The Smuggler is located in Kokanee Glacier Provincial Park. Smuggler mineralization occurs along a northwest trending structure that hosts Slocan Chief (082FNW119) and Molly Gibson (082FNW121). The galena-sphalerite-arsenopyrite-quartz-iron carbonate veins characteristically are black (manganese oxide) weathering. The veins are unique in that they contain abundant arsenopyrite. The veins are vuggy with variable amounts of chalcedonic quartz.
A grab sample taken in 1987, assayed 1100 grams per tonne silver, 8.43 per cent arsenic, 2.2 grams per tonne gold, 0.22 per cent copper, 4.89 per cent lead and 5.4 per cent zinc (Open File 1988-11).
Production, sometime before 1928 amounted to 13 tonnes grading 9463 grams per tonne silver and 65 per cent lead.