Company") is pleased to announce that four holes have now been completed at its Rickard Gold Project (the "Property"). The holes all intersected multiple (1 to 3 metre) wide multi-staged shear-zone hosted quartz-carbonate veins. The veins are observed to contain locally abundant massive to semi-massive pyrite, blebby chalcopyrite, and unidentified fine-grained smoky sulphide minerals which may be the source of gold historically identified in the area. Strong to pervasive albite-sericite-silica-pyrite alteration forms halos around the main vein sets, see figures 1 and 2 below or on the Company's website under the Rickard Gold Project page. Highlights: Initial holes cut multiple 1- to 3-metre-wide greenstone hosted quartz-carbonate veins.