Furnas
Estratovolcán · Portugal · 805 m
- Tipo
- Estratovolcán
- País
- Portugal
- Región
- Océano Atlántico / Azores-Terceira Rift Volcanic Province
- Altitud
- 805 m
- Coordenadas
- 37.770, -25.320
- Última erupción
- 1630
- Contexto tectónico
- Rift zone / Oceanic crust (< 15 km)
- Forma volcánica
- Composite
- Roca principal
- Trachyte / Trachydacite
Resumen geológico
Furnas volcano lies at the eastern end of Sao Miguel Island, immediately west of the older Nordeste shield volcano and its Povoaçao caldera. There are at least two calderas, a younger one that is 6-km wide and a larger older one that is less topographically distinct. The eastern wall of the 500-m-deep Furnas caldera overlaps the western wall of the Nordeste Povoaçao caldera. Volcanic activity dates back about 100,000 years. At least 11 trachytic pumice layers, all erupted during the past 5000 years, post-date the caldera. The most prominent post-caldera feature is the Pico do Gaspar lava dome, east of the Lagoa das Furnas caldera lake. A zone of late-Pleistocene to Holocene basaltic-to-trachytic cinder cones and lava domes is located between Furnas and Agua de Pau volcanoes. Two historical eruptions have occurred, one sometime between 1439 and 1443 and the other in 1630. The latter was one of the largest Holocene explosive eruptions in the Azores and caused significant damage and fatalities.
Resumen de Wikipedia
Resumen en inglésFurnas is a civil parish in the municipality of Povoação on the island of São Miguel in the Portuguese Azores. The population in 2011 was 1,439, in an area of 34.43 km2. The parish is one of the largest in the island and in the Azores. It is located east of Lagoa and Ponta Delgada, west of Povoação and southeast of Ribeira Grande.
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Historial de erupciones
Línea de tiempo detallada
- 1630VEI 5Observado1630-09-03 – 1630-11-02South end of caldera (Pico da Areia)
- 1441 (±2 años)VEI 4Observado1441 – En cursoCenter of caldera (Gaspar)
- 1430 (±100 años)VEI 3Estimación geológica1430 – En cursoEast caldera floor
- 1170 (±100 años)VEI 4Estimación geológica1170 – En cursoE caldera floor (Lake crater)
- 840 (±100 años)VEI 4Estimación geológica840 – En cursoCenter of caldera (Gaspar)
- 80 (±100 años)VEI 5Estimación geológica80 – En cursoN floor of younger caldera
- 360 a. C. (±150 años)VEI ?Estimación geológicaBCE 360 – En curso
- 1670 a. C. (±1460 años)VEI ?Estimación geológicaBCE 1670 – En curso
- 4570 a. C.VEI ?Estimación geológicaBCE 4570 – En cursoEast rim of caldera (Pico do Canário)
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.