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トファ山

Tofua

カルデラ · Tonga · 515m

A small plume rises from Lofia cone on the N side of the caldera lake of Tofua volcano in this 1990 aerial photograph. Recent tephra was emplaced onto the caldera rim to the NW. The steep walls of the 5-km-wide caldera are about 500 m high. Three post-caldera cones were constructed at the N end of a cold fresh-water caldera lake, whose surface lies only 30 m above sea level.
A small plume rises from Lofia cone on the N side of the caldera lake of Tofua volcano in this 1990 aerial photograph. Recent tephra was emplaced onto the caldera rim to the NW. The steep walls of the 5-km-wide caldera are about 500 m high. Three post-caldera cones were constructed at the N end of a cold fresh-water caldera lake, whose surface lies only 30 m above sea level. · 写真: Aerial photo by Tonga Ministry of Lands, Survey, and Natural Resources, 1990 (published in Taylor and Ewart, 1997). · Wikimedia Commons
タイプ
カルデラ
Tonga
地域
Tonga-Kermadec Volcanic Regions / Tofua Volcanic Arc
標高
515m
座標
-19.750, -175.070
最終噴火
2026年
テクトニクス環境
Subduction zone / Oceanic crust (< 15 km)
火山地形
Caldera
主要岩石
Andesite / Basaltic Andesite
地質学的概要

The low, forested Tofua Island in the central part of the Tonga Islands group is the emergent summit of a large stratovolcano that was seen in eruption by Captain Cook in 1774. The summit contains a 5-km-wide caldera whose walls drop steeply about 500 m. Three post-caldera cones were constructed at the northern end of a cold fresh-water caldera lake, whose surface lies only 30 m above sea level. The easternmost cone has three craters and produced young basaltic andesite lava flows, some of which traveled into the caldera lake. The largest and northernmost of the cones, Lofia, has a steep-sided crater that is 70 m wide and 120 m deep and has been the source of historical eruptions, first reported in the 18th century. The fumarolically active crater of Lofia has a flat floor formed by a ponded lava flow.

Wikipedia の要約

英語版の要約

Tofua is a volcanic island in Tonga. Located in the Haʻapai island group, it is a steep-sided composite cone with a summit caldera. It is part of the highly active Kermadec-Tonga subduction zone and its associated volcanic arc, which extends from New Zealand north-northeast to Fiji, and is formed by the subduction of the Pacific Plate under the Indo-Australian Plate. It lies about 100 km (62 mi) above a very active seismic zone. It is connected to the nearby island of Kao by a submarine ridge. As of August 2025, the cone contains a lava lake.

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噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
1774~1798 · 2件 · 最大 VEI 21822~1846 · 1件 · 最大 VEI 01846~1870 · 2件 · 最大 VEI 21870~1895 · 1件 · 最大 VEI 21895~1919 · 2件 · 最大 VEI 21943~1967 · 1件 · 最大 VEI 21991~2015 · 3件 · 最大 VEI 117741822189519431991

詳細タイムライン

  1. 2015年VEI 0観測記録
    2015-10-02 ~ 2026-03-17
    Lofia crater
  2. 2004年VEI 1観測記録
    2004-03-19 ~ 2014-10-18
    Lofia crater
  3. 1993年VEI 0地質学的推定
    1993-04-29 ~ 進行中
    Northern part of caldera
  4. 1958年VEI 2観測記録
    1958-12-31 ~ 1960-07-02
    Northern part of caldera
  5. 1906年VEI 2観測記録
    1906-01 ~ 1906-02
    Northern part of caldera
  6. 1906年VEI 2観測記録
    1906-12 ~ 進行中
    Northern part of caldera
  7. 1885年VEI 2観測記録
    1885-10 ~ 進行中
  8. 1854年VEI 2観測記録
    1854 ~ 進行中
  9. 1847年VEI 1観測記録
    1847-07-10 ~ 進行中
  10. 1845年VEI 0観測記録
    1845-07-01 ~ 進行中
  11. 1792年VEI 0観測記録
    1792 ~ 進行中
  12. 1774年VEI 2観測記録
    1774-06 ~ 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。