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Prismo Metals Acquires Data and Updates Model for Hot Breccia Copper Project in Arizona

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VANCOUVER, BC / ACCESSWIRE / September 3, 2024 / Prismo Metals Inc. (the "Company") (CSE:PRIZ)(OTCQB:PMOMF)(FSE:7KU) is pleased to announce that it has updated the mineralization model for the Hot Breccia project in Southern Arizona based on important historical information recently acquired from a third party. The information includes historic Bear Creek Mining Company (then a subsidiary of Kennecott Copper Co. (now part of Rio Tinto, ASX: RIO) exploration data, gathered between the completion of a masters thesis by Larry Barrett (1972) (1) through the completion of their first drill hole on our Hot Breccia property between 1972 and mid-1974. The recently acquired information includes a complete log and assays for hole OC-1 and a geological interpretation after holes OC-1 to OC-3 were completed(2).

An important portion of the acquired data shows the distribution of post mineral quartz diorite dikes containing fragments of copper bearing mineralization brought up from depth (Fig 2), as well as the location of shallow and deep IP anomalies compiled from several different sources. The shallow IP anomaly follows the orientation of the swarm of quartz diorite dikes, probably reflecting pyrite bearing alteration associated with it. The deeper IP anomaly covers much of the central portion of the claim block and may be related to alteration around a mineralized intrusion or a related sulfide body. Bear Creek's interpretation of the IP data indicates that mineralization is present over a larger area than they had previously recognized. Notably, their deep IP anomaly, as well as the distribution of copper bearing xenoliths in quartz diorite dikes, correspond closely to the area of the conductive anomaly identified in Prismo's 2023 ZTEM geophysical survey (Fig. 2) (see News Release of February 9, 2024).

Also, included in the Bear Creek data is the complete description and assay data for hole OC-1, drilled to a depth of 733 meters in early 1974 (Fig 2), as well as an interpretation of the results by Barrett (1974)(2) (Fig 3). Hole OC-1 was collared in the area of one of the property's namesake breccias that hosts copper skarn fragments sourced from deep below the surface. A Prismo sample of one of these fragments assayed 5.7% copper, as reported in the Company's News Release dated March 26, 2024.

Prismo Metals previously possessed only a portion of the OC-1 drill log to a depth of 295 meters, all in volcanic rocks, with only summary assay data that indicated a mineralized interval deeper in the hole. According to the new data, hole OC-1 cut 403 meters of Cretaceous volcanic and volcano-sedimentary rocks as expected from the geology in the area, followed by an interval of 330 meters of quartz diorite porphyry including a pyritic and copper-bearing stock not exposed at the surface. Bear Creek suggested that this quartz porphyry includes an intrusive phase interpreted to be associated with mineralization, cut by later dikes that include fragments of previously formed skarn. The mineralized porphyry includes a 23.5-meter pendant of skarn mineralization averaging 0.54% Cu including 1.8 meters of 1.81% Cu. The hole was strongly copper-anomalous to the bottom and ended in mineralization.