Jepang · Stratovolkan
Mount Bandai
Bandaisan
- Tipe
- Stratovolkan
- Ketinggian
- 1816 m
- Letusan terakhir
- 1888

- Tipe
- Stratovolkan
- Negara
- Jepang
- Wilayah
- Pasifik Barat Laut / Northeast Japan Volcanic Arc
- Ketinggian
- 1816 m
- Koordinat
- 37.601, 140.072
- Letusan terakhir
- 1888
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Komposit
- Batuan utama
- Andesit / Andesit basaltik
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 InggrisMount 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
14 tercatatGlosariumGaris waktu rinci
- 1888VEI 4Teramati1888-07-15 – 1888-07-15Kobandai
- 1808VEI 2Teramati1808-07-02 – akhir tidak diketahuiNumanotaira
- 1787VEI 2Teramati1787 – akhir tidak diketahui
- 1767 (±16 tahun)VEI ?Metode tidak dinyatakan1767 – akhir tidak diketahuiMt. Hanzawa (Bandai foothills)
- 1719VEI ?Metode tidak dinyatakan1719 – akhir tidak diketahui
- 1611VEI ?Metode tidak dinyatakan1611 – akhir tidak diketahui
- 806VEI 3Teramati806 – akhir tidak diketahuiO-Bandai
- 550 SMVEI ?Perkiraan geologi550 SM – akhir tidak diketahuiNumanotaira
- 1800 SM (±1250 tahun)VEI ?Perkiraan geologi1800 SM – akhir tidak diketahuiNumanotaira
- 3850 SMVEI ?Perkiraan geologi3850 SM – akhir tidak diketahui
- 4650 SMVEI ?Perkiraan geologi4650 SM – akhir tidak diketahui
- 5050 SMVEI ?Perkiraan geologi5050 SM – akhir tidak diketahui
- 6350 SMVEI ?Perkiraan geologi6350 SM – akhir tidak diketahui
- 7450 SMVEI ?Perkiraan geologi7450 SM – akhir tidak diketahui
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