Green Mountain
Ascension
Estratovolcán · United Kingdom · 822 m

- Tipo
- Estratovolcán
- País
- United Kingdom
- Región
- Océano Atlántico / Central Mid-Atlantic Rift Volcanic Province
- Altitud
- 822 m
- Coordenadas
- -7.946, -14.367
- Última erupción
- 1508
- Contexto tectónico
- Rift zone / Oceanic crust (< 15 km)
- Forma volcánica
- Composite
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
Ascensión Island, just west of the Mid-Atlantic Ridge ~2,250 km E of the eastern-most point of Brazil, is the 12-km-diameter emergent summit of a stratovolcano that rises ~3,000 m above the seafloor. The isolated island has more than 100 youthful cones and lava domes, many aligned along two fissures. Basaltic rocks dominate on the island, but trachytic lava domes are also present, mostly on the eastern side. Two of the youngest lava flows were erupted from flank vents and reached the sea on the N and S coasts. Argon-Argon dating by Preece and others (2018) identified three eruptions within the past 2,000 years. No eruptive activity has occurred since it was visited on Ascensión Day in 1501 by the Portuguese navigator Joao da Nova.
Resumen de Wikipedia
Resumen en inglésGreen Mountain is a common name for "The Peak", the highest point and a stratovolcano on Ascension Island, which has gained some fame for claims that it is one of very few large-scale artificial forests. Green Mountain is ranked 38th by topographic isolation.
Wikipedia · CC BY-SA · Leer artículo completo →
Historial de erupciones
Línea de tiempo detallada
- 1508 (±180 años)VEI 0Estimación geológica1508 – En cursoSouth Sisters lava flow
- 1468 (±120 años)VEI 0Estimación geológica1468 – En cursoComfortless Cove lava flow
- 378 (±370 años)VEI 0Estimación geológica378 – En cursoDavidson lava flow
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.