Jepang · Stratovolkan
Hakkōda Mountains
Hakkodasan
- Tipe
- Stratovolkan
- Ketinggian
- 1584 m
- Letusan terakhir
- 1550

- Tipe
- Stratovolkan
- Negara
- Jepang
- Wilayah
- Pasifik Barat Laut / Northeast Japan Volcanic Arc
- Ketinggian
- 1584 m
- Koordinat
- 40.659, 140.877
- Letusan terakhir
- 1550
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Komposit
- Batuan utama
- Andesit / Andesit basaltik
Ringkasan geologi
The Hakkodasan complex includes at least 17 stratovolcanoes and lava domes south of Mutsu Bay at the northern end of Honshu. The NE rim of an 8-km-wide Pleistocene caldera forms an arcuate ridge across a flat caldera-floor moat NE of the Hakkoda group volcanoes, which bury the SE caldera wall. A northern group of volcanoes, constructed within the caldera, appears to be younger. The craters at Hakkoda-Odake, Ido-dake, and Tsurugi-dake appear morphologically young. Akakuradake has a 1-km-wide explosion crater breached to the north. An active solfatara occurs at Idodake, and hot springs are found at several locations within the caldera. Three minor phreatic events from Jigokunuma on the SW flank of Odake volcano produced tephra radiocarbon dated to the 13th-17th centuries. Three soldiers on a training mission in July 1997 were killed on the lower N flank of Hakkoda when they slipped into a depression containing a high percentage of CO2 gas wiht a magmatic origin.
Ringkasan Wikipedia
Ringkasan InggrisThe Hakkōda Mountains are an active volcanic complex in south-central Aomori Prefecture, Japan, in Towada-Hachimantai National Park. Often called Mount Hakkōda or simply Hakkōda (八甲田), the mountains are collectively listed as one of the 100 Famous Japanese Mountains. Its highest peak, Mount Ōdake, lies 21.3 kilometers (13.2 mi) southeast of central Aomori and 28 kilometers (17 mi) west of central Towada and has an elevation of 1,585 meters (5,200 ft). The Hakkōda Mountains are a part of the Ōu Mountains which make up part of the Northeastern Japan Arc, a segment of the Pacific Ring of Fire. The volcanic complex consists of fourteen stratovolcanoes and lava domes arranged into two volcanic groups. The Northern Hakkōda Volcanic Group emerges from the rim of an 8-kilometer-wide (5.0 mi) caldera that dates back to the Pleistocene. The Southern Hakkōda Volcanic Group predates the caldera.
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Riwayat letusan
7 tercatatGlosariumGaris waktu rinci
- 1550 (±100 tahun)VEI 1Perkiraan geologi1550 – akhir tidak diketahuiSW flank of O-dake (Jigoku-numa)
- 1340 (±75 tahun)VEI 1Perkiraan geologi1340 – akhir tidak diketahuiSW flank of O-dake (Jigoku-numa)
- 450VEI 1Perkiraan geologi450 – akhir tidak diketahuiO-dake
- 50 SMVEI 1Perkiraan geologi50 SM – akhir tidak diketahuiO-dake
- 1150 SMVEI 1Perkiraan geologi1150 SM – akhir tidak diketahuiO-dake
- 2250 SMVEI 3Perkiraan geologi2250 SM – akhir tidak diketahuiO-dake
- 2850 SMVEI 2Perkiraan geologi2850 SM – akhir tidak diketahuiO-dake
Gunung api terdekat
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.