A discontinuous veinlet up to 5 centimetres thick crosscuts chloritic metavolcanic rocks (andesite?) near the base of a large limestone lens within a predominantly sedimentary portion of the Upper Triassic Stuhini Group. The veinlet strikes to the north- east and dips steeply, and contains chlcopyrite and malachite in a gangue of quartz. A single grab sample yielded values of 58.0 parts per million silver (average) and 5.0 per cent copper (average).