The area is underlain by the Upper Triassic Vancouver Group consisting of Karmutsen Formation volcanics rocks which are overlain on the northeast by a northwest trending belt of Quatsino Formation limestone. The latter is known historically as the "lime-belt". These are in fault and/or intrusive contact to the northeast with intrusive rocks of the Jurassic to Tertiary Coast Plutonic Complex.
A body of pyrrhotite with quartz about 1 metre wide has been exposed at the mouth of a tunnel that has been driven 33 metres south- west in limestone. The Condor occurrence is situated to the north- west of the Anaconda (092K 111), which exhibits similar geology. The latter occurs at the contact of andesitic rock and limestone. The intrusive contact occurs within a few hundred metres to the northeast.
A sample of pyrrhotite and quartz assayed 0.69 grams per tonne gold, 6.86 grams per tonne silver and 0.9 per cent copper (Minister of Mines Annual Report 1913, page 285).