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Nueva Zelanda · Estratovolcán

Rumble V Seamount

Rumble V

Tipo
Estratovolcán
Altitud
400 m (submarino)
Última erupción
Desconocido
A bathymetric map view shows Rumble V submarine volcano at the southern end of the South Kermadec volcano group. A large plume of gas bubbles was acoustically detected rising from the summit in 1992. Rumble V, the southernmost of a group of seamounts on the southern Kermadec Ridge known as the Rumbles, rises more than 2,000 m to about 400 m below the sea surface.
A bathymetric map view shows Rumble V submarine volcano at the southern end of the South Kermadec volcano group. A large plume of gas bubbles was acoustically detected rising from the summit in 1992. Rumble V, the southernmost of a group of seamounts on the southern Kermadec Ridge known as the Rumbles, rises more than 2,000 m to about 400 m below the sea surface. · Foto: Courtesy of Ian Wright (National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand).
Tipo
Estratovolcán
País
Nueva Zelanda
Región
Tonga y Kermadec / Southern Kermadec Volcanic Arc
Altitud
400 m (submarino)
Coordenadas
-36.142, 178.196
Última erupción
Desconocido
Contexto tectónico
Zona de subducción / Corteza oceánica (< 15 km)
Forma volcánica
Compuesto
Roca principal
Andesita / Andesita basáltica
Resumen geológico

Rumble V was discovered in 1992 at the southernmost end of the Rumble seamounts on the southern Kermadec Ridge, 17 km ESE of Rumble IV. Andesitic and basaltic andesite rocks have been dredged from this volcano, which rises more than 2,000 m to nearly 400 m below the ocean surface and shows a pristine morphology. A large plume of gas bubbles was acoustically detected rising from the summit in 1992, and subsequent expeditions detected evidence of vigorous hydrothermal activity.

Historial de erupciones

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Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.