Kuya Silver Corporation reported a drill core intersection of native silver mineralization at its wholly-owned Campbell-Crawford area of the Silver Kings Project, located in the Cobalt, Ontario mining camp. This new discovery is located within a 1 km radius of five major mines, with a total historic production of 48.2 million ounces of silver (Crown Reserve, Deerhorn, Drummond, King Edward, Nova Scotia). The area is less than 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. (Benner 1982).

Native silver was intersected in the second drill hole at the Campbell-Crawford area and drilling is ongoing along trend. Mineralization in this vein appears to be primarily native silver, but minor cobalt mineralization is also recognized. Silver stringers occur above and below the silver vein, significantly increasing the potential width of mineralization.

Drill intersection was made 170 m below the nearest underground workings (1910s exploratory tunnelling) and 230 m below surface. The Campbell-Crawford area, despite being surrounded by historic mines and mineral occurrences, has remained virtually untested since exploration occurred in the early twentieth century and the area has never been mined. Assay results are pending.

Campbell-Crawford target area: Cobalt-bearing veins (which are known to occur with, or grade into, silver-bearing veins), were discovered on surface in 1906. Between 1906 and 1930, two small shafts were sunk and 175 m of exploratory tunneling (adit and associated drifting) was done on a single level, with the maximum depth of workings is 35 m below surface. All shafts and adit workings are restricted to rocks of the Nipissing Diabase sill.

Two diamond drill holes, totaling 560 m, were drilled in 1930. The historic description of the property is compiled after Sergiades (1968). Mineralization in the Cobalt mining camp is spatially associated with the margins of a 300 m thick, subhorizontal and gently-folded sheet of Nipissing Diabase.

The historic Campbell-Crawford workings are located near the center of this sheet; in contrast, this mineralized veining was intersected approximately 10 m below the contact.