Pululahua
Kaldera · Ecuador · 3360 m

- Tipe
- Kaldera
- Negara
- Ecuador
- Wilayah
- South America Volcanic Regions / 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
Pululahua adalah gunung berapi tidak aktif di daerah utara Kanton Quito, Provinsi Pichincha, Ekuador. Gunung berapi ini berada di Cordillera Barat di Andes Ekuador utara, kira-kira di barat daya Mojanda dan di utara gunung berapi Casitahua. Kaldera Gunung Pululahua memiliki lebar sekitar 5 km.
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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.