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The volcanogenic massive sulphide Eskay Creek property, 102 km southeast includes several deposits of polymetallic sulphide mineralization as both exhalative massive sulphides and discordant veins, transitional between sub aerial hot spring Au-Ag deposits and deeper water exhalites and the alkalic porphyry copper-gold deposits within the Galore Creek area are hosted primarily by highly altered potassium-enriched volcanic rocks and pipe-like breccias adjacent to dikes and stocks (intrusives) which have intruded coeval with the Stuhini Group rocks.
Assay results confirm the presence of significant gold mineralization associated with south-dipping, en echelon, discordant veins within a mylonitic phyllite unit, with vein widths of up to 4m.