ティンギリリカ火山
Tinguiririca
成層火山 · Chile · 4280m
- タイプ
- 成層火山
- 国
- Chile
- 地域
- South America Volcanic Regions / Southern Andean Volcanic Arc
- 標高
- 4280m
- 座標
- -34.814, -70.352
- 最終噴火
- 1917年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
Tinguiririca is composed of at least seven Holocene scoria cones W of the Chile-Argentina border constructed along a NNE-SSW fissure over an eroded Pleistocene stratovolcano. The complex was constructed during three eruptive cycles dating back to the middle Pleistocene. The latest activity produced a series of youthful small stratovolcanoes and craters, of which the youngest appear to be Tinguiririca and Fray Carlos. Constant fumarolic activity occurs within and on the NW wall of the summit crater. Hot springs and fumaroles with sulfur deposits are found on the W flanks of the summit cones. A single historical eruption was recorded in 1917.
Wikipedia の要約
英語版の要約Tinguiririca Volcano is a massive and active stratovolcano located in Chile's VI Region (O'Higgins) near the Argentinian border. Constant fumarolic activity occurs within and on the NW wall of its summit crater and hot springs and fumaroles can also be seen on the western flanks, as illustrated by the image on the right. It was near this volcano that the Uruguayan Air Force Flight 571 crashed in 1972, and those passengers who had survived the crash were lost for 72 days.
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噴火履歴
詳細タイムライン
- 1994年VEI 2地質学的推定1994-01-15 ~ 1994-01-15
- 1917年VEI 1観測記録1917 ~ 進行中
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。