Articles on Mount Cayley Volcanic Field, Including: Mount Cayley, Mount Fee, Mount Brew (Cheakamus River), Ring Mountain (British Columbia), Ember Rid

Hephaestus Books represents a new publishing paradigm, allowing disparate content sources to be curated into cohesive, relevant, and informative books. To date, this content has been curated from Wikipedia articles and images under Creative Commons licensing, although as Hephaestus Books continues to increase in scope and dimension, more licensed and public domain content is being added. We believe books such as this represent a new and exciting lexicon in the sharing of human knowledge. This particular book is a collaboration focused on Mount Cayley volcanic field.More info: The Mount Cayley volcanic field is a remote north-south trending volcanic zone on the Coast of British Columbia that stretches from the Pemberton Icefield to the Squamish River. The field is located in the Sea-to-Sky Corridor of southwestern British Columbia, Canada. It forms the central segment of the Garibaldi Volcanic Belt, the Canadian portion of the Cascade Volcanic Arc, which extends from Northern California to southwestern British Columbia. Most of the Cayley volcanoes were formed during periods of volcanism under sheets of glacial ice throughout the last glacial period. These subglacial eruptions formed steep, flat-topped volcanoes and subglacial lava domes, most of which have been entirely exposed by deglaciation. However, at least two volcanoes predate the last glacial period and both are highly eroded. The field gets its name from Mount Cayley, the largest and most persistent volcano, located at the southern end of the Powder Mountain Icefield. This icefield covers much of the central portion of the volcanic field and is one of the several glacial fields in the Pacific Ranges of the Coast Mountains.

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