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Gannet Island (New Zealand) : ウィキペディア英語版
Gannet Island (New Zealand)

Gannet Island (Karewa in Māori) is a small island some offshore from Kawhia on the west coast of New Zealand's North Island.
==Description==
The island consists of the eroded remnant of a tuff ring, erupted about half a million years ago. It is considerably younger than, and compositionally distinct from, the nearby onshore Alexandra Volcanics (Mount Karioi and Mount Pirongia) and Okete Volcanics. It is located on the eastern edge of the North Taranaki Graben, rising above sea level from a base about deep.〔R. M. Briggs, M. D. Rosenberg, P. J. de Lange, T. Itaya, P. R. King and R. C. Price. (1997). (Geology and geochemistry of Gannet (Karewa) Island, Tasman Sea: a rift-related nephelinitic tuff ring ), ''New Zealand Journal of Geology and Geophysics'', 40, 263-272.〕

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