The occurrence lies approximately 800 metres south of Swanson Bay, on the southwest side of a creek which flow northwest into Swanson Bay.

In 1918, ownership of these claims belonged to J. C. McNichols of Swanson Bay, and associates. A small amount of rock trenching was done by the owners that year.

Quartz stringers containing pyrite and minor galena occur in silicified micaceous schist. The mineralized zone lies in a faulted zone parallel to the schistosity which strikes 150 degrees and dips 65 to 75 degrees northeast. Microscopic minerals include pyrrhotite, sphalerite, and chalcopyrite.