The Frog Creek occurrence is located in the northern head waters of Olympic Creek, a tributary of the Kennedy River.

The area is underlain by Karmutsen Formation volcanics of the Upper Triassic Vancouver Group, which have been intruded by the Early to Middle Jurassic Island Intrusions consisting of granodiorite to quartz diorite. The Karmutsen rocks consist of andesitic to basaltic flows, tuffs and volcaniclastics. Northwest trending fault shear zones of Tertiary age cut the rocks.

Locally, quartz veins host pyrite and chalcopyrite mineralization.

In 1986, K. Gourley staked the Blaster claim and completed a prospecting program and a geochemical silt survey the following year. From 1987 to 1988, Nationwide Gold Mines and Golden Spinnaker Minerals optioned the property and completed programs of trenching, VLF-EM surveys and diamond drilling. In 1988, bulk sampling and fourteen diamond drillholes, totalling 819 metres, were completed on the Elite 1 vein and the nearby Rachel vein. In 1991, Kancana Ventures optioned the property. From 1993 to 1995, the property was returned to and later prospected by K. Gourley. In 1995, a 0.20 metre chip sample returned values of 2.6 grams per tonne gold and 2.7 grams per tonne silver (JK-167; Assessment Report 25493).