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Mount Sanbe

Sanbesan

Stratovolkan · 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
Tipe
Stratovolkan
Negara
Japan
Wilayah
Western Pacific Volcanic Regions / Nankai Volcanic Arc
Ketinggian
1126 m
Koordinat
35.141, 132.622
Letusan terakhir
650
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Dacite
Ringkasan geologi

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).

Ringkasan Wikipedia

Ringkasan Inggris

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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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
3550 BCE~3350 BCE · 1 letusan · VEI maks. ?1950 BCE~1750 BCE · 1 letusan · VEI maks. 4450~650 · 1 letusan · VEI maks. ?3550 BCE2550 BCE1550 BCE550 BCE450

Garis waktu rinci

  1. 650 (±50 tahun)VEI ?Perkiraan geologi
    650 – Berlangsung
  2. 1920 SMVEI 4Perkiraan geologi
    BCE 1920 – Berlangsung
    Taihei-zan
  3. 3550 SM (±50 tahun)VEI ?Perkiraan geologi
    BCE 3550 – Berlangsung

Tautan eksternal

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