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Tofua

Caldera · Tonga · 515 m

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. · Foto: Aerial photo by Tonga Ministry of Lands, Survey, and Natural Resources, 1990 (published in Taylor and Ewart, 1997). · Wikimedia Commons
Tipo
Caldera
Paese
Tonga
Regione
Tonga e Kermadec / Tofua Volcanic Arc
Altitudine
515 m
Coordinate
-19.750, -175.070
Ultima eruzione
2026
Contesto tettonico
Subduction zone / Oceanic crust (< 15 km)
Forma vulcanica
Caldera
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

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.

Sintesi da Wikipedia

Riassunto in inglese

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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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
1774~1798 · 2 eruzioni · VEI max. 21822~1846 · 1 eruzioni · VEI max. 01846~1870 · 2 eruzioni · VEI max. 21870~1895 · 1 eruzioni · VEI max. 21895~1919 · 2 eruzioni · VEI max. 21943~1967 · 1 eruzioni · VEI max. 21991~2015 · 3 eruzioni · VEI max. 117741822189519431991

Cronologia dettagliata

  1. 2015VEI 0Osservata
    2015-10-02 – 2026-03-17
    Lofia crater
  2. 2004VEI 1Osservata
    2004-03-19 – 2014-10-18
    Lofia crater
  3. 1993VEI 0Stima geologica
    1993-04-29 – In corso
    Northern part of caldera
  4. 1958VEI 2Osservata
    1958-12-31 – 1960-07-02
    Northern part of caldera
  5. 1906VEI 2Osservata
    1906-01-16 – 1906-02-16
    Northern part of caldera
  6. 1906VEI 2Osservata
    1906-12-16 – In corso
    Northern part of caldera
  7. 1885VEI 2Osservata
    1885-10-16 – In corso
  8. 1854VEI 2Osservata
    1854-07-02 – In corso
  9. 1847VEI 1Osservata
    1847-07-10 – In corso
  10. 1845VEI 0Osservata
    1845-07-01 – In corso
  11. 1792VEI 0Osservata
    1792 – In corso
  12. 1774VEI 2Osservata
    1774-06 – In corso

Link esterni

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