八甲田山
Hakkodasan
成層火山 · Japan · 1584m

- タイプ
- 成層火山
- 国
- Japan
- 地域
- 北西太平洋 / Northeast Japan Volcanic Arc
- 標高
- 1584m
- 座標
- 40.659, 140.877
- 最終噴火
- 1550年
- テクトニクス環境
- Subduction zone / Continental crust (> 25 km)
- 火山地形
- Composite
- 主要岩石
- Andesite / Basaltic Andesite
地質学的概要
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.
噴火履歴
詳細タイムライン
- 1550年 (±100年)VEI 1地質学的推定1550 ~ 進行中SW flank of O-dake (Jigoku-numa)
- 1340年 (±75年)VEI 1地質学的推定1340 ~ 進行中SW flank of O-dake (Jigoku-numa)
- 450年VEI 1地質学的推定450 ~ 進行中O-dake
- 紀元前 50年VEI 1地質学的推定BCE 50 ~ 進行中O-dake
- 紀元前 1150年VEI 1地質学的推定BCE 1150 ~ 進行中O-dake
- 紀元前 2250年VEI 3地質学的推定BCE 2250 ~ 進行中O-dake
- 紀元前 2850年VEI 2地質学的推定BCE 2850 ~ 進行中O-dake
外部リンク
⚠ 参考情報です。緊急対応には使用しないでください。