LOCATED WITHIN THE PROLIFIC COBALT MINING CAMP
The Project is located near the town of Cobalt in northeast Ontario, Canada. The Project hosts the historic Thomas Edison, Shakt-Davis and Cobalt-Kittson mines, as well as numerous historic workings, the deepest extending down to 628 feet, and over 2,500 feet of lateral workings. Cobalt mineralization occurs in Proterozoic-aged quartz-carbonate veins hosted in brittle shears in Nipissing diabase. This style of mineralization is similar to that of the famous Cobalt Silver Camp Located ~15 km east of the Property, which produced 420 million ounces of silver with cobalt as a significant by-product. Veins hosting the mineralization at the Kittson-Cobalt Project differ from the typical Cobalt Silver Camp veins in that they are lower in silver but richer in cobalt, and are associated with significant gold. Historic reports from the Shakt-Davis mine indicate values of 1.5% Co over 1.37 metres and select grab samples returning up to 4% Co and 93.3 g/t Au. Locally significant nickel, copper and to a lesser extend lead, zinc and bismuth also occur within the quartz-carbonate veins.
THREE PAST PRODUCING MINES ON THE PROPERTY
The Shakt Davies mine saw intermittent development from 1906 – 1964, with the bulk of the underground working completed between 1924 – 1926. No production records remain, however historic reports indicate values of 1.5% cobalt over 1.37 meters and select grab samples returning up to 4% cobalt and 93.3 g/t gold. More recent sampling (1987) of the mine waste pile by the Ontario Geological Survey personnel returned 0.25% cobalt, 0.75 % nickel, 0.05% copper and 3.4 g/t gold.