Cruz Announces Intent to Spin-Out the Hector Silver-Cobalt Project

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Vancouver, British Columbia--(Newsfile Corp. - August 1, 2024) - Cruz Battery Metals Corp. (CSE: CRUZ) (OTC Pink: BKTPF) (FSE: A3CWU7) ("Cruz" or the "Company") is pleased to announce its intention to undertake a strategic reorganization of certain of the Company's mineral exploration assets pursuant to which the Company proposes to spin-out (the "Spin-Out") its Hector Silver-Cobalt Project located near Cobalt, Ontario (the "Hector Property") into a recently incorporated, wholly-owned subsidiary, Makenita Resources Inc. ("SpinCo").

James Nelson, President of Cruz states, "This spinout makes sense for our shareholders. To unlock the value of the Silver-Cobalt asset as a standalone project will enable the shareholders of record of Cruz to benefit from ownership in two companies. Cruz is focused on its lithium projects in Nevada and expects to have a work program this summer. Cruz shareholders will achieve a win-win scenario as they will be shareholders of each company at no cost to them. Management is optimistic about the future of each company and hopes the Cruz shareholders of record will share the excitement."

The Hector Property consists of 126 contiguous unpatented mining claims totalling 2,243 hectares (5,542-acres) and is located within the Coleman and Gillies Limit Townships, Larder Lake Mining Division, Timiskaming District, Ontario, Canada. The Property is approximately 500 kilometres (km) north of Toronto, 150 km north of North Bay, and 10 km southwest of the town of Cobalt, Ontario. Cruz holds 100% ownership of the 126 mining claims, which are active and in good standing.

The principal deposit type of interest within the Hector Property is arsenide silver-cobalt vein deposits, which are epigenetic vein deposits. Metallic minerals occur in fracture filling lenses or veinlets, or as disseminations within wall rocks in association with carbonate and/or quartz gangue. Wall rocks adjacent to the veins are commonly hydrothermally altered. The majority of mineral occurrences with the Hector Property consist of narrow fracture controlled northwest-southeast, or northeast-southwest striking, sub-vertical to steeply dipping, quartz-carbonate-potassium feldspar veins containing variable percentages of disseminated to clotty pyrite, chalcopyrite, pyrrhotite, and erythrite (hydrous cobalt arsenate) mineralization. Veins range in width from less than 5 cm up to 25 cm in width. The majority of historically reported mineral occurrences are represented by one or more shallow prospect pits and trenches, or water-filled shafts.