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Almolonga

成層火山 · Guatemala · 3173m

The rounded hills in the middle of the photo are part of a chain of lava domes of the Almolonga volcanic field. Partial flank collapse of an edifice sometime prior to 84,000 years ago formed a 3.3-km-wide collapse scarp that is surrounded by a ring-dike configuration of dacite and rhyolite lava domes, seen here from the east. Cerro Quemado is a young dome near the center of the horizon, right of the larger Santa María, that produced a 2.5-km-long lava flow on its eastern flank in 1818.
The rounded hills in the middle of the photo are part of a chain of lava domes of the Almolonga volcanic field. Partial flank collapse of an edifice sometime prior to 84,000 years ago formed a 3.3-km-wide collapse scarp that is surrounded by a ring-dike configuration of dacite and rhyolite lava domes, seen here from the east. Cerro Quemado is a young dome near the center of the horizon, right of the larger Santa María, that produced a 2.5-km-long lava flow on its eastern flank in 1818. · 写真: Photo by Lee Siebert, 1988 (Smithsonian Institution). · Wikimedia Commons
タイプ
成層火山
Guatemala
地域
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
標高
3173m
座標
14.797, -91.519
最終噴火
1818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

Volcán de Almolonga is an andesitic stratovolcano with a 3.3-km-wide late-Pleistocene central caldera that is located along the Zunil fault zone. The caldera is surrounded by a ring-dike configuration of dacitic and rhyolitic lava domes. The youngest and only historically active dome complex is Cerro Quemado (whose name means Burned Peak), located immediately south of Guatemala's second largest city, Quezaltenango. About 1200 radiocarbon years ago, part of the andesitic-to-dacitic Cerro Quemado dome collapsed, producing a debris avalanche and an associated lateral explosion that swept across the valley to the west as far as the flanks of Siete Orejas volcano. The latest eruption in 1818 produced a blocky 2.5-km-long lava flow. Hot springs are located on the northern and eastern flanks of Cerro Quemado, and the Zuníl geothermal field, the site of a geothermal exploration project, lies on the SE flank of Cerro Quemado.

噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
800~902 · 1件 · 最大 VEI 31716~1818 · 2件 · 最大 VEI 28001004130915131716

詳細タイムライン

  1. 1818年VEI 2観測記録
    1818-01-16 ~ 1818-06-19
    East flank of Cerro Quemado
  2. 1765年VEI 2観測記録
    1765-10-24 ~ 1765-10-25
    Cerro Quemado
  3. 800年 (±50年)VEI 3地質学的推定
    800 ~ 進行中
    Cerro Quemado

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。