Antillanca Group
Antillanca Volcanic Complex
成層火山 · Chile · 1979m

- タイプ
- 成層火山
- 国
- Chile
- 地域
- South America Volcanic Regions / Southern Andean Volcanic Arc
- 標高
- 1979m
- 座標
- -40.783, -72.150
- 最終噴火
- -230年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
The Antillanca Volcanic Complex is a cluster of late-Pleistocene to Holocene basaltic-to-andesitic scoria cones, maars, and small stratovolcanoes covering an area of 380 km2 SE of Lago Puyehue and NE of Lago Rupanco. The most prominent edifice is the Holocene Casablanca stratovolcano, which has a truncated conical profile and produced major explosive eruptions about 2,910 and 2,260 radiocarbon years ago. Older late-Pleistocene stratovolcanoes, such as Sarnoso to the SW and Fiuchá to the NW, are extensively dissected by glaciers. Fissures oriented in four major directions influence the orientation of the cones. Thermal areas are found in scattered locations on the NW side of the complex.
Wikipedia の要約
英語版の要約The Antillanca Group is a volcanic group of scoria cones, maars and small stratovolcanoes, in Chile. Casablanca stratovolcano is the tallest volcano of the group, which shelters the Antillanca ski resort on its west flank. Aguas Calientes and Puyehue Hot springs also form part of this volcanic group. The complex encompasses 380 km2 and to the west is bordered by the lakes Puyehue and Rupanco.
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噴火履歴
詳細タイムライン
- 紀元前 230年 (±200年)VEI 5地質学的推定BCE 230 ~ 進行中Casablanca (Raihuén crater)
- 紀元前 960年 (±150年)VEI 5地質学的推定BCE 960 ~ 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。