Cordón del Azufre
Cordon del Azufre
複成火山 · Chile-Argentina · 5481m

- タイプ
- 複成火山
- 国
- Chile-Argentina
- 地域
- South America Volcanic Regions / Central Andean Volcanic Arc
- 標高
- 5481m
- 座標
- -25.336, -68.521
- 最終噴火
- 不明
- 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
Cordón del Azufre is a small volcanic complex straddling the Chile-Argentina border. The complex consists of a cluster of lava flows from vents on the NE side, wholly within Argentina, and a 5-km-long chain of vents along the border with Chile. An older andesitic-dacitic edifice with a 1.3-km-wide crater was mostly covered by younger Holocene andesitic lava flows. The youngest cone, 300-m-high Volcán la Moyra, was the source of fresh-looking blocky andesitic lava flows that descended 6 km into Chile and 3 km into Argentina.
Wikipedia の要約
英語版の要約Cordón del Azufre is an inactive complex volcano located in the Central Andes, at the border of Argentina and Chile. It consists of three stages of volcanic cones and associated lava flows, and its activity is a consequence of the subduction of the Nazca Plate underneath the South American Plate. North of it are the dormant volcano Lastarria and the actively uplifting Lazufre region.
Wikipedia · CC BY-SA · 記事全文を読む →
噴火履歴
詳細タイムライン
噴火記録はありません。
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。