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Tofua

칼데라 · 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. · 사진: Aerial photo by Tonga Ministry of Lands, Survey, and Natural Resources, 1990 (published in Taylor and Ewart, 1997). · Wikimedia Commons
화산 유형
칼데라
국가
Tonga
지역
Tonga-Kermadec Volcanic Regions / Tofua Volcanic Arc
해발
515m
좌표
-19.750, -175.070
마지막 분화
2026년
판구조 환경
Subduction zone / Oceanic crust (< 15 km)
화산 지형
Caldera
주요 암석
Andesite / Basaltic Andesite
지질학적 요약

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 요약

영어 요약

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.

Wikipedia · CC BY-SA · 전체 기사 보기

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
1774~1798 · 2건 · 최고 VEI 21822~1846 · 1건 · 최고 VEI 01846~1870 · 2건 · 최고 VEI 21870~1895 · 1건 · 최고 VEI 21895~1919 · 2건 · 최고 VEI 21943~1967 · 1건 · 최고 VEI 21991~2015 · 3건 · 최고 VEI 117741822189519431991

상세 타임라인

  1. 2015년VEI 0관측 기록
    2015-10-02 ~ 2026-03-17
    Lofia crater
  2. 2004년VEI 1관측 기록
    2004-03-19 ~ 2014-10-18
    Lofia crater
  3. 1993년VEI 0지질학적 추정
    1993-04-29 ~ 진행 중
    Northern part of caldera
  4. 1958년VEI 2관측 기록
    1958-12-31 ~ 1960-07-02
    Northern part of caldera
  5. 1906년VEI 2관측 기록
    1906-01 ~ 1906-02
    Northern part of caldera
  6. 1906년VEI 2관측 기록
    1906-12 ~ 진행 중
    Northern part of caldera
  7. 1885년VEI 2관측 기록
    1885-10 ~ 진행 중
  8. 1854년VEI 2관측 기록
    1854 ~ 진행 중
  9. 1847년VEI 1관측 기록
    1847-07-10 ~ 진행 중
  10. 1845년VEI 0관측 기록
    1845-07-01 ~ 진행 중
  11. 1792년VEI 0관측 기록
    1792 ~ 진행 중
  12. 1774년VEI 2관측 기록
    1774-06 ~ 진행 중

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