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]
| Enid Creek Cone | |
|---|---|
  Enid Creek Cone Location in British Columbia | |
 | |
| Interactive map of Enid Creek Cone | |
| Highest point | |
| Coordinates | 58°23′N 129°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 region | Stikine volcanic belt |
See also
editReferences
edit- ^ "Catalogue of Canadian volcanoes: Enid Creek Cone". Archived from the original on 2011-07-06. Retrieved 2009-06-25.
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