The property is underlain by a thick sequence of siliceous metasedimentary rocks consisting predominantly of quartz-mica schist, grey quartzite and micaceous quartzite with minor inter- beds of carbonate-graphite phyllite.

Mineralization occurs as sparse pockets of massive pyrite, pyrrhotite and chalcopyrite within quartz blebs and as finely disseminated stratabound pyrrhotite and chalcopyrite within quartzites.