Terceira
Stratovolkan · Portugal · 1023 m

- Tipe
- Stratovolkan
- Negara
- Portugal
- Wilayah
- Atlantic Ocean Volcanic Regions / Azores-Terceira Rift Volcanic Province
- Ketinggian
- 1023 m
- Koordinat
- 38.730, -27.320
- Letusan terakhir
- 2000
- Kondisi tektonik
- Rift zone / Oceanic crust (< 15 km)
- Bentuk lahan
- Composite
- Batuan utama
- Basalt / Picro-Basalt
Ringkasan geologi
Terceira Island contains multiple stratovolcanoes constructed along a prominent ESE-WNW fissure zone that cuts across the island. Historically active Santa Barbara volcano at the western end of the island is truncated by two calderas, the youngest of which formed about 15,000 years ago. Comenditic lava domes fill and surround the caldera. Pico Alto lies north of the fissure zone in the north-central part of the island and contains a Pleistocene caldera largely filled by lava domes and lava flows. Guilherme Moniz caldera lies along the fissure zone immediately to the south, and 7-km-wide Cinquio Picos caldera is at the SE end of the island. Historical eruptions have occurred from Pico Alto, the fissure zone between Pico Alto and Santa Barbara, and from submarine vents west of Santa Barbara. Most Holocene eruptions have produced basaltic-to-rhyolitic lava flows from the fissure zone.
Ringkasan Wikipedia
Terceira adalah sebuah pulau di Portugal. Pulau ini merupakan bagian dari kepulauan Azores. Tepatnya di bagian Samudra Atlantik utara. Pada tahun 2011, pulau ini memiliki jumlah penduduk sebesar 56.437 jiwa dan memiliki luas wilayah 400,6 km².
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
Garis waktu rinci
- 1998VEI 0Teramati1998-11-25 – 2000-03-16Serreta Ridge (submarine vent W of Terceira)
- 1867VEI 3Teramati1867-06-01 – 1867-06-08Submarine vent 3-6 WNW of Terceira
- 1761VEI 2Teramati1761-04-17 – 1761-04-28Fissure zone (east of Santa Barbara)
- 1400 (±50 tahun)VEI ?Perkiraan geologi1400 – BerlangsungFarol I dome (Santa Barbara)
- 1200 (±300 tahun)VEI ?Perkiraan geologi1200 – BerlangsungGuilherme Moniz (Pico Alto)
- 920 (±50 tahun)VEI ?Perkiraan geologi920 – BerlangsungGuilherme Moniz (Quinta da Madalena)
- 820 (±40 tahun)VEI ?Perkiraan geologi820 – BerlangsungSanta Barbara
- 190 (±40 tahun)VEI ?Perkiraan geologi190 – BerlangsungGuilherme Moniz (Pico Alto)
- 70 (±40 tahun)VEI ?Perkiraan geologi70 – BerlangsungFissure zone (east of Santa Barbara)
- 60 SMVEI ?Perkiraan geologiBCE 60 – BerlangsungFissure zone (south of Pico Alto)
- 90 SM (±100 tahun)VEI ?Perkiraan geologiBCE 90 – BerlangsungFissure zone (east of Santa Barbara)
- 670 SM (±300 tahun)VEI ?Perkiraan geologiBCE 670 – BerlangsungGuilherme Moniz
- 940 SM (±50 tahun)VEI ?Perkiraan geologiBCE 940 – BerlangsungSanta Barbara NW flank (Lagoinha dome)
- 2530 SM (±40 tahun)VEI ?Perkiraan geologiBCE 2530 – BerlangsungFissure zone (east of Santa Barbara)
- 6720 SM (±50 tahun)VEI ?Perkiraan geologiBCE 6720 – BerlangsungGuilherme Moniz (Pico das Pardelas)
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.