White Metal Resources Corp. is revaluating the prospectivity of its 100% owned Seagull Lake Pt-Pd Property (the "Property'), located about 50 km south of Impala Canada's Lac des Iles Mine (previously North American Palladium) in northwestern Ontario. The 6,168 hectare property, approximately one hour drive north of the port city of Thunder Bay, is also about 28 km north of the new copper, nickel, platinum, and palladium discoveries of Rio Tinto and Panoramic Resources (previously Magma Metals). The Seagull Lake Intrusion ("SLI") is described as being a 10 km diameter, circular intrusive composed of ultramafic rocks with a high olivine content that has been derived from a deep mantle source. Layering and multiple phases of intrusion have been recognized which creates a favourable setting for Noril'sk Type sulphide accumulation. The SLI is located in the Nipigon Plate, which is interpreted to represent the failed third arm of a Proterozoic-aged, mid-continent rift system, the bulk of which lies beneath Lake Superior to the south. Three styles of PGE mineralization have been identified in the SLI: near surface, PGE-rich detrital "black sands"; magnetite associated, PGE-rich layers or "reef-type"; and, sulphide associated, basal Cu-Ni-PGE mineralization, interpreted as "Noril'sk-type". Although the detrital and reef-type mineralization was the first style known in the SLI, the discovery of Noril'sk- type Cu-Ni-PGE sulphide mineralization became the focus for subsequent exploration programs, which reported from diamond drilling 3.6 g/t Pt+Pd, 0.34% Cu and 0.21% Ni over 2.1 metres and 1.04 g/t Pt+Pd, 0.14% Cu and 0.16% Ni over 16.0 metres (from Pettigrew, 2002). The possibility for the discovery of other styles of sulphide mineralization remains including Contact-type deposits (e.g., Lac Des Iles Mine and River Valley deposits, Ontario) and structurally hosted high-grade concentrations along regional fault systems.