ソコンパ山
Socompa
成層火山 · Chile-Argentina · 6031m

- タイプ
- 成層火山
- 国
- Chile-Argentina
- 地域
- South America Volcanic Regions / Central Andean Volcanic Arc
- 標高
- 6031m
- 座標
- -24.396, -68.246
- 最終噴火
- -5250年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Dacite
地質学的概要
Straddling the Chile-Argentina border, Volcán Socompa is a massive dacitic stratovolcano that lies immediately north of the only railway line between the two countries. It is the youngest and southernmost of a NE-SW-trending chain of volcanoes including Pular and Pajonales. In contrast to the latter two volcanoes, no glacial moraines have been observed on the relatively uneroded Socompa. Collapse of the NW portion of the volcano about 7200 years ago produced a 600 km2 debris-avalanche deposit that extends about 40 km from the summit and is one of the world's largest and best exposed. Undated post-collapse eruptions constructed dacitic lava domes that have filled much of the head of the collapse scarp. No historical eruptions are known.
Wikipedia の要約
英語版の要約Socompa is a large stratovolcano on the border of Argentina and Chile. It has an elevation of 6,051 metres (19,852 ft) and is part of the Chilean and Argentine Andean Volcanic Belt (AVB). Socompa is within the Central Volcanic Zone, one of the segments of the AVB, which contains about 44 active volcanoes. It begins in Peru and runs first through Bolivia and Chile, and then Argentina and Chile. Socompa lies close to the pass of the same name where the Salta-Antofagasta railway crosses the Chilean border.
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噴火履歴
詳細タイムライン
- 紀元前 5250年VEI ?地質学的推定BCE 5250 ~ 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。