Investor Presentaiton

OURCES ING Drone-based Magnetics IRV:CNX At Omui mine site, a plot of magnetic analytic signal shows a complex network of low magnetic intensity (blue) where hydrothermal alteration has obliterated traces of magnetite in volcanic rocks, a possible indication of vein systems at depth. Note, the northwest-trending zone of low magnetic intensity extending from the Nanko prospect through the historic Honpi mine site. This is parallel to a prominent gravity gradient highlighting a graben-bounding fault underlying this area (lower right). R Honpi Nanko ine 1 km 20 20

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