The Wide West skarn showing is located 2.5 kilometers south of Eldorado mountain, near the head of Taylor Creek. The showing is within Mississippian to Jurassic Bridge River Complex (Group) crystalline limestone, interbedded with slate and greenstone and adjacent to diorite of the nearby Paleocene Eldorado pluton. Mineralization consists of pyrrhotite and minor chalcopyrite as solid masses, making up 60 per cent of the rock. The limestone body is six metres wide and is partly to wholly replaced with sulphides. A sample taken in 1913 assayed about 7 grams per tonne gold (Minister of Mines Annual Report 1913, page 268).