Reyna Gold Corp. announced more sample results from the ongoing district-scale exploration at its 24,215 hectare La Gloria Property in Sonora, Mexico. Results are returning high grades of precious, base, and critical metals, and substantially increasing the size of the mineralization footprints at Las Carmelitas, La Republicana and Western targets.

Main Area 'Potential Enrichment Zone' at Las Carmelitas expanded to 1km length by 250m average width Major Conglomerate and Agglomerate Zone discovered at Las Carmelitas 2.5km length by 1.7km average width Disseminated mineralization identified within Conglomerate, Agglomerate, and Sandstone host rocks at Las Carmelitas New La Republicana North Zone discovered, expanding known mineralization footprint at La Republicana to 2.67 sq km (267 hectares). Western target mineralization footprint expanded to 1.5km length by 450m average width, with high-grades of Tellurium found throughout the Western mineral system At the Las Carmelitas target, multiple high-grade samples up to 9.47% Copper (Cu), 272 g/t Silver (Ag), and 2.44% Antimony (Sb), and high grades of Mercury (Hg), Barium (Ba), and Strontium (Sr) have been received, adding to the thesis they identify a supergene enrichment zone at the top of a mineral system at Las Carmelitas. In total, 43 samples have been taken in the main area of Las Carmelitas with average grades of 2.25% Copper, 89.14 g/t Silver, 0.21 g/t gold (Au), and 0.48% Antimony.

The high-grade mineralization occurs within an extremely large silica alternation (4km in length, average 1km in width), aligned with a regional fault. At Las Carmelitas, the mineralization is hosted within conglomerate, agglomerate, and medium-grained sandstone host rocks. The geological team has identified disseminated mineralization in all three of the host rocks.

The IP survey was designed to test the size and depth of the conglomerate/agglomerate and the silica alternation. The geological team has identified a conglomerate/agglomerate footprint at surface of approximately 2.5km by 1.7km and believes it continues undercover in multiple directions, particularly along the northwest-southeast regional Main Zone Fault. The discovery of multiple Antimony samples of more than 1% up to 2.44% is a very positive addition to the potential of Las Carmelitas.

Antimony is on the United States Critical Mineral List and is a critical mineral for producing semiconductors, electric storage batteries, fire retardantsand bullets. Reyna Gold's geological team is currently working on a trenching program and an IP geophysical survey in the Las Carmelitas Target to more clearly determine the size of the potential supergene enrichment zone and identify the potential of the system at depth. At the Western target, the mapping and sampling work has focused on initially developing a core area.

The geological team has discovered new parallel structures and the continuation of those previously reported within the northeast-southwest trending system. In addition, secondary trending structures northwest-southeast, east-west, and north-south have been identified. The footprint of the core target area now has a length of 1,500 m and a 450 m average width; the system is open, both longitudinally and transversally.

The geological team is excited about the continuous nature of the gold mineralization within the veins at surface and the presence of Tellurium widely throughout the system. The gold values are correlated with an abundance of Tellurium in the system and with sub-anomalies of silver (guide grades). These results, along with the presence of diorite host rocks, are all positive factors that indicate great potential for a robust mineral system at depth.

Tellurium is on the United States Critical Minerals List and is a critical metal used in manufacturing solar panels and thermoelectric devices. At the La Republicana Target, mapping and sampling continued in the core northwest-southeast trend zone, where previously reported drill-hole 30 produced a 59 m of 1.45 g/t gold intercept. The geological team has now extended this zone with discontinuous veins and veinlets to 2.8 km in length with an average width of 625 m. La Republicana North has been discovered to the north of the main target area with the same host rocks, meta-rhyolite and meta-andesite (rocks favorable for mineralization).

La Republicana North is separated from the main area by faults trending northeast-southwest, which probably separated and rotated the structures towards the northeast, and in turn, a graben was generated. The main structural system presents a northwest-southeast trend with east-west variations. At least 3 hydrothermal events have occurred in the zone: 1) veins and veinlets of white quartz (occasionally greyish) with the presence of galena, chalcopyrite, and covellite, 2) veins and veinlets of quartz-tourmaline (cutting first event structures) coarse pyrite is observed, traces of chalcopyrite and secondary minerals such as hematite, jarosite, malachite and chrysocolla, 3) filling of calcite and iron carbonates within second event structures.

In La Republicana North, a zone of parallel and semi-parallel veins and veinlets has been identified with a length of 570 m and an average width of 480 m, with grades of up to 18.95 g/t Gold, 199 g/t Ag Silver, 1.03% Copper and 5.33% Lead. The three zones of La Republicana now total 2.675 km2, with grades of up to 103.50 g/t Gold, 283.00 g/t Silver, 2.4% Copper, 5.33% Lead, and 0.12% Zinc.