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トンガ · カルデラ

Niuatahi

タイプ
カルデラ
標高
1270m (海底)
最終噴火
不明
タイプ
カルデラ
国
トンガ
地域
トンガ・ケルマデック / Northeast Lau Basin Volcano Group
標高
1270m (海底)
座標
-15.367, -174.003
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
カルデラ
地質学的概要

Niuatahi is a nearly circular caldera ~15 km in diameter, with a floor at a depth of about 2 km (Arculus, 2012). A young cone (Motu Tahi) in the SE sector rises 730 m above the floor to a summit depth of about 1,270 m. The volcano is in the Northeast Lau Basin, ~40 km W of the edifices along the Tofua Volcanic Arc, and 25 km E of the central ridge of the Northeast Lau Spreading Center. The composition of the cone and surrounding floor is predominantly dacite. Towing with seafloor cameras over the cone and various parts of the caldera in 2012 resulted in the discovery of at least three sources of hydrothermal particle venting on the cone's summit and adjacent to the inner caldera walls. The Tonga Ministry of Lands, Environment, Climate Change and Natural Resources named the volcano Niuatahi, which means 'sea' in Tongan, with the small cone of Motutahi meaning 'island in the sea'; it had previously been given an unofficial research cruise designation of "Volcano O."

Wikipedia の要約

英語版の要約

Niuatahi or Volcano O is a submarine volcano located in the far northern territory of Tonga. Since the cone in the middle is named Motutahi, the volcano is sometimes referred to as Niuatahi-Motutahi. Despite not having any record of any eruption, Niuatahi does have a record of recent hydrothermal activity.

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