Portugal · Stratovolcano
Sete Cidades Massif
Sete Cidades
- Type
- Stratovolcano
- Elevation
- 842m
- Last eruption
- 1880
- Type
- Stratovolcano
- Country
- Portugal
- Region
- Atlantic Ocean / Azores-Terceira Rift Volcanic Province
- Elevation
- 842m
- Coordinates
- 37.865, -25.785
- Last eruption
- 1880
- Tectonic setting
- Rift zone / Oceanic crust (< 15 km)
- Landform
- Composite
- Major rock type
- Trachyte / Trachydacite
Geological summary
Sete Cidades volcano at the western end of Sao Miguel Island contains a 5-km-wide summit caldera occupied by two caldera lakes. The steep-walled, 500-m-deep caldera was formed about 22,000 years ago, and at least 22 post-caldera eruptions have occurred. A large group of Pleistocene post-caldera trachytic lava domes, lava flows, and pyroclastic-flow deposits is found on the western-to-northern flanks. A nearly circular ring of six Holocene pyroclastic cones on the caldera floor have been the source of a dozen trachytic pumice-fall deposits erupted during the past 5,000 years. Recorded eruptions date back to the 15th century and have occurred both within the caldera and from submarine vents off the west coast.
From Wikipedia
Sete Cidades Massif is a stratovolcanic complex, referring to a polygenetic volcano and caldera, located in western part of the island of São Miguel, in the Portuguese archipelago of the Azores. More recognizable for the Lagoa das Sete Cidades at its centre, the volcanic complex includes centuries of geomorphological structures that include lava domes, cones, lava flows and maar geomorphology that have marked its history.
Wikipedia · CC BY-SA · Read full article →
Eruption history
16 recordedGlossaryDetailed timeline
- 1880VEI 0Method not stated1880-07-02 – end unknownVolcano Uncertain: submarine vent off Sao Miguel
- 1861VEI 0Method not stated1861-07-02 – end unknownVolcano Uncertain: submarine vent off Sao Miguel
- 1811VEI 2Observed1811-02-01 – 1811-02-08Submarine vent west of Sete Cidades
- 1811VEI 3Observed1811-06-14 – 1811-06-22Submarine vent west of Sete Cidades
- 1713VEI 2Observed1713 – end unknownWest flank (Pico das Camarinhas)
- 1682VEI 2Observed1682-12-13 – end unknownSubmarine vent west of Sete Cidades
- 1638VEI 2Observed1638-07-03 – 1638-07-28Submarine vent west of Sete Cidades
- 1444VEI 4Observed1444 – end unknownSW side of caldera (Caldeira Seca)
- 1110 (±50 yrs)VEI 2Geological estimate1110 – end unknownWest flank (Ponta de Ferraria)
- 950 (±100 yrs)VEI 2Geological estimate950 – end unknownSE flank (Ferraria)
- 670 (±150 yrs)VEI 3Geological estimate670 – end unknownSE flank (Carvao)
- 380 (±300 yrs)VEI 4Geological estimate380 – end unknownSE caldera floor (Lagoa Rasa)
- 90 (±100 yrs)VEI 4Geological estimate90 – end unknownSE caldera floor (Lagoa de Santiago)
- 750 BCE (±300 yrs)VEI ?Geological estimate750 BCE – end unknownSE flank (Eguas)
- 2050 BCE (±1000 yrs)VEI ?Geological estimate2050 BCE – end unknownCaldeira do Alfreres and NW flank
- 3050 BCEVEI 4Geological estimate3050 BCE – end unknownSeara Cerrado da Ladeira
Nearby volcanoes
External links
⚠ For reference only. Not for emergency response.