Exploration Pipeline

Dike Swarm is an overburden-covered, undrilled area within a broad IP anomaly that extends southeast from the Getty North deposit. Historical drilling along the flank of this 1 km-long target shows ubiquitous propylitic and weak sericitic alteration, commonly associated with strongly anomalous copper values in the hundreds of ppm (parts per million) range.

A large zone of anomalous copper in pine bark samples underlain by post-mineral cover. The anomaly is considered relevant because similar bark biogeochemical anomalies are associated with the Getty North and Getty South deposits, and the target is considered prospective based on projected mineralization trends and structural features.

A large zone of anomalous copper in pine bark samples underlain by post-mineral cover. The anomaly is considered relevant because similar bark biogeochemical anomalies are associated with the Getty North and Getty South deposits, and the target is considered prospective based on projected mineralization trends and structural features.

Woods Creek is an overburden-covered IP (induced polarization) chargeability anomaly and magnetic low extending for more than 2 km. Widely spaced historical drill holes fringing this anomaly encountered abundant disseminated pyrite, potentially part of the alteration halo of a porphyry deposit.

North Glossie is an overburden-covered area with a coincident IP anomaly and magnetic low. Subtle anomalous copper in soil located down-ice, together with copper oxides mapped in nearby bedrock, contribute to the prospectivity of the target. There is no historical drilling in the immediate target area.