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The Girard Lake zone is five km northwest of the Ball No. 2 zone. The Girard Lake zone consists of iron formation and magnetite and was reported by Bergeron in 1952 as, "A preliminary sampling showed an iron content varying between 60% and 68%." The zone was outlined by pits and trenches in excess of 400 feet and with widths varying from 12 to 40 feet. Kadillac
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