Lewati ke konten utama

Tofua

Kaldera · 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
Tipe
Kaldera
Negara
Tonga
Wilayah
Tonga-Kermadec Volcanic Regions / Tofua Volcanic Arc
Ketinggian
515 m
Koordinat
-19.750, -175.070
Letusan terakhir
2026
Kondisi tektonik
Subduction zone / Oceanic crust (< 15 km)
Bentuk lahan
Caldera
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

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.

Ringkasan Wikipedia

Tofua adalah sebuah kaldera puncak dari sebuah kerucut komposit bersisi curam yang membentuk Pulau Tofua di Tonga. Pulau Tofua berada di kepulauan Ha'apai.

Wikipedia · CC BY-SA · Baca artikel lengkap

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1774~1798 · 2 letusan · VEI maks. 21822~1846 · 1 letusan · VEI maks. 01846~1870 · 2 letusan · VEI maks. 21870~1895 · 1 letusan · VEI maks. 21895~1919 · 2 letusan · VEI maks. 21943~1967 · 1 letusan · VEI maks. 21991~2015 · 3 letusan · VEI maks. 117741822189519431991

Garis waktu rinci

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

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.