Japón · Estratovolcán
Hakkōda Mountains
Hakkodasan
- Tipo
- Estratovolcán
- Altitud
- 1584 m
- Última erupción
- 1550

- 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 inglésThe 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 registradasGlosarioLínea de tiempo detallada
- 1550 (±100 años)VEI 1Estimación geológica1550 – fin desconocidoSW flank of O-dake (Jigoku-numa)
- 1340 (±75 años)VEI 1Estimación geológica1340 – fin desconocidoSW flank of O-dake (Jigoku-numa)
- 450VEI 1Estimación geológica450 – fin desconocidoO-dake
- 50 a. C.VEI 1Estimación geológica50 a. C. – fin desconocidoO-dake
- 1150 a. C.VEI 1Estimación geológica1150 a. C. – fin desconocidoO-dake
- 2250 a. C.VEI 3Estimación geológica2250 a. C. – fin desconocidoO-dake
- 2850 a. C.VEI 2Estimación geológica2850 a. C. – fin desconocidoO-dake
Volcanes cercanos
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.