Ember Ridge
Ember Ridge is a volcanic mountain ridge associated with the Mount Cayley volcanic field in British Columbia, Canada. Ember Ridge is made of a series of steep-sided domes of glassy, complexly jointed, hornblende-phyric basalt with the most recent eruptions during the Holocene.[1] The domes have structural similarities which indicate that the domes are similar in age and could have formed by the same foundation.
Volcanoes[]
Lava domes associated with Ember Ridge include:
- Ember Ridge North (50°4′36″N 123°14′20″W / 50.07667°N 123.23889°W)
- Ember Ridge Northeast (50°4′20″N 123°12′55″W / 50.07222°N 123.21528°W)
- Ember Ridge Northwest (50°4′33″N 123°15′23″W / 50.07583°N 123.25639°W)
- Ember Ridge Southeast (50°2′47″N 123°13′19″W / 50.04639°N 123.22194°W)
- Ember Ridge Southwest (50°2′45″N 123°15′8″W / 50.04583°N 123.25222°W)
- Ember Ridge West (50°4′2″N 123°15′41″W / 50.06722°N 123.26139°W)
See also[]
- Mount Cayley
- Cascade Volcanoes
- List of Cascade volcanoes
- List of volcanoes in Canada
- Volcanism of Canada
- Volcanism of Western Canada
References[]
Categories:
- Volcanoes of British Columbia
- Ridges of British Columbia
- Subglacial mounds of Canada
- Ridges of Canada
- Pleistocene volcanoes
- Holocene volcanoes
- Mount Cayley volcanic field
- British Columbia Coast geography stubs