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Curtis Island volcano

Submarine volcano 137 m / 449 ft
New Zealand, Kermadec Islands, -30.54°S / -178.56°W
Current status: normal or dormant (1 out of 5) | Reports
Curtis Island volcano books
Typical eruption style: sin especificar
Erupciones del volcán Curtis Island: unknown, no recent eruptions
Fecha / HoraRevista / ProfundidadDistanciaUbicación
Mon, 22 Jun 2020
Mon, 22 Jun 06:49 UTCM 4.6 / 170.8 km23 km New Zealand
Tue, 14 Apr 2020
Tue, 14 Apr 15:04 UTCM 5.1 / 33 km17 km New Zealand
Wed, 8 Apr 2020
Wed, 8 Apr 06:30 UTCM 4.7 / 321.5 km19 km New Zealand
Tue, 7 Jan 2020
Tue, 7 Jan 02:54 UTCM 4.4 / 279.3 km21 km New Zealand
Sun, 19 May 2019
Sun, 19 May 13:29 UTCM 5.0 / 483.8 km22 km New Zealand
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Background:

Curtis and nearby Cheeseman Islands are the uplifted portion of a submarine volcano astride the Kermadec Ridge. The age of the small islands is considered to be Pleistocene, and rocks consist dominantly, if not entirely, of andesitic pyroclastic-flow deposits (Lloyd, 1992). Curtis Island, only 500 x 800 m in diameter and 137-m high, contains a large, fumarolically active crater whose floor is only 10 m above sea level. Reports of possible historical eruptions probably represent increased thermal activity. Geologic studies have documented a remarkable uplift of 18 m of Curtis Island during the past 200 years, with 7 m of uplift occurring between 1929 and 1964 (Doyle et al., 1979). An active submarine magmatic or solfataric vent is believed to exist near Curtis Island, but its activity cannot unequivocally be associated with Curtis volcano (Lloyd, 1992).
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Smithsonian / GVP volcano information

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