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The Goldstone discovery is hosted by a Breccia within the Early to Middle Jurassic Ladner Group. The Ladner Group sits unconformably to the east of the Early Jurassic Hozameen Group, separated by the Hozameen fault. The Ladner Group is distinguished from the other sediments by its rusty appearance on weathered surfaces due to its relatively high pyrite content. The tourmaline breccia pipes, which host the historic copper/silver/gold mineralization at the Giant Copper property, are all confined to the Ladner Group. Significant assay intervals reported represent apparent widths. Insufficient geological information is available to confirm the geological model and true width of significant assay intervals. ....

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