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Jepang · Stratovolkan

Hakkōda Mountains

Hakkodasan

Tipe
Stratovolkan
Ketinggian
1584 m
Letusan terakhir
1550
Hakkōda Mountains
Foto: Mccunicano · CC BY-SA 4.0 · Wikimedia Commons
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 Inggris

The 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 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu · Gunakan tombol panah untuk berpindah batang, Enter untuk membuka
2850 SM~2650 SM · 1 letusan · VEI maks. 22250 SM~2050 SM · 1 letusan · VEI maks. 31250 SM~1050 SM · 1 letusan · VEI maks. 150 SM~150 · 1 letusan · VEI maks. 1350~550 · 1 letusan · VEI maks. 11150~1350 · 1 letusan · VEI maks. 11350~1550 · 1 letusan · VEI maks. 12850 SM1850 SM650 SM3501350

Garis waktu rinci

  1. 1550 (±100 tahun)VEI 1Perkiraan geologi
    1550 – akhir tidak diketahui
    SW flank of O-dake (Jigoku-numa)
  2. 1340 (±75 tahun)VEI 1Perkiraan geologi
    1340 – akhir tidak diketahui
    SW flank of O-dake (Jigoku-numa)
  3. 450VEI 1Perkiraan geologi
    450 – akhir tidak diketahui
    O-dake
  4. 50 SMVEI 1Perkiraan geologi
    50 SM – akhir tidak diketahui
    O-dake
  5. 1150 SMVEI 1Perkiraan geologi
    1150 SM – akhir tidak diketahui
    O-dake
  6. 2250 SMVEI 3Perkiraan geologi
    2250 SM – akhir tidak diketahui
    O-dake
  7. 2850 SMVEI 2Perkiraan geologi
    2850 SM – akhir tidak diketahui
    O-dake

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