The San Diego Bay prospect is typified by an extensive 40 square kilometre area of gossan, strong hydrothermal alteration and intrusive rocks, consistent with porphyry systems such as the adjacent Pyramid deposit. All porphyry alteration facies have been observed, including zones of potassic, advanced argillic, phyllic and pyrite zones; previous landsat imagery has identified widespread zones of high-temperature clay alteration. Strongly anomalous precious and base metal values were collected by previous operators; an important consideration for exploration is that the adjacent Pyramid deposit hosts a leach cap of 10 to 100 meters in thickness, and underlain by a supergene enrichment blanket. Cobbles of copper oxide mineralization have been identified by local, Aleut shareholders on beaches adjacent to the alteration zone. Interpretations suggest that San Diego Bay may represent overlapping hydrothermal systems, including potential lithocaps. San Diego Bay represents a Tier-1 sized porphyry target with an excellent location.