The PI occurrence is located approximately 27 kilometres south of Ashcroft. The exact location is uncertain.

The area straddles the contact between the Upper Triassic to Lower Jurassic Guichon Creek Batholith Border phase quartz diorites and Middle and Upper Cretaceous Spences Bridge Group volcanics.

Locally, hematite with minor chalcopyrite occurs in a shear zone within quartz diorites.

Work History

In 1970, Tower Mines Ltd. completed a 16.0 line-kilometre induced polarization survey on the area as the PI claim.