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Global Volcanism Program | Image GVP-01595

Motukorea (also known as Brown's Island) in Waitemata Harbour, New Zealand, is composed of a remnant tuff ring (right side), scoria cones (center), and lava flows that form the flat peninsula in the foreground. It is one of more than 50 Pleistocene-to-Holocene centers in the Auckland Volcanic Field. The low-angle slopes of lava flows from Rangitoto are visible to the north in the background. Photo by B. Thompson (published in Green and Short, 1971).

Motukorea (also known as Brown's Island) in Waitemata Harbour, New Zealand, is composed of a remnant tuff ring (right side), scoria cones (center), and lava flows that form the flat peninsula in the foreground. It is one of more than 50 Pleistocene-to-Holocene centers in the Auckland Volcanic Field. The low-angle slopes of lava flows from Rangitoto are visible to the north in the background.

Photo by B. Thompson (published in Green and Short, 1971).

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

Keywords: tuff ring | scoria cone | island volcano


Auckland Volcanic Field