Gold production (1876 to 1880) totalling 10,698 grams is recorded for Porcupine Creek, which flows into Porcupine Lake, located about 14 kilometres west of the north end of Dease Lake.
The creek drains an area underlain by volcanic sandstone, argillaceous tuff and conglomerate of the Upper Triassic undivided Shonektaw and Nazcha formations (Takla Group) and also upper Mississippian-Permian serpentinite, peridotite and pyroxenite of the Cache Creek Complex.