The Victory showing is located on the slopes east of Williams Creek, 2 kilometres south-southeast of Barkerville.

The showing lies within the Barkerville Terrane of the Omineca Belt. The Barkerville Terrane is in thrust contact with Triassic Quesnel Terrane rocks to the west and Hadrynian to Lower Paleozoic Cariboo Terrane rocks to the east. The Barkerville Terrane in this region is underlain by the dominantly metasedimentary rocks of the Hadrynian to Lower Paleozoic Snowshoe Group. In this area the Snowshoe Group comprises limestone, phyllite and quartzite. These rocks have been regionally metamorphosed to greenschist facies.

The showing comprises several quartz veins cutting phyllites and quartzites of the Upper Proterozoic-Paleozoic Snowshoe Group. The veins were worked on the former Victory claim in the early 1900s. Two of these veins, both striking northeast and ranging from 15 to 20, and 25 to 38 centimetres wide respectively, are mineralized with arsenopyrite, pyrite and galena (Geological Survey of Canada Memoir 149, page 196, workings 1 and 2). The narrower of these two veins contains stringers up to 5 centimetres wide of massive arsenopyrite with pyrite and galena. In 1926, a sample of this heavily mineralized material yielded 338.74 grams per tonne gold and 75.43 grams per tonne silver, and another sample analyzed 464.23 grams per tonne gold and 115.54 grams per tonne silver (Geological Survey of Canada Memoir 149, page 205).