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Spokoyny

Spokoiny

成層火山 · Russia · 2171m

Spokoiny, seen here from the east, lies immediately south of Ostry and NE of Iktunup volcano in the northern Sredinny Range. Lava flows from the summit cone extend down drainages to the east and west.
Spokoiny, seen here from the east, lies immediately south of Ostry and NE of Iktunup volcano in the northern Sredinny Range. Lava flows from the summit cone extend down drainages to the east and west. · 写真: Copyrighted photo by Maria Pevzner, 2005 (Russian Academy of Sciences, Moscow). · Wikimedia Commons
タイプ
成層火山
Russia
地域
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
標高
2171m
座標
58.130, 160.820
最終噴火
-3450年
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Composite
主要岩石
Dacite
地質学的概要

The dacitic-to-rhyolitic Spokoiny stratovolcano lies immediately south of Ostry volcano and NE of Iktunup volcano in the northern Sredinny Range. The volcano, also known as Kutina, was active during the early and mid-Holocene. Deposits from five eruptions during this interval have been documented, the last of which took place about 5400 years ago. Cinder cones are located on the W flank, and lava flows from the symmetrical summit cone extend down drainages to both the east and west.

Wikipedia の要約

英語版の要約

Spokoyny is a stratovolcano in the northern part of the Sredinny Range in Russia's Kamchatka Peninsula. It forms part of the Volcanoes of Kamchatka Unesco world heritage site.

Wikipedia · CC BY-SA · 記事全文を読む

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
3450 BCE~3450 BCE · 1件 · 最大 VEI ?3450 BCE3450 BCE3449 BCE3449 BCE3449 BCE

詳細タイムライン

  1. 紀元前 3450年VEI ?地質学的推定
    BCE 3450 ~ 進行中

外部リンク

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