The Victory showing is a silicified zone, about 2.7 metres wide, that contains minor disseminated sphalerite and pyrite, and which is hosted in garnetiferous gneiss of the Proterozoic and/or Paleozoic Shuswap assemblage. The zone strikes about 325 degrees across Black Point, a promontory about 2 kilometres in length that juts into Mara Lake on the west side. The zone is characterized by considerable development of pegmatite.

A tunnel had been driven along this zone for 8.5 metres from a point at the south end of the promontory, at about 3 metres above the level of the lake. It followed a well-defined hangingwall with a northerly strike and dip to the west. At a distance of a metre from the portal, sphalerite was reported to be distributed in small quantities throughout the whole width of the zone. A shipment of about 37 tonnes of this material was made to the Trail smelter. Returns from this shipment were not available, but it is understood that they did not come up to the owner's expectations (Minister of Mines Annual Report 1927, page C198).

A sample taken across 2.4 metres of the silicified zone, at the face of the tunnel, assayed trace gold, 6.8 grams per tonne silver and nil zinc (Minister of Mines Annual Report 1927, page C198).