Hachijōjima
Hachijojima
Estratovolcán · Japan · 854 m

- Tipo
- Estratovolcán
- País
- Japan
- Región
- Northwestern Pacific Volcanic Regions / Izu Volcanic Arc
- Altitud
- 854 m
- Coordenadas
- 33.137, 139.766
- Última erupción
- 1606
- Contexto tectónico
- Subduction zone / Oceanic crust (< 15 km)
- Forma volcánica
- Composite
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
Hachijojima, in the central Izu Islands about 300 km S of Tokyo, consists of two small Quaternary dominantly basaltic stratovolcanoes forming an elongated NW-SE-trending island. The eroded Pleistocene-to-Holocene Higashiyama volcano occupies the SE end of the 14-km-long island. The symmetrical Holocene Nishiyama volcano the NW end has cones on the SE flank. The small volcanic island of Kojima lies several kilometers W of Hachijojima. Growth of Higashiyama began several tens of thousands of years ago, and included the formation of two small calderas. The initial submarine and early subaerial eruptions of Nishiyama took place from 10,000 to 8,000 years before present (BP). Its latest major activity, from the early Holocene until about 4,000 BP, was restricted to flank eruptions. Eruptions recorded since the 15th century have been restricted to the summit of Nishiyama and a submarine vent of unknown location.
Resumen de Wikipedia
Resumen en inglésHachijō-jima is a volcanic island of Japan in the Pacific Ocean. It is about 287 km (178 mi) south of the special wards of Tokyo. It is part of the Izu archipelago and within the Fuji-Hakone-Izu National Park. Its only municipality is Hachijō. On 1 March 2018, its population was 7,522 people living on 63 km2. Some inhabitants speak Hachijō language, which is considered an endangered language and the number of speakers is unknown. The island has been inhabited since the Jōmon period, and was used as a place of exile during the Edo period. In modern times, it has been used for farming sugarcane and housing a secret submarine base during World War II; it is now a tourist destination within Japan.
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Historial de erupciones
Línea de tiempo detallada
- 1707VEI 2Estimación geológica1707 – En curso
- 1606VEI 2Observado1606-01-23 – En cursoSubmarine flank
- 1605VEI 2Observado1605-10-27 – En cursoNishi-yama SE flank
- 1518VEI 2Observado1518-02 – 1523Nishi-yama
- 1487VEI 2Observado1487-12-07 – En cursoNishi-yama
- 850 (±200 años)VEI ?Estimación geológica850 – En cursoNishi-yama summit and SE flank
- 150 a. C. (±50 años)VEI ?Estimación geológicaBCE 150 – En cursoNishi-yama
- 350 a. C. (±500 años)VEI 3Estimación geológicaBCE 350 – En cursoNW flank of Higashi-yama
- 1150 a. C. (±700 años)VEI ?Estimación geológicaBCE 1150 – En cursoSE flank of Nishi-yama (Kanda-yama)
- 1250 a. C. (±800 años)VEI ?Estimación geológicaBCE 1250 – En cursoNishi-yama
- 2050 a. C.VEI 5Estimación geológicaBCE 2050 – En cursoSE of Nishi-yama, NE of Higashi-yama
- 2450 a. C. (±500 años)VEI 4Estimación geológicaBCE 2450 – En cursoNishi-yama
- 2550 a. C. (±500 años)VEI 3Estimación geológicaBCE 2550 – En cursoS flank of Higashi-yama (Myohoji)
- 2700 a. C. (±100 años)VEI 3Estimación geológicaBCE 2700 – En cursoBetween Nishi-yama & Higashi-yama
- 3350 a. C. (±1300 años)VEI ?Estimación geológicaBCE 3350 – En cursoNishi-yama
- 4650 a. C.VEI 5Estimación geológicaBCE 4650 – En cursoNishi-yama
- 5020 a. C. (±370 años)VEI 3Estimación geológicaBCE 5020 – En cursoHigashi-yama south flank
- 7650 a. C. (±3000 años)VEI ?Estimación geológicaBCE 7650 – En cursoNishi-yama
- 8020 a. C. (±2640 años)VEI 4Estimación geológicaBCE 8020 – En cursoNishi-yama
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.