Pululagua
Pululahua
Caldera · Ecuador · 3360m

- Type
- Caldera
- Country
- Ecuador
- Region
- South America Volcanic Regions / Northern Andean Volcanic Arc
- Elevation
- 3360m
- Coordinates
- 0.046, -78.490
- Last eruption
- 290
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Caldera
- Major rock type
- Dacite
Geological summary
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.
From Wikipedia
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.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
- 290VEI ?Geological estimate290 – Ongoing
- 450 BCE (±150 yrs)VEI 4Geological estimateBCE 450 – Ongoing
- 690 BCE (±150 yrs)VEI 5Geological estimateBCE 690 – Ongoing
- 4800 BCEVEI ?Geological estimateBCE 4800 – Ongoing
External links
⚠ For reference only. Not for emergency response.