The Anuk RB 16 showing is located about 91 kilometres south-southwest of the town of Telegraph Creek.

The Anuk RB 16 showing is underlain by volcanic rock of the Upper Triassic Stuhini Group. A carbonate alteration zone hosts quartz-carbonate veins up to 5 centimetres thick and containing bornite, chalcopyrite and hematite. A grab sample of chlorite-epidote altered andesite assayed 0.8 per cent copper, 0.78 gram per tonne gold and and 7.9 grams per tonne silver (Sample W9) (Assessment Report 21146).

Refer to Anuk RB 18 and Anuk RB 12 (104G 497) for expanded geological information and a common work history.