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八甲田山

Hakkodasan

成層火山 · Japan · 1585m

Hakkoda consists of a group of 14 cones 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 the caldera floor to the NE of the Hakkoda group volcanoes, which bury the SE caldera wall. This view looks from the W towards the northern Akakuradake, Idodake, and Hakkodasan volcanoes seen from left to right.
Hakkoda consists of a group of 14 cones 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 the caldera floor to the NE of the Hakkoda group volcanoes, which bury the SE caldera wall. This view looks from the W towards the northern Akakuradake, Idodake, and Hakkodasan volcanoes seen from left to right. · 写真: Photo by Takashi Kudo, 1996 (Hokkaido University). · Wikimedia Commons
タイプ
成層火山
Japan
地域
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
標高
1585m
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 basaltic-to-rhyolitic Hakkodasan volcano 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 than the southern group. Hakkoda-Odake, Ido-dake, and Tsurugi-dake have well-preserved craters. Akakuradake has a 1-km-wide explosion crater breached to the north. No historical eruptions are known, although an active solfatara occurs at Idodake, and hot springs are found at several locations within the caldera. Three minor phreatic eruptions were documented from Jigokunuma on the SW flank of Odake volcano from the 13th-17th centuries. Three soldiers on a training mission in July 1997 were killed by inhalation of volcanic gas.

Wikipedia の要約

要約が短いです。詳細は記事全文をご覧ください。

八甲田山(はっこうださん)は、青森市の南側にそびえる大岳(標高1,584m)を主峰とする18の山々からなる複数火山の総称。日本百名山の一つ。

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噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
2850 BCE~2650 BCE · 1件 · 最大 VEI 22250 BCE~2050 BCE · 1件 · 最大 VEI 31250 BCE~1050 BCE · 1件 · 最大 VEI 150 BCE~150 · 1件 · 最大 VEI 1350~550 · 1件 · 最大 VEI 11150~1350 · 1件 · 最大 VEI 11350~1550 · 1件 · 最大 VEI 12850 BCE1850 BCE650 BCE3501350

詳細タイムライン

  1. 1550年 (±100年)VEI 1地質学的推定
    1550 ~ 進行中
    SW flank of O-dake (Jigoku-numa)
  2. 1340年 (±75年)VEI 1地質学的推定
    1340 ~ 進行中
    SW flank of O-dake (Jigoku-numa)
  3. 450年VEI 1地質学的推定
    450 ~ 進行中
    O-dake
  4. 紀元前 50年VEI 1地質学的推定
    BCE 50 ~ 進行中
    O-dake
  5. 紀元前 1150年VEI 1地質学的推定
    BCE 1150 ~ 進行中
    O-dake
  6. 紀元前 2250年VEI 3地質学的推定
    BCE 2250 ~ 進行中
    O-dake
  7. 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。