Skip to main content

Mount Sanbe

Sanbesan

Stratovolcano · Japan · 1126m

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. · Photo: Photo by Yoshinobu Tatsu, 1998 (Shimane Prefectural Sanbe Shizenkan Nature Museum). · Wikimedia Commons
Type
Stratovolcano
Country
Japan
Region
Western Pacific Volcanic Regions / Nankai Volcanic Arc
Elevation
1126m
Coordinates
35.141, 132.622
Last eruption
650
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Dacite
Geological summary

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).

From Wikipedia

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.

Wikipedia · CC BY-SA · Read full article

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
3550 BCE~3350 BCE · 1 eruptions · max VEI ?1950 BCE~1750 BCE · 1 eruptions · max VEI 4450~650 · 1 eruptions · max VEI ?3550 BCE2550 BCE1550 BCE550 BCE450

Detailed timeline

  1. 650 (±50 yrs)VEI ?Geological estimate
    650 – Ongoing
  2. 1920 BCEVEI 4Geological estimate
    BCE 1920 – Ongoing
    Taihei-zan
  3. 3550 BCE (±50 yrs)VEI ?Geological estimate
    BCE 3550 – Ongoing

External links

⚠ For reference only. Not for emergency response.