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.
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Location of Ember Ridge in British Columbia
Volcanoes
Lava domes associated with Ember Ridge include:
- Ember Ridge North (50°4′36″N 123°14′20″W)
- Ember Ridge Northeast (50°4′20″N 123°12′55″W)
- Ember Ridge Northwest (50°4′33″N 123°15′23″W)
- Ember Ridge Southeast (50°2′47″N 123°13′19″W)
- Ember Ridge Southwest (50°2′45″N 123°15′8″W)
- Ember Ridge West (50°4′2″N 123°15′41″W)
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See also
References
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