Almolonga
成層火山 · Guatemala · 3173m

- タイプ
- 成層火山
- 国
- 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
詳細タイムライン
- 1818年VEI 2観測記録1818-01-16 ~ 1818-06-19East flank of Cerro Quemado
- 1765年VEI 2観測記録1765-10-24 ~ 1765-10-25Cerro Quemado
- 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。