Isla Graciosa
Graciosa
Estratovolcán · Portugal · 402 m

- Tipo
- Estratovolcán
- País
- Portugal
- Región
- Océano Atlántico / Azores-Terceira Rift Volcanic Province
- Altitud
- 402 m
- Coordenadas
- 39.020, -27.970
- Última erupción
- -1950
- Contexto tectónico
- Rift zone / Oceanic crust (< 15 km)
- Forma volcánica
- Composite
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
The SE end of Graciosa, the northernmost of the central Azorean islands, contains a 0.9 x 1.6 km caldera with active fumaroles. The SE caldera rim is the high point of the 7 x 12 km island. The caldera has been the source of eruptions producing significant tephra falls, pyroclastic flows, lahars, and lava flows. Fumaroles are present in a volcanic cave inside the caldera, and a submarine fumarole occurs off the NW coast. Scoria cones erupted along several widely spaced NE-SW-trending fissures fed a youthful lava field that forms the NW end of the island. The most recent eruption from Pico Tomao, NW of the caldera, produced a lava flow during the mid-to-late Holocene that reached the eastern coast NW of the village of Praia.
Resumen de Wikipedia
Resumen en inglésGraciosa Island, also referred to as the White Island, is a volcanic island in the Atlantic Ocean. It is the northernmost of the Central Group of islands in the Azores archipelago. The ovular Portuguese island has an area of 60.65 square kilometres, a length of 10 kilometres and a width of 7 kilometres. Its landscape is dominated by a 1.6-kilometre-wide (1.0-mile) central caldera located in the southeast.
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Historial de erupciones
Línea de tiempo detallada
- 1950 a. C. (±1400 años)VEI ?Estimación geológicaBCE 1950 – En cursoSan Tamao
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.