The Keefers showing is located in old opencuts north of the Nahatlatch River, 2.4 kilometres southwest of Keefers.

The area is underlain by Lower and Middle Jurassic Ladner Group metasediments comprising argillite, slate and phyllite. These occur in normal contact with a northwest trending belt of lower greenschist facies Permian(?) to Lower Cretaceous Bridge River Complex (Group) phyllites and schists.

The showings were staked by D. Pride in 1954 then optioned to Northwest Ventures in 1955. Opencutting, surface work and diamond drilling are reported. A representative sample sent to Sudbury is reported to have assayed 1.42 per cent copper, 2.24 per cent nickel, 0.15 per cent cobalt, 3.77 grams per tonne platinum and 0.79 gram per tonne palladium (National Mineral Inventory 92I/4 Ni1).