Pululagua
Pululahua
Caldera · Ecuador · 3360 m

- Tipo
- Caldera
- Paese
- Ecuador
- Regione
- South America Volcanic Regions / Northern Andean Volcanic Arc
- Altitudine
- 3360 m
- Coordinate
- 0.046, -78.490
- Ultima eruzione
- 290
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Caldera
- Roccia principale
- Dacite
Sintesi geologica
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.
Sintesi da Wikipedia
Riassunto in inglesePululahua 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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Storia delle eruzioni
Cronologia dettagliata
- 290VEI ?Stima geologica290 – In corso
- 450 a.C. (±150 anni)VEI 4Stima geologicaBCE 450 – In corso
- 690 a.C. (±150 anni)VEI 5Stima geologicaBCE 690 – In corso
- 4800 a.C.VEI ?Stima geologicaBCE 4800 – In corso
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.