Mikurajima
Estratovolcán · Japan · 851 m

- Tipo
- Estratovolcán
- País
- Japan
- Región
- Northwestern Pacific Volcanic Regions / Izu Volcanic Arc
- Altitud
- 851 m
- Coordenadas
- 33.874, 139.602
- Última erupción
- -4100
- Contexto tectónico
- Subduction zone / Oceanic crust (< 15 km)
- Forma volcánica
- Composite
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
Mikurajima is a small steep-sided island located between the more well-known Miyakejima and Hachijojima volcanoes. Oyama forms the summit of the basaltic-to-andesitic island, which is surrounded by cliffs and dissected on the southern-to-eastern sides. The sparsely populated island consists of a large stratovolcano with lava domes on the SE side. Several small sea stacks are located immediately offshore. Growth of the stratovolcano took place until about 7,000 years ago, and the latest activity occurred about 6,000 years ago, when explosive eruptions and pyroclastic surges accompanied lava dome growth.
Resumen de Wikipedia
Resumen en inglésMikura-jima (御蔵島) is an inhabited volcanic Japanese island in the Pacific Ocean. The island is administered by Tōkyō Metropolis and is located approximately 200 kilometres (120 mi) south of Tokyo and 19 kilometres (12 mi) south-southeast of Miyakejima. It is one of the Izu Seven Islands group of the seven northern islands of the Izu archipelago. Mikurashima is administratively part of Mikurashima Village under Miyake Subprefecture of Tokyo Metropolis. As of 2009, the island's population was 351. Mikura-shima is also within the boundaries of the Fuji-Hakone-Izu National Park.
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Historial de erupciones
Línea de tiempo detallada
- 4100 a. C. (±100 años)VEI ?Estimación geológicaBCE 4100 – En cursoTsubunegamori & Yasukajigamori domes
- 5050 a. C.VEI ?Estimación geológicaBCE 5050 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.