| Enid Creek Cone | |
|---|---|
| |
| Interactive map of Enid Creek Cone | |
| Highest point | |
| Coordinates | 58°23′N129°31′W / 58.38°N 129.52°W |
| Geography | |
| Location | British Columbia, Canada |
| District | Cassiar Land District |
| Geology | |
| Rock age | Pleistocene |
| Mountain type | Subglacial mound |
| Volcanic zone | Stikine volcanic belt |
Enid Creek Cone is a subglacial mound in northwestern British Columbia, Canada, located in the Dark Mountain area. It last erupted during the Pleistocene epoch. [1]