more reason for hope

High grade gold-quartz glacial boulders, recovered down ice from Bell Lake south of Kerrs property, have been assayed for gold / silver and analysed for multi-element ICP. Results show background levels of arsenic, copper, chrome and boron with enrichment of lead, consistent with typical analyses returned from the green carbonate breccia mineralization encountered in the Kerrs Gold system. High grade visible gold in this boulder sample assayed 91.5.g/t gold and 23g/t silver. The gold/silver ratio is also similar to the higher grades observed in K-06-01. There is compelling evidence that the “East Ford Lake Gold boulders” were glacially eroded from subcroppings of the “Kerrs Gold System”, possibly below and on strike of Bell Lake.