TV Tower is underlain by hydrothermally-altered intermediate volcanic rocks and intrusive bodies.  The highest elevations of the property are host to residual quartz ledges and ribs with oxidized high sulphidation epithermal (“HSE”) gold mineralization and/or unoxidized gold-silver-copper mineralization. Gold-copper porphyry systems lie immediately under or adjacent to the oxidized gold zones, often with a zone of supergene copper mineralization at the interface. Low sulphidation epithermal (“LSE”) gold-silver veins often flank the HSE and porphyry systems. The volcanic rocks overlie a basement of metamorphic rocks that are exposed in the deepest valleys and in the western portion of the project.