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恐山

Osorezan

成層火山 · Japan · 878m

The SE side of Osorezan is seen here above Mutsu Bay is the Shimokita Peninsula in northernmost Honshu. It contains a 3-km-wide caldera partly occupied by a shallow lake that drains through the north caldera wall.
The SE side of Osorezan is seen here above Mutsu Bay is the Shimokita Peninsula in northernmost Honshu. It contains a 3-km-wide caldera partly occupied by a shallow lake that drains through the north caldera wall. · 写真: Copyrighted photo by Tadahide Ui (Japanese Quaternary Volcanoes database, RIODB, http://riodb02.ibase.aist.go.jp/strata/VOL_JP/EN/index.htm and Geol Surv Japan, AIST, http://www.gsj.jp/). · Wikimedia Commons
タイプ
成層火山
Japan
地域
北西太平洋 / Northeast Japan Volcanic Arc
標高
878m
座標
41.279, 141.120
最終噴火
1787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

Osorezan, on the Shimokita Peninsula in northernmost Honshu, contains a 5-km-wide caldera partly occupied by a shallow lake that drains through the N caldera wall. Dissected lava domes ring the caldera floor. The andesitic-to-dacitic volcano is largely Pleistocene in age, with activity dating back about 800,000 years. The last identified distal tephra deposit was erupted during the late Pleistocene. The only report of historical activity was in a Tohoku district travel document published in 1787, which stated that Yakeyama in Mutsu country (Osoreyama) had erupted. Older residents reported that large fires and clouds were sometimes seen from the summit, accounting for the volcano's local name, Yakeyama, or "Burning Mountain" (Murayama, 1987). Earthquake swarms have been documented during the second half of the 20th century, and magma bodies have been detected beneath the volcano.

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
1787~1787 · 1件 · 最大 VEI ?17871787178817881788

詳細タイムライン

  1. 1787年VEI ?観測記録
    1787 ~ 進行中

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。