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ニウアフォオウ島

Niuafo'ou

楯状火山 · Tonga · 260m

Niuafo'ou is a low, 8-km-wide ring-shaped island that forms the summit of a largely submerged shield volcano. The 5-km-wide caldera is seen here from its eastern rim, displaying caldera lakes, the large Vai Lahi (background), and the much smaller Vai Si'i (foreground). The caldera is mostly filled by Vai Lahi with a lake bottom that extends to below sea level. Historical eruptions recorded since 1814 have often damaged villages on the island.
Niuafo'ou is a low, 8-km-wide ring-shaped island that forms the summit of a largely submerged shield volcano. The 5-km-wide caldera is seen here from its eastern rim, displaying caldera lakes, the large Vai Lahi (background), and the much smaller Vai Si'i (foreground). The caldera is mostly filled by Vai Lahi with a lake bottom that extends to below sea level. Historical eruptions recorded since 1814 have often damaged villages on the island. · 写真: Photo by Paul Taylor (published in Taylor and Ewart, 1997). · Wikimedia Commons
タイプ
楯状火山
Tonga
地域
Tonga-Kermadec Volcanic Regions / Northeast Lau Basin Volcano Group
標高
260m
座標
-15.600, -175.630
最終噴火
1946年
テクトニクス環境
Subduction zone / Oceanic crust (< 15 km)
火山地形
Shield
主要岩石
Basalt / Picro-Basalt
地質学的概要

Niuafo'ou ("Tin Can Island") is a low 8-km-wide island that forms the summit of a largely submerged basaltic shield volcano in the north central Lau Basin about 170 km W of the northern end of the Tofua volcanic arc. The circular island encloses a 5-km-wide caldera that is mostly filled by a lake whose bottom extends to below sea level. The inner walls of the caldera drop sharply to the lake, named Big Lake (or Vai Lahi), which contains several small islands and pyroclastic cones on its NE shore. Eruptions recorded since 1814, mostly from circumferential fissures on the west-to-south side of the island, have often damaged villages. A major eruption in 1946 forced evacuation of most of its 1,200 inhabitants.

Wikipedia の要約

ニウアフォオウ島(ニウアフォオウとう、Niuafoʻou)は、トンガの島。ニウアトプタプ島、タファフィ島とともにニウアス諸島を形成する。首都ヌクアロファのあるトンガタプ島より北に574km、ヴァヴァウ諸島より北に337km離れており、トンガ最北の島のひとつである。面積15km2、人口650人(2006年)。火山島であり、過去に何度も大噴火を起こしていて、現在でも活発に活動している。

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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
1814~1831 · 1件 · 最大 VEI 21848~1865 · 1件 · 最大 VEI 01865~1882 · 1件 · 最大 VEI 11882~1900 · 2件 · 最大 VEI 41900~1917 · 1件 · 最大 VEI 21917~1934 · 1件 · 最大 VEI 21934~1951 · 4件 · 最大 VEI 21968~1985 · 1件 · 最大 VEI 018141848190019341968

詳細タイムライン

  1. 1985年VEI 0観測記録
    1985-03-21 ~ 1985-03-22
    NE part of caldera lake (Vai Lahi)
  2. 1947年VEI ?地質学的推定
    1947-01 ~ 進行中
  3. 1946年VEI 2観測記録
    1946-09-09 ~ 1946-09-17
    North flank
  4. 1943年VEI 2観測記録
    1943-09-26 ~ 1943-10-16
    SW flank
  5. 1935年VEI 2観測記録
    1935-12-07 ~ 1936-02
    South flank
  6. 1929年VEI 2観測記録
    1929-07-25 ~ 1929-07-26
    West flank
  7. 1912年VEI 2観測記録
    1912-10-15 ~ 進行中
    West side, near Alele 'Uta village
  8. 1887年VEI 2観測記録
    1887 ~ 進行中
  9. 1886年VEI 4観測記録
    1886-08-31 ~ 1886-09-18
    NE side of caldera
  10. 1867年VEI 1観測記録
    1867-04-12 ~ 進行中
    SSW flank
  11. 1853年VEI 0観測記録
    1853-06-24 ~ 1853-06-24
    SW caldera rim (Ahau village area)
  12. 1814年VEI 2観測記録
    1814 ~ 進行中
    South end of caldera ?

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。