The Cor 14 showing is located 4.5 kilometres east of Alberni Inlet, 16 kilometres south of Port Alberni.

The area is underlain by Upper Triassic Karmutsen Formation (Vancouver Group) volcanics which are intruded by biotite- granodiorite of the Early to Middle Jurassic Island Plutonic Suite. The volcanics consist of greenstones, andesites and basalts. Quartz- carbonate veins mineralized with minor pyrite and chalcopyrite, cut both rock types (volcanics and intrusives) but are more common in the andesite.

A quartz-carbonate vein, up to 50 centimetres wide, occurs in brecciated greenstone. Pyrite, chalcopyrite and minor arsenopyrite are disseminated in the vein. The best assays from vein samples taken from this area were 0.9 grams per tonne gold and 0.09 per cent copper (Assessment Report 6676).

The vein has been exposed by trenching and a small adit, which are likely connected to work on the Star of the West showing (092F 215).