セント・ヴィンセント島のソフリエール火山の噴火,1971年-1972年
まとめ
1971年から1972年のセントヴィンセントのスフリエール火山噴火は,静かで水中のイベントでした. 溶岩の流出により島が形成され,1902年の爆発的な噴火と大きく対照的です.
科学分野:
- 火山学 火山学とは
- 地質学 地質学 地質学
背景:
- セント・ヴィンセント島のスフリエール火山は,重大な噴火の歴史があります.
- 1902年から1903年のような以前の噴火は,非常に爆発的で破壊的でした.
研究 の 目的:
- 1971年から1972年のスフリエール火山の噴火を記録し,特徴づけること.
- 噴火様式と関連する現象を歴史的噴火と比較するために.
主な方法:
- 噴火期間 (1971年10月 - 1972年3月) の観測データ収集.
- 噴火した物質 (ベースルティック・アンデサイト・ラバ) の分析.
- クレーター湖のバチメトリと島形成の評価.
主要な成果:
- 約80 x 10^6 m^3の玄武岩アンデサイト・ラバが挤出されました.
- 噴火は,主に180m深いクレーター湖内の水中噴火でした.
- 崖っぷちの島がクレーター湖から浮上した.
- 噴火は,地震活動が最小限で,穏やかな噴出スタイルで特徴付けられました.
結論:
- 1971年から1972年のスフリエール噴火は,爆発的な噴火とは異なり,噴出量があり,水中のイベントでした.
- 新しい島の形成は,噴出的な火山活動中に重要な地形の変化の可能性を示しています.
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