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Atlasov

Nylgimelkin

楯状火山 · Russia · 1764m

This cone formed at the top of Nylgimelkin, with the larger Pleistocene Khuvkhoitun volcano visible in the background. Lava flows from Nylgimelkin were erupted along a fissure about 5,500 years ago.
This cone formed at the top of Nylgimelkin, with the larger Pleistocene Khuvkhoitun volcano visible in the background. Lava flows from Nylgimelkin were erupted along a fissure about 5,500 years ago. · 写真: Copyrighted photo by Maria Pevzner, 2005 (Russian Academy of Sciences, Moscow).
タイプ
楯状火山
Russia
地域
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
標高
1764m
座標
57.970, 160.650
最終噴火
-3550年
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Shield
主要岩石
Basalt / Picro-Basalt
地質学的概要

The basaltic Nylgimelkin (also known as Atlasov) shield volcano and the topographically higher but smaller shield of Novagrablenova are dwarfed by their neighbor, the glacier-clad Pleistocene Khuvkhoitun, the highest Quaternary volcano of the northern Sredinny Range. The two youthful shields were constructed on the W and NW flanks of Khuvkhoitun. Lava flows from them extend primarily to the west. Cinder cones and a lava flow were erupted along a fissure at Nylgimelkin about 5,500 years ago.

Wikipedia の要約

英語版の要約

Atlasova is a basaltic shield volcano situated in Kamchatka. It is named after Russian explorer Vladimir Atlasov.

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
3550 BCE~3550 BCE · 1件 · 最大 VEI ?3550 BCE3550 BCE3549 BCE3549 BCE3549 BCE

詳細タイムライン

  1. 紀元前 3550年VEI ?地質学的推定
    BCE 3550 ~ 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。