The Mount Shaw Project offers massive exploration upside in a proven, world-class mineralized corridor. Situated along the same structural trend as the giant Mount Morgan (8Moz) and Cracow (3Moz) deposits, Mount Shaw is defined by a large surface anomaly yielding up to 18% Copper. Recent geochemistry has confirmed the presence of a highly active system, with standout samples returning 5,000 ppm Cu alongside propylitic alteration—a classic indicator of the outer halo of a major porphyry system. With strong geochemical vectors pointing directly toward the core of the mineralization, Mount Shaw is primed for a significant, large-scale discovery.