The Kennedy Mountain showing occurs on the east slope of Kennedy Mountain, 1.5 kilometres northwest of the Ingerbelle mine (092HSE004) and 12.5 kilometres southwest of Princeton.

The area between Whipsaw Creek and the Similkameen River is underlain by calcareous siltstone and sandstone, conglomerate, massive and pillowed andesite, andesitic tuff and volcanic breccia of the Upper Triassic Nicola Group. These rocks strike roughly north and dip 25 to 55 degrees west. They are cut by feldspar porphyritic dykes, possibly related to the Early Jurassic Lost Horse Intrusions, striking 025 to 050 degrees.

The showing is hosted in pillowed andesite, with lenses and interbeds of impure limestone and volcanic breccia. Mineralization consists of lenses and veins of chalcopyrite and bornite, with abundant malachite staining. These sulphides appear to be confined to narrow zones of fracturing and shearing that are interlaced with stringers of coarsely crystalline white calcite and epidote.

The showing was trenched and diamond drilled some time in the late 1960's.