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.
Lava domes associated with Ember Ridge include:
Volcanoes of the Garibaldi Volcanic Belt | |
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