| Second Canyon Cone | |
| Elevation M: | 300 |
| Location: | British Columbia, Canada |
| Range: | Boundary Ranges |
| Coordinates: | 56.41°N -130.72°W |
| Type: | Volcanic plug |
| Age: | Holocene |
| Volcanic Arc/Belt: | Northern Cordilleran Volcanic Province |
| Last Eruption: | Holocene |
Second Canyon Cone, also called Canyon Creek Cone is a cinder cone in the Boundary Ranges of the Coast Mountains in northwestern British Columbia, Canada. It is a volcanic feature of the Iskut-Unuk River Cones which is part of the Northern Cordilleran Volcanic Province and formed in the past 10,000 years of the Holocene epoch.[1]