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アイスランド · 楯状火山

セイスタレイキャルブンガ

Theistareykir

タイプ
楯状火山
標高
563m
最終噴火
-900年
Stóravíti crater, seen here from the SE, is 600 m across and 140 m deep. It is located in the summit area of the Holocene Theistareykjarbunga shield volcano, part of the northernmost subaerial volcanic system along the Eastern Volcanic Zone of Iceland. The youngest dated eruption in this system produced the Theistareykjahraun lava flow about 2,400 years ago.
Stóravíti crater, seen here from the SE, is 600 m across and 140 m deep. It is located in the summit area of the Holocene Theistareykjarbunga shield volcano, part of the northernmost subaerial volcanic system along the Eastern Volcanic Zone of Iceland. The youngest dated eruption in this system produced the Theistareykjahraun lava flow about 2,400 years ago. · 写真: Photo by Michael Ryan, 1984 (U.S. Geological Survey).
タイプ
楯状火山
国
アイスランド
地域
大西洋 / Iceland Neovolcanic Rift Volcanic Province
標高
563m
座標
65.883, -16.967
最終噴火
-900年
テクトニクス環境
リフト帯 / 海洋地殻 (< 15 km)
火山地形
楯状火山
主要岩石
玄武岩 / ピクライト質玄武岩
地質学的概要

The Holocene Theistareykir fissure system, including the basaltic Theistareykjarbunga shield volcano, extends from north of Myvatn lake to the coast of Iceland. This is the northernmost subaerial volcanic system along the Eastern Volcanic Zone of Iceland. The 30 km3 Theistareykjarbunga shield volcano formed slightly after deglaciation; the youngest dated eruption produced the Theistareykjahraun lava flow about 2,400 years ago.

Wikipedia の要約

英語版の要約

Theistareykjarbunga is a shield volcano in north-eastern Iceland with two fissure vents called Þeistareykjahraun and Borgahraun, and two cones: the 370 m (1,210 ft) Stórahversmór and the 540 m (1,770 ft), 30 km3 (7.2 cu mi) Stóravíti. They both are currently extinct, although there is evidence suggesting the potential for activity such as recent localised uplift and seismicity. The multiple vents make up the Theistareykir (Þeistareykir) volcanic system, with more recent evidence that the former classification as a shield volcano is better considered an embryonic central volcano with associated fissure swarm, as rhyolite has erupted in a limited area. The recent lava has picrite, olivine tholeiite basalt characteristics but before the ice age there were basaltic andesite and rhyolite eruptions. There is a central high temperature geothermal area with numerous steam vents and fumaroles. This has been utilised by a 90 MWe power station.

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噴火履歴

3件の記録用語集
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 · 矢印キーで棒を移動、Enterで表示
紀元前 9500~紀元前 9213 · 1件 · 最大 VEI 0紀元前 6920~紀元前 6633 · 1件 · 最大 VEI 0紀元前 1187~紀元前 900 · 1件 · 最大 VEI 0紀元前 9500紀元前 7493紀元前 5200紀元前 3193紀元前 1187

詳細タイムライン

  1. 紀元前 900年 (±100年)VEI 0地質学的推定
    紀元前 900 ~ 終了日不明
    Storihver (Theistareykjahraun)
  2. 紀元前 6800年VEI 0地質学的推定
    紀元前 6800 ~ 終了日不明
    Borgarhraun and other flows
  3. 紀元前 9500年VEI 0地質学的推定
    紀元前 9500 ~ 終了日不明
    Theistareykjabunga shield volcano

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外部リンク

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