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Mount Sanbe

Sanbesan

Stratovulcano · 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
Stratovulcano
Paese
Japan
Regione
Western Pacific Volcanic Regions / Nankai Volcanic Arc
Altitudine
1126 m
Coordinate
35.141, 132.622
Ultima eruzione
650
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Dacite
Sintesi geologica

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).

Sintesi da Wikipedia

Riassunto in inglese

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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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
3550 BCE~3350 BCE · 1 eruzioni · VEI max. ?1950 BCE~1750 BCE · 1 eruzioni · VEI max. 4450~650 · 1 eruzioni · VEI max. ?3550 BCE2550 BCE1550 BCE550 BCE450

Cronologia dettagliata

  1. 650 (±50 anni)VEI ?Stima geologica
    650 – In corso
  2. 1920 a.C.VEI 4Stima geologica
    BCE 1920 – In corso
    Taihei-zan
  3. 3550 a.C. (±50 anni)VEI ?Stima geologica
    BCE 3550 – In corso

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.