Irruputuncu
成層火山 · Chile-Bolivia · 5163m

- タイプ
- 成層火山
- 国
- Chile-Bolivia
- 地域
- South America Volcanic Regions / Central Andean Volcanic Arc
- 標高
- 5163m
- 座標
- -20.730, -68.550
- 最終噴火
- 1995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
Irruputuncu is a small stratovolcano that straddles the Chile/Bolivia border. It is the youngest and most southerly of a NE-SW-trending chain of volcanoes. It was constructed within the collapse scarp of a Holocene debris avalanche whose deposit extends to the SW. Subsequent eruptions filled much of this scarp and produced thick, viscous lava flows down the W flank. The summit complex contains two craters, the southernmost of which is fumarolically active. The first unambiguous historical eruption took place in November 1995, when phreatic explosions produced dark ash clouds.
Wikipedia の要約
英語版の要約Irruputuncu is a volcano in the commune of Pica, Tamarugal Province, Tarapacá Region, Chile, as well as San Pedro de Quemes Municipality, Nor Lípez Province, Potosí Department, Bolivia. The mountain's summit is 5,163 m (16,939 ft) high and has two summit craters—the southernmost 200 m (660 ft)-wide one has active fumaroles. The volcano also features lava flows, block and ash flows and several lava domes. The volcano is part of the Andean Central Volcanic Zone (CVZ).
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噴火履歴
詳細タイムライン
- 1995年VEI 2観測記録1995-09-01 ~ 1995-09-26
- 1989年VEI ?地質学的推定1989-12-16 ~ 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。