Hakkōda Mountains
Hakkodasan
Estratovolcán · Japan · 1584 m

- Tipo
- Estratovolcán
- País
- Japan
- Región
- Pacífico Noroccidental / Northeast Japan Volcanic Arc
- Altitud
- 1584 m
- Coordenadas
- 40.659, 140.877
- Última erupción
- 1550
- Contexto tectónico
- Subduction zone / Continental crust (> 25 km)
- Forma volcánica
- Composite
- Roca principal
- Andesite / Basaltic Andesite
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.
Historial de erupciones
Línea de tiempo detallada
- 1550 (±100 años)VEI 1Estimación geológica1550 – En cursoSW flank of O-dake (Jigoku-numa)
- 1340 (±75 años)VEI 1Estimación geológica1340 – En cursoSW flank of O-dake (Jigoku-numa)
- 450VEI 1Estimación geológica450 – En cursoO-dake
- 50 a. C.VEI 1Estimación geológicaBCE 50 – En cursoO-dake
- 1150 a. C.VEI 1Estimación geológicaBCE 1150 – En cursoO-dake
- 2250 a. C.VEI 3Estimación geológicaBCE 2250 – En cursoO-dake
- 2850 a. C.VEI 2Estimación geológicaBCE 2850 – En cursoO-dake
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.