The region is underlain by (?)Hadrynian to Paleozoic Snowshoe Group rocks, which occur within the Barkerville Terrane of south central British Columbia. These metasedimentary rocks consist primarily of marble, quartzite and phyllite which in the area of the showing is underlain by garnetiferous schist. Metamorphism of the region varies from chlorite grade to sillimanite and higher. The lode gold deposits of the region occur in rocks metamorphosed no higher than greenschist facies.

Scheelite mineralization occurs within quartz veins which crosscut limestone. The limestone strikes at 160 degrees and dips 20 degrees to the west. The veins strike 020 degrees and dip 30 degrees east.