Portugal · Stratovolcano
Terceira Island
Terceira
- Type
- Stratovolcano
- Elevation
- 1023m
- Last eruption
- 2000

- Type
- Stratovolcano
- Country
- Portugal
- Region
- Atlantic Ocean / Azores-Terceira Rift Volcanic Province
- Elevation
- 1023m
- Coordinates
- 38.730, -27.320
- Last eruption
- 2000
- Tectonic setting
- Rift zone / Oceanic crust (< 15 km)
- Landform
- Composite
- Major rock type
- Basalt / Picro-basalt
Geological summary
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.
From Wikipedia
Terceira is a volcanic island in the Azores archipelago of Portugal, 1,181 km (734 mi) due west of Lisbon. It is one of the larger islands of the archipelago, with a population of 53,311 inhabitants in an area of approximately 396.75 km2 (153.19 sq mi).
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Eruption history
15 recordedGlossaryDetailed timeline
- 1998VEI 0Observed1998-11-25 – 2000-03-16Serreta Ridge (submarine vent W of Terceira)
- 1867VEI 3Observed1867-06-01 – 1867-06-08Submarine vent 3-6 WNW of Terceira
- 1761VEI 2Observed1761-04-17 – 1761-04-28Fissure zone (east of Santa Barbara)
- 1400 (±50 yrs)VEI ?Geological estimate1400 – end unknownFarol I dome (Santa Barbara)
- 1200 (±300 yrs)VEI ?Geological estimate1200 – end unknownGuilherme Moniz (Pico Alto)
- 920 (±50 yrs)VEI ?Geological estimate920 – end unknownGuilherme Moniz (Quinta da Madalena)
- 820 (±40 yrs)VEI ?Geological estimate820 – end unknownSanta Barbara
- 190 (±40 yrs)VEI ?Geological estimate190 – end unknownGuilherme Moniz (Pico Alto)
- 70 (±40 yrs)VEI ?Geological estimate70 – end unknownFissure zone (east of Santa Barbara)
- 60 BCEVEI ?Geological estimate60 BCE – end unknownFissure zone (south of Pico Alto)
- 90 BCE (±100 yrs)VEI ?Geological estimate90 BCE – end unknownFissure zone (east of Santa Barbara)
- 670 BCE (±300 yrs)VEI ?Geological estimate670 BCE – end unknownGuilherme Moniz
- 940 BCE (±50 yrs)VEI ?Geological estimate940 BCE – end unknownSanta Barbara NW flank (Lagoinha dome)
- 2530 BCE (±40 yrs)VEI ?Geological estimate2530 BCE – end unknownFissure zone (east of Santa Barbara)
- 6720 BCE (±50 yrs)VEI ?Geological estimate6720 BCE – end unknownGuilherme Moniz (Pico das Pardelas)
Nearby volcanoes
External links
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