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Pululagua

Pululahua

Caldera · Ecuador · 3360m

Pululahua is a relatively low-profile, forested volcano immediately north of the equator, 27 km N of Quito. Loma Pondona (left) and the lower Rumiloma (right center) are two of a group of lava domes that partially fill a 3-km-wide caldera. They are seen here from the SE caldera rim. The caldera was formed during the latest dated eruption about 2,400 years ago. Large explosive eruptions were accompanied by pyroclastic flows during the late Pleistocene and Holocene.
Pululahua is a relatively low-profile, forested volcano immediately north of the equator, 27 km N of Quito. Loma Pondona (left) and the lower Rumiloma (right center) are two of a group of lava domes that partially fill a 3-km-wide caldera. They are seen here from the SE caldera rim. The caldera was formed during the latest dated eruption about 2,400 years ago. Large explosive eruptions were accompanied by pyroclastic flows during the late Pleistocene and Holocene. · Photo: Photo by Lee Siebert, 1978 (Smithsonian Institution). · Wikimedia Commons
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

Summary (VEI over time)
Click a bar to see individual eruptions
4800 BCE~4604 BCE · 1 eruptions · max VEI ?885 BCE~689 BCE · 1 eruptions · max VEI 5493 BCE~297 BCE · 1 eruptions · max VEI 494~290 · 1 eruptions · max VEI ?4800 BCE3625 BCE2255 BCE1080 BCE94

Detailed timeline

  1. 290VEI ?Geological estimate
    290 – Ongoing
  2. 450 BCE (±150 yrs)VEI 4Geological estimate
    BCE 450 – Ongoing
  3. 690 BCE (±150 yrs)VEI 5Geological estimate
    BCE 690 – Ongoing
  4. 4800 BCEVEI ?Geological estimate
    BCE 4800 – Ongoing

External links

⚠ For reference only. Not for emergency response.