A small zone of sparse copper-molybdenum mineralization occurs 3 kilometres northeast of the head of Pender Harbour, 3 kilometres southeast of Sakinaw Lake on Sechelt Peninsula.

The Jon showing is hosted in granite and granodiorite of Upper Jurassic age within the southwestern margin of the Jurassic to Tertiary Coast Plutonic Complex.

A fault zone striking 150 degrees for at least 140 metres and dipping 60 degrees northeast is mineralized with disseminated pyrite and pyrrhotite with minor to trace amounts of chalcopyrite and molybdenite. The zone varies up to 32 metres in width. The granite and granodiorite are silicified and weakly clay altered within this fault zone. Two 1.5 metre long chip samples assayed 0.1 per cent copper, trace molybdenum, and 0.01 per cent copper, 0.01 per cent molybdenum respectively (R.N. Beewar, 1972).