ materially from those expressed in, or implied by, these forward-looking statements. These risks, uncertainties and factors may include, but are not limited to unavailability of financing, failure to identify commercially viable mineral reserves, fluctuations in the market valuation for commodities, difficulties in obtaining required approvals for the development of a mineral project, increased regulatory compliance costs, expectations of project funding by joint venture partners and other factors.
Readers are cautioned not to place undue reliance on these forward-looking statements, which speak only as of the date of this news release or as of the date otherwise specifically indicated herein. Due to risks and uncertainties, including the risks and uncertainties identified in this news release, and other risk factors and forward-looking statements listed in the Company’s MD&A for the quarter ended September 30, 2024 (the “MD&A”), and the most recently filed Annual Information Form (“AIF”) for the year ended December 31, 2023, actual events may differ materially from current expectations. More information about the Company, including the MD&A, the AIF and financial statements of the Company, is available on SEDAR at www.sedarplus.ca and on the SEC’s EDGAR website at www.sec.gov.
To view the source version of this press release, please visit https://www.newsfilecorp.com/release/239599