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Cosa Resources Reports Uranium Assays from the 100% Owned Ursa Project, Athabasca Basin, Saskatchewan

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Vancouver, British Columbia--(Newsfile Corp. - December 19, 2024) - Cosa Resources Corp. (TSXV: COSA) (OTCQB: COSAF) (FSE: SSKU) ("Cosa" or the "Company") is pleased to report assay results from basement-hosted radioactivity intersected in the fall drilling program at the Company's 100% owned Ursa uranium Project in the Athabasca Basin, Saskatchewan ("Ursa" or the "Property").

Highlights

  • Uranium confirmed as source of anomalous radioactivity intersected by UR24-06, including 0.22% U3O8 over 0.7 metres

  • Uranium mineralization in UR24-06 is the strongest and widest intersected to date on the Project

  • Cosa's 2024 exploration confirmed prospective geology is present at Ursa and developed numerous follow-up targets which remain untested

Andy Carmichael, Vice President Exploration, commented: "In only 18 months, Cosa has significantly derisked the Ursa Project and proven that the geology of the Kodiak trend is highly consistent with that underpinning producing mines in the eastern Athabasca. Our strategy of using large-scale Ambient Noise Tomography (ANT) surveys to prioritize conductive strike produced the strongest and widest mineralization on the Project from our very first drill hole to test an ANT target. With only 21 drill holes completed within the 65-kilometre-long Project, Ursa has vast underexplored and increasingly prospective exploration space to fit multiple tier-1 deposits, and we have demonstrated that modern geophysical surveys have produced target areas far beyond conventional EM alone."

UR24-06 Assay Results

Chemical assays have confirmed that uranium mineralization is the source of radioactivity intersected by UR24-06 (See Cosa news release dated October 30, 2024). As at basement-hosted uranium deposits in the region (e.g, Gryphon, Arrow, and Eagle Point), mineralization is monometallic and significant enrichment of uranium pathfinder elements such as arsenic, nickel, and cobalt is not present.

The mineralization was intersected by drill hole UR24-06 (Table 1) which tested an ANT anomaly along the Kodiak conductive trend interpreted to reflect favourable structural disruption and/or hydrothermal alteration of the Athabasca sandstone. UR24-06 intersected a zone of sandstone-hosted structure and alteration from 814 to 923 metres. The unconformity was intersected at 1033.0 metres. Multiple intervals of basement-hosted uranium mineralization were intersected between 1087.8 and 1116.8 metres. The strongest mineralization is between 1088.6 and 1089.3 metres where disseminated and fracture-filling uranium mineralization within weakly graphitic and pyritic pelitic gneiss averaged 0.22% U3O8 over 0.7 metres. Several additional intervals of weak uranium mineralization were intersected as much as 84 metres below the unconformity with a strong correlation to increased pervasive hematite alteration. As UR24-06 did not intersect conductive basement rocks and mineralization is located more than 50 metres below the unconformity, the drill hole is interpreted to have missed the optimal target.