The W.P.L. occurrence is situated near a marble-granitic gneiss contact where massive pyrrhotite-chalcopyrite-arsenopyrite is hosted in a skarn zone. The massive mineralization is exposed on fault planes, while disseminated sulphides occur in schists and green garnetiferous zones; small veins cut these zones. Hostrocks belong to the Precambrian-Paleozoic(?) Shuswap Metamorphic Complex.

Rock samples taken from the mineralized zones analysed as high as 0.4 per cent copper, 1.85 grams per tonne gold and 5.7 grams per tonne silver (Assessment Report 14805).