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Mount Bandai

Bandaisan

Stratovolcano · Japan · 1816m

Akahaniyama to the right is one of several cones that form Bandaisan, seen here above rice fields N of Lake Inawashiro. The forested ridge in the left foreground is part of an earlier Pleistocene debris avalanche deposit.
Akahaniyama to the right is one of several cones that form Bandaisan, seen here above rice fields N of Lake Inawashiro. The forested ridge in the left foreground is part of an earlier Pleistocene debris avalanche deposit. · Photo: Photo by Lee Siebert, 1988 (Smithsonian Institution). · Wikimedia Commons
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.

Wikipedia · CC BY-SA · Read full article

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
7450 BCE~7139 BCE · 1 eruptions · max VEI ?6516 BCE~6205 BCE · 1 eruptions · max VEI ?5271 BCE~4960 BCE · 1 eruptions · max VEI ?4960 BCE~4649 BCE · 1 eruptions · max VEI ?4026 BCE~3715 BCE · 1 eruptions · max VEI ?1847 BCE~1536 BCE · 1 eruptions · max VEI ?602 BCE~291 BCE · 1 eruptions · max VEI ?643~954 · 1 eruptions · max VEI 31577~1888 · 6 eruptions · max VEI 47450 BCE5271 BCE2781 BCE602 BCE1577

Detailed timeline

  1. 1888VEI 4Observed
    1888-07-15 – 1888-07-15
    Kobandai
  2. 1808VEI 2Observed
    1808 – Ongoing
    Numanotaira
  3. 1787VEI 2Observed
    1787 – Ongoing
  4. 1767 (±16 yrs)VEI ?Geological estimate
    1767 – Ongoing
    Mt. Hanzawa (Bandai foothills)
  5. 1719VEI ?Geological estimate
    1719 – Ongoing
  6. 1611VEI ?Geological estimate
    1611 – Ongoing
  7. 806VEI 3Observed
    806 – Ongoing
    O-Bandai
  8. 550 BCEVEI ?Geological estimate
    BCE 550 – Ongoing
    Numanotaira
  9. 1800 BCE (±1250 yrs)VEI ?Geological estimate
    BCE 1800 – Ongoing
    Numanotaira
  10. 3850 BCEVEI ?Geological estimate
    BCE 3850 – Ongoing
  11. 4650 BCEVEI ?Geological estimate
    BCE 4650 – Ongoing
  12. 5050 BCEVEI ?Geological estimate
    BCE 5050 – Ongoing
  13. 6350 BCEVEI ?Geological estimate
    BCE 6350 – Ongoing
  14. 7450 BCEVEI ?Geological estimate
    BCE 7450 – Ongoing

External links

⚠ For reference only. Not for emergency response.