OF THE SILVER QUEEN MINE AREA , OWEN LAKE , CENTRAL BRITISH COLUMBIA ( 93 L ) By

Geological Fieldwork 1989, Paper 1990-1 Columbia (Figure 2-8-1). The geology of the 20 squa~f : kilometre area surrounding the deposit'has been mapped, antl results suggest that the slratifiedrocks hosting this epithemxll gold-silver-zinc-lead-copper vein deposit (the Late Crt taceous Tip Top Hill volcanics; Church, 1971) may tf: correlative with rocks h(xting the Equity Silver depos,it, antl are lithologically similar to the Kasalka Group of IateEarly to early-Late Cretaceous, age. The geological mapping is pa? of a more extensive project dealing with the geol,ozy and origin of polymetallic vzin deposits in the Owen Lake areil