Prismo Metals To Resume Drilling at Palos Verdes

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Prismo Samples 930 g/t Silver and 10.55 g/t gold at Palos Verdes (2,605 g/t AgEq*)

Vancouver, British Columbia--(Newsfile Corp. - February 6, 2024) - Prismo Metals Inc. (CSE: PRIZ) (OTCQB: PMOMF) ("Prismo" or the "Company") is pleased to provide an update for its exploration program at the Palos Verdes property located in the Panuco district in Mexico. Following the completion of its third drill campaign with 2,923 meters drilled in 15 holes, and in preparation of the upcoming expanded drill program to be drilled from Vizsla Silver Corp. (TSXV: VZLA) ("Vizsla") concessions adjacent to the Palos Verdes concession, the Company completed an alteration and geochemical study over the Palos Verdes property. This study was recommended by the Joint Prismo/Vizsla Technical Committee which is comprised of Prismo's CEO Dr. Craig Gibson, Vizsla Silver's VP Exploration Dr. Jesus Velador and Dr. Peter Megaw.

The results of this work indicate the possibility that the mineralized shoot defined by drilling to date on the west side of the property may be truncated and offset downward along a cross fault, and that a second blind mineralized shoot may exist to the northeast along the Palos Verdes vein.

Dr. Craig Gibson, President and CEO of the Company, stated, "The alteration study provides further evidence that our hypothesis for a downward offset of the northeastern portion of the Palos Verdes vein is correct. Our drilling has shown that the large high-grade mineralized shoot identified on the vein terminates abruptly against this northeast structure, indicating that mineralization was cut by it and offset to deeper levels. The deep drilling to be conducted from our Strategic Partner Vizsla Silver's ground is designed in part to explore this concept and will target the Palos Verdes vein at depth. We deeply appreciate our Partner's willingness to allow the drilling from their ground."

"In addition to giving strong indications of where the eastern end of the Palos Verdes vein lies, demonstrating that the NW-trending structure offsets one vein stage, while hosting mineralization and alteration itself is potentially important confirmation of multiple mineralization stages in this part of the district," said Dr. Peter Megaw, Prismo Exploration Advisor. "Finding blind veins is perhaps even more exciting as that mirror several of the discoveries Vizsla Silver, our Joint Exploration Committee partners have made in the western part of the district."

The alteration study was carried out using a field portable Terraspec Halo near-infrared spectrometer to identify mica and clay minerals that make up the wall rock alteration assemblage surrounding the mineralized veins in surface exposures and drill core. Clay minerals typically found at high structural levels in low sulfidation vein systems provide evidence that the northeastern portion of the property has been down-dropped, probably along the northerly trending cross structure previously identified.