The showing is situated on the Sechelt Peninsula, 1.9 kilometres north-northwest of the north end of Carlson Lake, 9.5 kilometres north-northeast of Halfmoon Bay.

The MC showing is hosted in a roof pendant of carbonates, amphibolite and related metavolcanics of the Upper Triassic Karmutsen Formation(?) (Vancouver Group), engulfed in diorite and quartz diorite of Upper Jurassic age, within the southwestern margin of the Jurassic to Tertiary Coast Plutonic Complex. The roof pendant trends north-northwest along the east side of the Sechelt Peninsula for 12 kilometres.

The showing consists of a shear zone striking for 15 metres in limestone and varying up to 3 metres in width and is mineralized with chalcopyrite and minor pyrite and magnetite. A grab sample assayed 0.96 per cent copper, 24.0 grams per tonne silver and a trace of gold (Assessment Report 4803, page 2).