エイヤフィヤトラヨークトル
Eyjafjallajokull
成層火山 · Iceland · 1651m

- タイプ
- 成層火山
- 国
- Iceland
- 地域
- Atlantic Ocean Volcanic Regions / Iceland Neovolcanic Rift Volcanic Province
- 標高
- 1651m
- 座標
- 63.633, -19.633
- 最終噴火
- 2010年
- テクトニクス環境
- Rift zone / Oceanic crust (< 15 km)
- 火山地形
- Composite
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
Eyjafjallajökull (also known as Eyjafjöll) is located west of Katla volcano. It consists of an elongated ice-covered stratovolcano with a 2.5-km-wide summit caldera. Fissure-fed lava flows occur on both the E and W flanks, but are more prominent on the western side. Although the volcano has erupted during historical time, it has been less active than other volcanoes of Iceland's eastern volcanic zone, and relatively few Holocene lava flows are known. An intrusion beneath the S flank from July-December 1999 was accompanied by increased seismic activity. The last historical activity prior to an eruption in 2010 produced intermediate-to-silicic tephra from the central caldera during December 1821 to January 1823.
噴火履歴
詳細タイムライン
- 2010年VEI 4観測記録2010-03-20 ~ 2010-06-23ENE flank (Fimmvörduháls) and summit
- 1821年VEI 2観測記録1821-12-19 ~ 1823-01-01
- 1612年VEI 2観測記録1612 ~ 進行中
- 920年VEI 3地質学的推定920 ~ 進行中NW flank (Skerin ridge)
- 550年VEI ?地質学的推定550 ~ 進行中
外部リンク
- 日本語版Wikipediaには未登録です。Wikidataで作成できます。
- 🔗 Smithsonian GVP 原典ページ
⚠ 参考情報です。緊急対応には使用しないでください。