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complexes in the central Anahim
Volcanic Belt. As a result, the swarms are thought to represent the roots of a
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to the volcanic centre at the surface, which has been extensively eroded to remnants of eruptive
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Mantle Plumes: Their
Identification Through Time (Special Paper (Geological Society of America))
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Dewit, Megan (2014). "The geothermal potential of Nazko Cone, British
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magma system in which they are the magma conduits connecting the underlying
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This article about a specific
Canadian geological feature is a
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186:: 895–908.
92:peralkaline
37:dike swarms
503:Categories
316:Nazko Cone
106:References
248:Volcanoes
61:comendite
57:trachyte
188:Bibcode
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