The property is situated in Jurassic volcanics on the margin of a graben developed along the NW-trending Gastre fault system. To-date, there has been very limited prospecting on the property. Outcrop is limited, however, numerous barite veins and epithermal chalcedonic quartz veins have been found. Limited, reconnaissance, ground magnetic and induced polarization surveys (400 meter spaced lines) have been completed. Prominent NW-trending and N-trending magnetic structures are associated with the quartz and barite veining, and there are local induced polarization and resistivity responses.