The Smith Mine complex, started in 1999, consists of several mineralized areas.


Gold mineralization in the main Smith, Mahala and West Dash deposits is associated with the northeast trending Coulee Fault and west-northwest trending faults and dikes. In Zone 1, high-grade gold mineralization is hosted in the upper and middle portions of the Hansen Creek III unit. Mineralization in Zones 2 and 3 is directly associated with west-northwest trending dikes.

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