Pululagua
Pululahua
カルデラ · Ecuador · 3360m

- タイプ
- カルデラ
- 国
- Ecuador
- 地域
- South America Volcanic Regions / Northern Andean Volcanic Arc
- 標高
- 3360m
- 座標
- 0.046, -78.490
- 最終噴火
- 290年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Caldera
- 主要岩石
- Dacite
地質学的概要
Pululahua is a relatively low, forested volcano about 15 km N of Quito. The 5-km-wide summit caldera is narrowly breached to the west and partially filled by a group of dacitic lava domes. Pre-caldera lava domes of different ages are found outside the caldera to the E, SE, and S. Four post-caldera domes rise up to 450 m above the caldera floor. Large explosive eruptions producing pyroclastic flows took place during the late Pleistocene and Holocene. Caldera formation took place during a series of eruptions lasting 150-200 years beginning about 2,650 radiocarbon years ago. The latest dated eruption occurred from the post-caldera lava domes about 1,670 years ago and produced lava flows and pyroclastic flows.
Wikipedia の要約
英語版の要約Pululahua is a dormant volcano in the north of Quito Canton, Pichincha Province, Ecuador. The volcano is in the Western Cordillera of the northern Ecuadorian Andes, approximately west-southwest of Mojanda and north of Casitahua volcanoes. Pululahua's caldera is approximately 5 km wide.The volcano is within an Ecuadorian national park known as Reserva Geobotánica Pululahua.
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噴火履歴
詳細タイムライン
- 290年VEI ?地質学的推定290 ~ 進行中
- 紀元前 450年 (±150年)VEI 4地質学的推定BCE 450 ~ 進行中
- 紀元前 690年 (±150年)VEI 5地質学的推定BCE 690 ~ 進行中
- 紀元前 4800年VEI ?地質学的推定BCE 4800 ~ 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。