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Coquitlam, BC – TheNewswire – September 21, 2023- Grid Battery Metals Inc. (the “Company” or “Grid Battery”) (TSXV:CELL), (OTC:EVKRF), (FRA:NMK2) announces that further to its news release that was dated September 21, 2023, the Company has closed a non-brokered private placement financing offering of 4,000,000 units (“Units”) at a price of CAD$0.12 per Unit for gross proceeds of CAD$480,000 and not $240,000.
Each Unit is comprised of one common share and one share purchase warrant (“Warrant”). Each Warrant will entitle the holder thereof to purchase one additional common share of the Company at an exercise price of CAD$0.155 per share for a period of five years from closing, subject to TSX Venture Exchange (“Exchange”) approval.
The Company also paid finder fees in the amount of 400,000 shares in connection with the private placement. The finder fees are subject to Exchange approval.
All securities issued in connection with the private placement are subject to a four‐month and a day hold period expiring on January 22, 2024 in accordance with applicable Canadian Securities Laws.
The proceeds of the Private Placement will be used for exploration and development and for general working capital purposes.
About Grid Battery Metals Inc.
Grid Battery Metals Inc. is a Canadian based exploration company whose primary listing is on the TSX Venture Exchange. The Company’s maintains a focus on exploration for high value battery metals required for the electric vehicle (EV) market. www.gridbatterymetals.com.
About Texas Springs Property
The Company owns a 100% interest in the Texas Spring Property which consists of mineral lode claims located in Elko County, Nevada. The Property is in the Granite Range southeast of Jackpot, Nevada, about 73 km north-northeast of Wells, Nevada. The target is a lithium clay deposit in volcanic tuff and tuffaceous sediments of the Humbolt Formation.
The Texas Spring property adjoins the southern border of the Nevada North Lithium Project – owned by Surge Battery Metals Inc. (“Surge”) (TSXV: NILI, OTC: NILIF) and comprised of 303 mineral claims. Surge’s first round of drilling identified strongly mineralized lithium bearing clays. The average lithium content within all near surface clay zones intersected in the 2022 drilling program, applying a 1000 ppm cut-off, was 3254 ppm. (Press release March 29, 2023). More recent results have shown higher grade lithium up to 8070 ppm on this property after initial drilling (Press release September 12, 2023).
About Clayton Valley Lithium Project
The Company owns a 100% interest in 113 lithium lode and placer claims covering over 640 hectares in Clayton Valley. Clayton Valley is a down-dropped closed basin formed by the Miocene age Great Basin extension and is still active due to movement along the Walker Lane structural zone. As a result, the basin has preserved multiple layers of lithium bearing volcanic ash, resulting from multiple eruptive events over the past 6 million years including eruptions from the 700,000-year-old Long Valley Caldera system and related events. These ash layers are thought to contribute to the lithium brines extracted by Albemarle and are also likely involved in the formation of the exposed lithium rich clay deposits on the east side of Clayton Valley.
Volt Canyon Lithium Property
The Company owns a 100% interest in 80 placer claims covering approximately 635 hectares of alluvial sediments and clays located 122 km northeast of Tonopah, Nevada.
About the British Columbia, Nickel Projects
The Mount Sidney Williams Group consists of three claim blocks with a total area of 10,569 hectares in the area surrounding Mount Sidney Williams, both adjoining and near the Decar project of FPX Nickel Corp., located 100 kilometres northwest of Fort St. James, B.C., in the Omineca mining division. Metallic mineralization includes nickel, cobalt, and chromium. At least some of the nickel mineralization occurs as awaruite. The Mitchell Range Group area claim consists of one claim block covering 8,659 hectares with demonstrated metallic mineralization including nickel, cobalt, and chromium. Nickel cobalt mineralization has not been well explored, but the presence of awaruite has been documented.
On Behalf of the Board of Directors
“Tim Fernback”
Tim Fernback, President & CEO
Contact Information:
Email: [email protected]
Phone: 604- 428-5690
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. This news release may contain forward-looking statements which include, but are not limited to, comments that involve future events and conditions, which are subject to various risks and uncertainties. Except for statements of historical facts, comments that address resource potential, upcoming work programs, geological interpretations, receipt and security of mineral property titles, availability of funds, and others are forward-looking. Forward-looking statements are not guarantees of future performance and actual results may vary materially from those statements. General business conditions are factors that could cause actual results to vary materially from forward-looking statements.
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