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.
Location of Ember Ridge in British Columbia
Volcanoes edit
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 edit
References edit
- ^ Catalogue of Canadian volcanoes: Mount Cayley volcanic field Archived 2011-06-04 at the Wayback Machine
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