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Mount Bandai

Bandaisan

Stratovolkan · Japan · 1816 m

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. · Foto: Photo by Lee Siebert, 1988 (Smithsonian Institution). · Wikimedia Commons
Tipe
Stratovolkan
Negara
Japan
Wilayah
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
Ketinggian
1816 m
Koordinat
37.601, 140.072
Letusan terakhir
1888
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

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.

Ringkasan Wikipedia

Ringkasan Inggris

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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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
7450 BCE~7139 BCE · 1 letusan · VEI maks. ?6516 BCE~6205 BCE · 1 letusan · VEI maks. ?5271 BCE~4960 BCE · 1 letusan · VEI maks. ?4960 BCE~4649 BCE · 1 letusan · VEI maks. ?4026 BCE~3715 BCE · 1 letusan · VEI maks. ?1847 BCE~1536 BCE · 1 letusan · VEI maks. ?602 BCE~291 BCE · 1 letusan · VEI maks. ?643~954 · 1 letusan · VEI maks. 31577~1888 · 6 letusan · VEI maks. 47450 BCE5271 BCE2781 BCE602 BCE1577

Garis waktu rinci

  1. 1888VEI 4Teramati
    1888-07-15 – 1888-07-15
    Kobandai
  2. 1808VEI 2Teramati
    1808 – Berlangsung
    Numanotaira
  3. 1787VEI 2Teramati
    1787 – Berlangsung
  4. 1767 (±16 tahun)VEI ?Perkiraan geologi
    1767 – Berlangsung
    Mt. Hanzawa (Bandai foothills)
  5. 1719VEI ?Perkiraan geologi
    1719 – Berlangsung
  6. 1611VEI ?Perkiraan geologi
    1611 – Berlangsung
  7. 806VEI 3Teramati
    806 – Berlangsung
    O-Bandai
  8. 550 SMVEI ?Perkiraan geologi
    BCE 550 – Berlangsung
    Numanotaira
  9. 1800 SM (±1250 tahun)VEI ?Perkiraan geologi
    BCE 1800 – Berlangsung
    Numanotaira
  10. 3850 SMVEI ?Perkiraan geologi
    BCE 3850 – Berlangsung
  11. 4650 SMVEI ?Perkiraan geologi
    BCE 4650 – Berlangsung
  12. 5050 SMVEI ?Perkiraan geologi
    BCE 5050 – Berlangsung
  13. 6350 SMVEI ?Perkiraan geologi
    BCE 6350 – Berlangsung
  14. 7450 SMVEI ?Perkiraan geologi
    BCE 7450 – Berlangsung

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.