Abstract
Andesitic or dacitic volcanism has occurred in Taranaki at least since the Miocene. The oldest known volcanic centres are dacitic. Th.e Egmont chain of andesitic vol canoes shows a progression of activity from north to south. The latest eruptions on this line were from Mt Egmont itself, emplacing a tholoid and then breaching the west crater wall. These eruptive events occurred about 400 years ago. Egmont is lssumed to be still potentially active, and renewed.eruptions may well take the form of directed explosions endangering several small townships. © 1964 Taylor & Francis Group, LLC. All rights reserved.
Cite
CITATION STYLE
Grant-Taylor, T. L. (1964). Volcanic History of Western Taranaki. New Zealand Journal of Geology and Geophysics, 7(1), 78–86. https://doi.org/10.1080/00288306.1964.10420158
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