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Vestmannaeyjar

割れ目火口 · Iceland · 283m

The island of Heimaey, about 10 km off the south coast of Iceland, is part of the Vestmannaeyjar volcanic system, which comprises numerous islands and submarine vents. Heimaey probably formed in the Holocene, through numerous eruptions. Here, an ash-laden eruption plume rises above a volcanic cone behind the town of Vestmannaeyjar in 1973. The water pumping operation in the foreground was designed to cool the front of an advancing lava flow that threatened the town and its harbor.
The island of Heimaey, about 10 km off the south coast of Iceland, is part of the Vestmannaeyjar volcanic system, which comprises numerous islands and submarine vents. Heimaey probably formed in the Holocene, through numerous eruptions. Here, an ash-laden eruption plume rises above a volcanic cone behind the town of Vestmannaeyjar in 1973. The water pumping operation in the foreground was designed to cool the front of an advancing lava flow that threatened the town and its harbor. · 写真: Photo by Jack Lockwood, 1973 (U.S. Geological Survey). · Wikimedia Commons
タイプ
割れ目火口
Iceland
地域
Atlantic Ocean Volcanic Regions / Iceland Neovolcanic Rift Volcanic Province
標高
283m
座標
63.416, -20.266
最終噴火
1973年
テクトニクス環境
Rift zone / Oceanic crust (< 15 km)
火山地形
Cluster
主要岩石
Basalt / Picro-Basalt
地質学的概要

The mostly submarine Vestmannaeyjar volcanic system is the southernmost and youngest volcanic center of the Eastern Volcanic Zone that cuts across E-central Iceland. It consists of a roughly 30 x 40 km group of basaltic islands and submarine cones occupying a shallow shelf off the S coast of Iceland, and was the site of two of Iceland's most noted 20th-century eruptions. The island of Surtsey grew from the ocean floor during 1963-67. The island of Heimaey, 20 km to the NE, was the site of eruptions in 1973, during which lava flows partially overran the town of Vestmannaeyjar and threatened its harbor. Twenty-two postglacial eruption sites are known, and all ten subaerial vents on Heimaey are of Holocene age.

Wikipedia の要約

要約が短いです。詳細は記事全文をご覧ください。

エルトフェットル は、アイスランドのヘイマエイ島にある標高200メートルの火山である。エルドフェトルとも表記する。

Wikipedia · CC BY-SA · 記事全文を読む

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
8050 BCE~7716 BCE · 1件 · 最大 VEI 47716 BCE~7382 BCE · 1件 · 最大 VEI 36379 BCE~6045 BCE · 1件 · 最大 VEI ?4709 BCE~4375 BCE · 1件 · 最大 VEI ?4375 BCE~4041 BCE · 1件 · 最大 VEI 34041 BCE~3707 BCE · 1件 · 最大 VEI ?1305~1639 · 1件 · 最大 VEI ?1639~1973 · 3件 · 最大 VEI 38050 BCE5711 BCE3038 BCE700 BCE1639

詳細タイムライン

  1. 1973年VEI 3観測記録
    1973-01-23 ~ 1973-06-28
    Heimaey (Eldfell)
  2. 1963年VEI 3観測記録
    1963-11-08 ~ 1967-06-05
    Surtsey
  3. 1896年VEI ?観測記録
    1896-09 ~ 進行中
    South or SE of Hellisey
  4. 1637年VEI ?観測記録
    1637-10 ~ 1638-02-28
    SW of Heimaey ?
  5. 紀元前 3950年 (±300年)VEI ?地質学的推定
    BCE 3950 ~ 進行中
    Heimaey (Helgafell)
  6. 紀元前 4270年 (±200年)VEI 3地質学的推定
    BCE 4270 ~ 進行中
    Heimaey (Saefell tuff cone)
  7. 紀元前 4550年 (±500年)VEI ?地質学的推定
    BCE 4550 ~ 進行中
    Heimaey (Stórhöfdi tuff cone)
  8. 紀元前 6050年VEI ?地質学的推定
    BCE 6050 ~ 進行中
    Alsey, Brandur, Sudurey, Hellisey
  9. 紀元前 7550年VEI 3地質学的推定
    BCE 7550 ~ 進行中
    NW Heimaey (Nordurklettar)
  10. 紀元前 8050年VEI 4地質学的推定
    BCE 8050 ~ 進行中
    NW Heimaey (Háin tuff ring)

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。