The ILE showing is situated on the north bank of Smith Creek, 11.5 kilometres west of Hedley.
The showing is hosted in a sequence of andesite ash and lapilli tuff of the Upper Triassic Whistle Creek Formation (Nicola Group), several hundred metres south of granodiorite and quartz monzonite of the Early Jurassic Bromley batholith.
Two zones of mineralization have been identified. An area of fine disseminated pyrrhotite in altered volcanics contains silver values of between 3 and 18 grams per tonne (Property File - Cukor, 1972, page 17). A second zone of strongly pyritized volcanics contains some chalcopyrite and sphalerite.