Mount Bandai
Bandaisan
Stratovolcano · Japan · 1816m

- Type
- Stratovolcano
- Country
- Japan
- Region
- Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
- Elevation
- 1816m
- Coordinates
- 37.601, 140.072
- Last eruption
- 1888
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
One of Japan's most noted volcanoes, Bandaisan rises above the north shore of Lake Inawashiro. This complex is formed of several overlapping andesitic stratovolcanoes, the largest of which is Obandai. Kobandaisan peak, which collapsed in 1888, was formed about 50,000 years ago. Obandai was constructed about 40,000 years ago after a Plinian eruption resulted in the collapse of an older edifice and the Okinajima debris avalanche to the SW. The last magmatic eruption took place more than 25,000 years ago, but four major phreatic eruptions have occurred during the past 5,000 years, most recently in 806 and 1888 CE. Seen from the south, Bandaisan presents a conical profile, but much of the north side of the volcano is missing as a result of the collapse of Kobandaisan during the 1888 eruption, causing a debris avalanche that buried several villages and formed several large lakes.
From Wikipedia
Mount Bandai is a stratovolcano located in Inawashiro-town, Bandai-town, and Kitashiobara village, in Yama-Gun, Fukushima prefecture. It is an active stratovolcano located to the north of Lake Inawashiro. Mount Bandai, including the Bandai heights, belongs to the Bandai-Asahi National Park.
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Eruption history
Detailed timeline
- 1888VEI 4Observed1888-07-15 – 1888-07-15Kobandai
- 1808VEI 2Observed1808 – OngoingNumanotaira
- 1787VEI 2Observed1787 – Ongoing
- 1767 (±16 yrs)VEI ?Geological estimate1767 – OngoingMt. Hanzawa (Bandai foothills)
- 1719VEI ?Geological estimate1719 – Ongoing
- 1611VEI ?Geological estimate1611 – Ongoing
- 806VEI 3Observed806 – OngoingO-Bandai
- 550 BCEVEI ?Geological estimateBCE 550 – OngoingNumanotaira
- 1800 BCE (±1250 yrs)VEI ?Geological estimateBCE 1800 – OngoingNumanotaira
- 3850 BCEVEI ?Geological estimateBCE 3850 – Ongoing
- 4650 BCEVEI ?Geological estimateBCE 4650 – Ongoing
- 5050 BCEVEI ?Geological estimateBCE 5050 – Ongoing
- 6350 BCEVEI ?Geological estimateBCE 6350 – Ongoing
- 7450 BCEVEI ?Geological estimateBCE 7450 – Ongoing
External links
⚠ For reference only. Not for emergency response.