Kuya Silver Corporation announced additional assay results from the Campbell-Crawford area. These results include remaining drill hole assay results from hole 23-SK-08, as well as drill holes 23-SK-11, -12 and -13. To date, the Company has reported a total of 1,287 m in four drill holes of a total 2,334m in seven drill holes at Campbell-Crawford.

Assays are pending for drill holes 23-SK-01 to -06 (North Drummond and Silver Leaf targets, Kerr Lake area) and 23-SK-07, -09 and -10 (Campbell-Crawford area). Angus Vein High-Grade Silver Mineralization Expanded: The Angus Vein has now been intersected in three oriented drill holes with drastically different silver/cobalt grades. The mineralized grades can be linked to the vertical distance from the Nipissing Diabase rock contact: 15,372 g/t silver, 0.08% cobalt over 3.34 m approximately 10 m below the diabase contact in Archean volcano-sedimentary rocks (23-SK-08 ­ 237 m), 2,424 g/t silver, 0.03% cobalt over 2.49 m approximately 30 m below the diabase contact in Archean volcano-sedimentary rocks (23-SK-13 ­ 258 m), and Low grade cobalt and arsenic identified by pXRF over 0.03 m (3 cm) carbonate vein approximately 115 m above the Nipissing Diabase contact and within the diabase (23-SK-07 ­ 108 m).

These three intersections match well with the mining camp model: mineralized vein structures are traditionally the most prolific close to the Nipissing Diabase contacts. Historically, the Archean volcano-sedimentary rocks are generally more prolific host rocks than the Nipissing Diabase, but extremely high silver grades are sometimes known just into the diabase host (for example Keeley-Frontier, Silver Cliff mines; Sergiades 1968) and this zone is untested at Campbell-Crawford. The assay results also indicate metal zonation with high-grade silver zones transitioning into mixed silver-cobalt-nickel zones at depth or on vein margins.

Very importantly, the NE-trending Angus Vein orientation and metal zonation suggests that these zones track along the lower diabase contact and may continue along trend; other NE-trending veins, indicated in these drill results and especially veins drilled within the Nipissing Diabase, have the same mineralizing potential as the Angus Vein near the lower diabase contact, with associated significant to high grades of silver, cobalt and nickel. Ongoing Work Plans: A surficial bedrock stripping program is commencing shortly in the Campbell-Crawford area to identify and trace surficial mineralized veins. Veins will be uncovered both along and across trend, testing for vein density, orientation and continuity and projected to depth, in preparation for a 2023 phase 2 drill campaign.