The Bachelor showing is located 8 kilometres southwest of Vernon, east of Okanagan Lake.
In this area, west of the Okanagan Valley fault zone, volcanic and sedimentary rocks of the Devonian to Triassic Harper Ranch Group are unconformably overlain by Upper Triassic to Lower Jurassic Nicola Group sedimentary and volcanic rocks. These units are intruded by Middle Jurassic granitic rocks informally named the Terrace Creek batholith. Granitic Coryell rocks of Eocene age intrude these rocks and patches of Eocene Penticton Group volcanic rocks overlie the older rocks.
A quartz vein in Middle Jurassic quartz diorite hosts gold and copper mineralization. The 1.1 to 2.4-metre thick vein carries pyrite, chalcopyrite and native gold. Selected surface samples assayed up to 800 grams per tonne gold ($480) while more representative samples taken at depth assayed 35 grams per tonne ($22) (Minister of Mines Annual Report 1896).
By 1899, exploration included the sinking of 2 shafts, totalling 12 metres, and 17 metres of tunnels.