カオ島
Kao
成層火山 · Tonga · 1009m

- タイプ
- 成層火山
- 国
- Tonga
- 地域
- Tonga-Kermadec Volcanic Regions / Tofua Volcanic Arc
- 標高
- 1009m
- 座標
- -19.668, -175.016
- 最終噴火
- 1847年
- テクトニクス環境
- Subduction zone / Oceanic crust (< 15 km)
- 火山地形
- Composite
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
The symmetrical Kao rises steeply from the ocean about 6 km N of Tofua Island in Tonga. It is elongated NNE-SSW and, with the exception of a small flat area on the SSW coast, rises at angles exceeding 35° to the summit, which has a series of small coalescing craters. The lower flanks of the basaltic andesite volcano are densely jungled, but the upper slopes are almost vegetation free. There are no fresh-looking lava flows, although the absence of sufficient time for erosion to produce deep gullies or high sea cliffs suggests a very recent origin. A missionary on a ship anchored at Tofua reported that "smoke" was "pouring forth" from Kao on 10 July 1847.
Wikipedia の要約
英語版の要約Kao is an island and stratovolcano in the Haʻapai island group of Tonga. It lies about 6 km (3.7 mi) north of Tofua island and reaches 1,030 m (3,379 ft) above sea level, the highest point in Tonga.
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噴火履歴
詳細タイムライン
- 1847年VEI 2観測記録1847-07-10 ~ 進行中
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。