Pululahua
Kaldera · Ecuador · 3360 m

- Tipe
- Kaldera
- Negara
- Ecuador
- Wilayah
- Amerika Selatan / Northern Andean Volcanic Arc
- Ketinggian
- 3360 m
- Koordinat
- 0.046, -78.490
- Letusan terakhir
- 290
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Caldera
- Batuan utama
- Dacite
Ringkasan geologi
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.
Ringkasan Wikipedia
Ringkasan InggrisPululahua 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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Riwayat letusan
Garis waktu rinci
- 290VEI ?Perkiraan geologi290 – Berlangsung
- 450 SM (±150 tahun)VEI 4Perkiraan geologiBCE 450 – Berlangsung
- 690 SM (±150 tahun)VEI 5Perkiraan geologiBCE 690 – Berlangsung
- 4800 SMVEI ?Perkiraan geologiBCE 4800 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.