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Global Volcanism Program | Image GVP-00332

Auckland, New Zealand's largest city, is constructed over the 600 km2 Auckland Volcanic Field. The field contains more than 50 maars, tuff rings, and scoria cones that were formed during eruptions over the past 193,000 years. Only one volcano was formed during the Holocene. About 620-570 years ago, two phases of eruptive activity formed a low shield volcano capped by a scoria cone at Rangitoto. Photo by Jim Cole (University of Canterbury).

Auckland, New Zealand's largest city, is constructed over the 600 km2 Auckland Volcanic Field. The field contains more than 50 maars, tuff rings, and scoria cones that were formed during eruptions over the past 193,000 years. Only one volcano was formed during the Holocene. About 620-570 years ago, two phases of eruptive activity formed a low shield volcano capped by a scoria cone at Rangitoto.

Photo by Jim Cole (University of Canterbury).

Creative Commons Icon This image is made available under the Creative Commons BY-NC-ND 4.0 license terms.

Galleries: Maars | Craters

Keywords: maar | crater lake | crater


Auckland Volcanic Field