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Japón · Estratovolcán

Hakkōda Mountains

Hakkodasan

Tipo
Estratovolcán
Altitud
1584 m
Última erupción
1550
Hakkōda Mountains
Foto: Mccunicano · CC BY-SA 4.0 · Wikimedia Commons
Tipo
Estratovolcán
País
Japón
Región
Pacífico Noroccidental / Northeast Japan Volcanic Arc
Altitud
1584 m
Coordenadas
40.659, 140.877
Última erupción
1550
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Compuesto
Roca principal
Andesita / Andesita basáltica
Resumen geológico

The Hakkodasan complex includes at least 17 stratovolcanoes and lava domes south of Mutsu Bay at the northern end of Honshu. The NE rim of an 8-km-wide Pleistocene caldera forms an arcuate ridge across a flat caldera-floor moat NE of the Hakkoda group volcanoes, which bury the SE caldera wall. A northern group of volcanoes, constructed within the caldera, appears to be younger. The craters at Hakkoda-Odake, Ido-dake, and Tsurugi-dake appear morphologically young. Akakuradake has a 1-km-wide explosion crater breached to the north. An active solfatara occurs at Idodake, and hot springs are found at several locations within the caldera. Three minor phreatic events from Jigokunuma on the SW flank of Odake volcano produced tephra radiocarbon dated to the 13th-17th centuries. Three soldiers on a training mission in July 1997 were killed on the lower N flank of Hakkoda when they slipped into a depression containing a high percentage of CO2 gas wiht a magmatic origin.

Resumen de Wikipedia

Resumen en inglés

The Hakkōda Mountains are an active volcanic complex in south-central Aomori Prefecture, Japan, in Towada-Hachimantai National Park. Often called Mount Hakkōda or simply Hakkōda (八甲田), the mountains are collectively listed as one of the 100 Famous Japanese Mountains. Its highest peak, Mount Ōdake, lies 21.3 kilometers (13.2 mi) southeast of central Aomori and 28 kilometers (17 mi) west of central Towada and has an elevation of 1,585 meters (5,200 ft). The Hakkōda Mountains are a part of the Ōu Mountains which make up part of the Northeastern Japan Arc, a segment of the Pacific Ring of Fire. The volcanic complex consists of fourteen stratovolcanoes and lava domes arranged into two volcanic groups. The Northern Hakkōda Volcanic Group emerges from the rim of an 8-kilometer-wide (5.0 mi) caldera that dates back to the Pleistocene. The Southern Hakkōda Volcanic Group predates the caldera.

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Historial de erupciones

7 registradasGlosario
Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales · Usa las flechas para moverte entre barras y Enter para abrir
2850 a. C.~2650 a. C. · 1 erupciones · VEI máx. 22250 a. C.~2050 a. C. · 1 erupciones · VEI máx. 31250 a. C.~1050 a. C. · 1 erupciones · VEI máx. 150 a. C.~150 · 1 erupciones · VEI máx. 1350~550 · 1 erupciones · VEI máx. 11150~1350 · 1 erupciones · VEI máx. 11350~1550 · 1 erupciones · VEI máx. 12850 a. C.1850 a. C.650 a. C.3501350

Línea de tiempo detallada

  1. 1550 (±100 años)VEI 1Estimación geológica
    1550 – fin desconocido
    SW flank of O-dake (Jigoku-numa)
  2. 1340 (±75 años)VEI 1Estimación geológica
    1340 – fin desconocido
    SW flank of O-dake (Jigoku-numa)
  3. 450VEI 1Estimación geológica
    450 – fin desconocido
    O-dake
  4. 50 a. C.VEI 1Estimación geológica
    50 a. C. – fin desconocido
    O-dake
  5. 1150 a. C.VEI 1Estimación geológica
    1150 a. C. – fin desconocido
    O-dake
  6. 2250 a. C.VEI 3Estimación geológica
    2250 a. C. – fin desconocido
    O-dake
  7. 2850 a. C.VEI 2Estimación geológica
    2850 a. C. – fin desconocido
    O-dake

Volcanes cercanos

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.