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Mount Sanbe

Sanbesan

Estratovolcán · Japan · 1126 m

Sanbe is the SW-most Holocene volcano on the island of Honshu. Seen here from the S, the highest peak is called Osanbe. It is flanked by Mesanbe on the right, Kosanbe on the left, and Magosanbe in the center. Sanbe had a large explosive eruption about 3,700 years ago that originated from Taiheizan lava dome.
Sanbe is the SW-most Holocene volcano on the island of Honshu. Seen here from the S, the highest peak is called Osanbe. It is flanked by Mesanbe on the right, Kosanbe on the left, and Magosanbe in the center. Sanbe had a large explosive eruption about 3,700 years ago that originated from Taiheizan lava dome. · Foto: Photo by Yoshinobu Tatsu, 1998 (Shimane Prefectural Sanbe Shizenkan Nature Museum). · Wikimedia Commons
Tipo
Estratovolcán
País
Japan
Región
Western Pacific Volcanic Regions / Nankai Volcanic Arc
Altitud
1126 m
Coordenadas
35.141, 132.622
Última erupción
650
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Dacite
Resumen geológico

Sanbesan stratovolcano, near the northern coast of SW Honshu, has a summit cut by a small caldera about 1 km in diameter. The highest point on the dacitic-to-andesitic volcano is O-Sanbe, at the northern end of the complex. There have been several large explosive eruptions during the Pleistocene and one strong Holocene eruption from the Taiheizan lava dome about 3,700 years ago. This eruption was accompanied by pyroclastic flows that swept down the NE-to-SE flanks and traveled 9 km down the Hayamizu River to the SW. Younger, undated eruptions have also occurred (Machida and Arai, 1992).

Resumen de Wikipedia

Resumen en inglés

Mount Sanbe, also known as Sanbesan, is an active stratovolcano in Ōda, Shimane Prefecture. The highest peak, Osanbe, has an elevation of 1,126 m (3,694 ft). At the center of the volcano is a caldera 1 km (0.62 mi) across. The volcano's composition is mainly dacite and andesite.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
3550 BCE~3350 BCE · 1 erupciones · VEI máx. ?1950 BCE~1750 BCE · 1 erupciones · VEI máx. 4450~650 · 1 erupciones · VEI máx. ?3550 BCE2550 BCE1550 BCE550 BCE450

Línea de tiempo detallada

  1. 650 (±50 años)VEI ?Estimación geológica
    650 – En curso
  2. 1920 a. C.VEI 4Estimación geológica
    BCE 1920 – En curso
    Taihei-zan
  3. 3550 a. C. (±50 años)VEI ?Estimación geológica
    BCE 3550 – En curso

Enlaces externos

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