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Tuhua/Mayor Island
楯状火山 · New Zealand · 355m

- タイプ
- 楯状火山
- 国
- New Zealand
- 地域
- Tonga-Kermadec Volcanic Regions / Taupo Volcanic Arc
- 標高
- 355m
- 座標
- -37.280, 176.250
- 最終噴火
- -5055年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Shield
- 主要岩石
- Rhyolite
地質学的概要
The 4-km-wide Tuhua/Mayor Island, offshore of North Island in the Bay of Plenty, is the emergent portion of a 15-km-wide peralkaline shield volcano constructed between about 120,000 and 35,000 years ago. A 3-km-wide composite caldera was formed in two or three collapse events, the last of which took place about 6,300 years ago, and was accompanied by a Plinian eruption that produced tephra deposits up to 70 cm thick on the mainland. Post-caldera eruptions generated a series of lava domes and flows emplaced from NNE-trending vents within the caldera that have filled it to depths of at least 180 m. The latest eruption has not been dated, but was considered by Houghton et al. (1992) to have occurred perhaps only 500-1,000 years ago.
Wikipedia の要約
英語版の要約Mayor Island / Tūhua is a dormant shield volcano located 26 km (16 mi) off the Bay of Plenty coast of New Zealand's North Island. It covers 13 km2 (5 sq mi).
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噴火履歴
詳細タイムライン
- 紀元前 5055年 (±155年)VEI 5地質学的推定BCE 5055 ~ 進行中South end of caldera, Taratimi Bay
- 紀元前 6050年 (±75年)VEI ?地質学的推定BCE 6050 ~ 進行中SE caldera rim
外部リンク
⚠ 参考情報です。緊急対応には使用しないでください。