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ゴールヌィー・インスチトゥート山

Gorny Institute

成層火山 · Russia · 2125m

Gorny Institute volcano, seen here from the south, lies at the NE end of chain of small late-Quaternary volcanoes extending NE from Kebeney volcano in the central Sredinny Range. It is one of the large stratovolcanoes in the Sredinny Range that have been active during the Holocene.
Gorny Institute volcano, seen here from the south, lies at the NE end of chain of small late-Quaternary volcanoes extending NE from Kebeney volcano in the central Sredinny Range. It is one of the large stratovolcanoes in the Sredinny Range that have been active during the Holocene. · 写真: Copyrighted photo by Maria Pevzner, 2004 (Russian Academy of Sciences, Moscow).
タイプ
成層火山
国
Russia
地域
北西太平洋 / Central Kamchatka Volcanic Arc
標高
2125m
座標
57.330, 160.200
最終噴火
1250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

Gorny Institute volcano lies at the NE end of chain of small late-Quaternary volcanoes extending NE from Kebeney volcano in the central Sredinny Range. It was constructed near the steep-walled eastern margin of a major NE-SW-trending graben extending NE from Kebeney volcano. A line of cinder cones with the same orientation is located on the NE and SW flanks. More than 20 pyroclastic horizons have been documented, and the last major eruption took place about 700 years ago.

Wikipedia の要約

英語版の要約

Gorny Institute, also spelled Gornyi Institut, is a stratovolcano located in the Sredinny Range on Russia's Kamchatka Peninsula. It lies just east of the Titila volcano and north of the Kebeney volcano.

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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
4250 BCE~4054 BCE · 1件 · 最大 VEI 0857~1054 · 1件 · 最大 VEI ?1054~1250 · 1件 · 最大 VEI ?4250 BCE2875 BCE1500 BCE321 BCE1054

詳細タイムライン

  1. 1250年VEI ?地質学的推定
    1250 ~ 進行中
  2. 1000年VEI ?地質学的推定
    1000 ~ 進行中
  3. 紀元前 4250年VEI 0地質学的推定
    BCE 4250 ~ 進行中
    South flank (Sedanka lava flow)

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。