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OUTCROP SILVER MAKES A DISCOVERY AT LOS MANGOS, STEPPING OUT FOUR KILOMETRES SOUTH

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VANCOUVER, BC, March 12, 2025 /CNW/ - Outcrop Silver & Gold Corporation (TSXV: OCG) (OTCQX: OCGSF) (DE: MRG) ("Outcrop Silver") is pleased to announce the discovery of high-grade mineralization through drilling at its 100% owned Santa Ana high-grade silver project in Colombia, after following the company's strategy of making large step-outs to the south, along the 17 kilometre fully permitted vein system corridor. This discovery reinforces the path for scalability and high-grade potential of the Santa Ana project as the drilling continues at this highly prospective target.

Drilling Highlights

  • Hole DH444 intercepted 1.92 metres grading 586 grams per tonne of silver equivalent, making a high-grade discovery at the Mangos SE vein (Table 1).

  • Hole DH442 intercepted 2.36 metres grading 404 grams per tonne of silver equivalent at Los Mangos vein (Table 1).

  • The discovery at Los Mangos confirms the success of Outcrop Silver's exploration strategy by making large step-outs along the 17-kilometre fully permitted mineralized corridor.  Los Mangos is 8 kilometres south of the resource and 4 kilometres south of the recent La Ye discovery.

"The results from Los Mangos are a major breakthrough for the Santa Ana project, confirming high-grade silver-gold mineralization in yet another significant step-out. Hitting strong grades more than 8 kilometers south of the closest resource vein proves the great potential of this system and validates our exploration strategy," comments Guillermo Hernandez, Vice President of Exploration. "With intercepts like 2.36 meters at 404 g/t AgEq, we are seeing wider mineralized veins that reinforce the strength of the vein system. This discovery not only extends our high-grade footprint but also unlocks new opportunities for further expansion in the underexplored central and southern portions of Santa Ana."

The Los Mangos is a high-grade silver-gold vein system located in the central portion of the Santa Ana project (Figure 1). The vein has a confirmed strike length exceeding 350 meters, highlighting its potential for further expansion. It trends 40° and 60° dipping 60° to 80° to the southeast, with localized northwest-dipping structures (Figure 1 and Figure 2). The main mineralized zone ranges up to 1.20 meters in width, with strong argillic and sericitic alteration in the surrounding wall rock, particularly evident  in the historic El 20 underground workings (Figure 3). The vein is hosted within green schists and granodioritic to dioritic dikes, indicating that mineralization is strongly influenced by both structural and lithological controls.