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The Giroux Project is located within the Walker Lane shear zone and consists of sediments with numerous felsic intrusives. Silicified fault zones and trends have been explored and mined via shafts, pits, and adits. At least one shaft is reported to have a depth of over 700 feet. Of particular interest is the presence of an overthrust nickel bearing serpentinite formation. In addition to nickel mineralization, the property contains gold, copper, silver, as well as lead-zinc and barite mineralization.