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Tofua

Caldera · 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. · Photo: Aerial photo by Tonga Ministry of Lands, Survey, and Natural Resources, 1990 (published in Taylor and Ewart, 1997). · Wikimedia Commons
Type
Caldera
Country
Tonga
Region
Tonga-Kermadec Volcanic Regions / Tofua Volcanic Arc
Elevation
515m
Coordinates
-19.750, -175.070
Last eruption
2026
Tectonic setting
Subduction zone / Oceanic crust (< 15 km)
Landform
Caldera
Major rock type
Andesite / Basaltic Andesite
Geological summary

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.

From Wikipedia

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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Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1774~1798 · 2 eruptions · max VEI 21822~1846 · 1 eruptions · max VEI 01846~1870 · 2 eruptions · max VEI 21870~1895 · 1 eruptions · max VEI 21895~1919 · 2 eruptions · max VEI 21943~1967 · 1 eruptions · max VEI 21991~2015 · 3 eruptions · max VEI 117741822189519431991

Detailed timeline

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

External links

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