The property is underlain by a sequence of Cambrian-Ordovician carbonates including the Jubilee, McKay and Beverfoot Formations. A northerly trending, tightly folded, overturned anticline is exposed in steep cliffs on the east side of the property. A north trending fault transects the property. Irregular plugs and dykes of feldspar porphyry intrude the sedimentary sequence west of the fault. Quartz veining with moderate disseminated pyrite occurs.