This occurrence is situated on the western flank of Sulphurets Mountain approximately 600 metres east of Sulphurets Glacier West.
Chalcopyrite and galena occur in an area underlain by rock of the Lower Jurassic Unuk River Formation, Hazelton Group (Annual Report 1968, Figure 8). The area is underlain by mixed sedimentary rocks with tuffaceous interbeds (Open File 1988-4). No further details of the showing are available.