Franklin Glacier Volcano is a deeply eroded and huge 20 km (12 mi) long and 6 km (4 mi) wide caldera complex in southwestern British Columbia, Canada, located east-southeast of the Silverthrone Caldera in the Hoodoo Creek and Franklin Glacier area on the northwest flank of the Waddington Massif of the Pacific Ranges of the Coast Mountains. Franklin Glacier Volcano consists of a series of dikes and high-level magma intrusions.
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“We are like travellers using the cinders of a volcano to roast their eggs. Whilst we see that it always stands ready to clothe what we would say, we cannot avoid the question whether the characters are not significant of themselves.”
—Ralph Waldo Emerson (1803–1882)