Kuya Silver Corporation announced assay results from the newly discovered, silver- bearing Angus Vein. The silver results in the Angus Vein were intersected in the second of two drill holes in the Campbell-Crawford area, which was historically explored but never mined. Highlights of New Discovery: Kuya Silver expedited the assaying of 3.80 m of visually identified silver mineralization in hole 23-SK-08: Best assay intercept to date of 74,418 g/t (2,393 oz/t) silver over 0.30 m (237.50 m to 237.80); Composite interval of 16,838 g/t silver, 0.08% cobalt over 3.04 m (235.20 m to 238.24); Logging indicates additional silver/cobalt mineralization in this drill hole.

Seven drill holes (2,334 m) at Campbell-Crawford area intersected up to six silver/cobalt mineralized veins per drill hole (visual and/or pXRF analysis); The Company intersected multiple silver/cobalt mineralized veins per drill hole, at a range of depths and with different orientations, suggesting that this is more likely a mineralized vein cluster and not an isolated vein; Campbell-Crawford discovery is located approximately 1 km north of the North Drummond area and 750 m southeast of a 1,300 oz/t silver intercept from 1981 underground drilling by Silver Century Explorations Ltd. The Angus Vein Discovery: The Angus Vein is one of two mineralized veins known in the historic Campbell-Crawford adit, and the vein may be exposed on surface as the Campbell-Crawford West vein. The vein trends 060°-240° and dips SE at 80° (060°/80°). The vein was intersected in hole 23-SK-07 at 108.5 m, confirming the southerly dip.

In all three of these cases, the vein occurs within the sheet-like Nipissing Diabase sill and mineralization is relatively low-grade. Immediately below the lower diabase contact, the vein orientation appears to change sharply. The 060°-240° trend seems to remain constant but the dip direction reverses to NW dipping at ~75°.

Hole 23-SK-08, which intersected the bonanza-grade mineralization, pierced the vein in this zone. However, this change in vein orientation is subparallel to subsequent drillholes 23-SK-09, -10, -11 and -12, which were drilled to the north. Drill hole 23-SK-13 was drilled southerly and a 1 m zone of veined to fracture-filling native silver was intersected, 11 m laterally and 18 m deeper than the initial silver intersection in hole 23-SK-08.

Three major points can be inferred from the drilling and this reversal of dip direction of the vein: The flexing of the vein occurs along the lower diabase contact. The intersection of the vein with the diabase contact trends 060°-240° and is calculated to plunge shallowly (~10° SW); Silver content increases significantly in this flexed zone; Silver content in this zone seems to persist for at least 30 m below the diabase contact.