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ニュージーランド · 成層火山

Rumble V Seamount

Rumble V

タイプ
成層火山
標高
400m (海底)
最終噴火
不明
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. · 写真: Courtesy of Ian Wright (National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand).
タイプ
成層火山
国
ニュージーランド
地域
トンガ・ケルマデック / Southern Kermadec Volcanic Arc
標高
400m (海底)
座標
-36.142, 178.196
最終噴火
不明
テクトニクス環境
沈み込み帯 / 海洋地殻 (< 15 km)
火山地形
複成火山
主要岩石
安山岩 / 玄武岩質安山岩
地質学的概要

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.

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