The WW showing is located beside the logging road north of Coleman Creek, 5.6 kilometres east of Alberni Inlet. The exact location is uncertain. The showing could possibly be part of the Copper King showing (092C 054).

The area is underlain by Lower Jurassic Bonanza Group volcanics and limestones of the Upper Triassic Quatsino Formation, Vancouver Group. These are intruded by granitic rocks of the Early to Middle Jurassic Island Plutonic Suite.

Mineralization consists of chalcopyrite, pyrite and pyrrhotite hosted in a matrix of actinolite in a fault 0.6 metres wide. The fault has been traced for 30 metres to the south and occurs at a contact between andesite (hanging wall) and limestone (footwall). The showing plots in rocks mapped as Island Plutonic Suite (Geological Survey of Canada 821).