The AT showing is located 29 kilometres north-northwest of Kelowna, north and west of Dun Waters Creek.
In this area, Middle Jurassic quartz monzonite of the informally named Terrace Creek batholith intrudes argillaceous sediments of the Upper Triassic to Lower Jurassic Nicola Group. The stock is intruded by diorite plugs and dikes which are cut by quartz monzonite and aplite dikes. The intrusive rocks are cut by Tertiary basalt dikes related to volcanic rocks which overlie the older rocks.
Chloritized and sericitized, moderately fractured quartz monzonite porphyry hosts molybdenum and a trace of copper mineralization. Quartz veinlets, usually 1 to 10 centimetres thick, carry disseminated molybdenite, pyrite and traces of chalcopyrite. Pyrite and molybdenite occur on fracture planes. Alteration is associated with the quartz stockwork and the fractures.
About 1 kilometre to the northwest, sericite and epidote-altered quartz monzonite porphyry hosts quartz veinlets carrying a trace of disseminated molybdenite.
In 1966-67, Noranda Exploration Co. Ltd. carried out soil geochemistry and trenching programs. In 1972, Canadian Johns- Manville Co. Ltd. carried out a soil geochemistry survey. In 1979-80, Cominco Ltd. carried out geological mapping, induced polarization and magnetometer surveys.