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Cherpuk Group

火砕丘 · Russia · 1868m

The Yuzhny Cherpuk cinder cone (left-center horizon) and its andesitic lava flow are located 11 km SSW from Ichinsky volcano. The fresh-looking lava flow was erupted about 6,500 years ago and traveled 18 km. Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that was constructed along the crest of the Sredinny Range.
The Yuzhny Cherpuk cinder cone (left-center horizon) and its andesitic lava flow are located 11 km SSW from Ichinsky volcano. The fresh-looking lava flow was erupted about 6,500 years ago and traveled 18 km. Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that was constructed along the crest of the Sredinny Range. · 写真: Copyrighted photo by Adam Kirilenko, 2000 (Holocene Kamchatka Volcanoes, www.kamchatka.ginras.ru).
タイプ
火砕丘
Russia
地域
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
標高
1868m
座標
55.550, 157.470
最終噴火
-4550年
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Minor
主要岩石
Andesite / Basaltic Andesite
地質学的概要

Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky volcano that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that fed 1.8 km3 lava flows down both sides of the range to the NW and SE. A narrow tongue of the SE flow diverted an additional 10 km S, for a total distance of 22 km. Yuzhny Cherpuk, 11 km SSW of Ichinsky, produced a 1.7 km3 lava flow that traveled 18 km S and then SE. The flow descended to 640 m elevation and dammed tributaries of the Ketachan River, producing three lakes. The two cones are sometimes considered to be satellitic cones to Ichinsky, but Pevzner et al. (2000) noted petrological distinctions that suggest an independent origin. Unpublished radiocarbon ages revise those in Pevzner et al. (2000) and indicate that both cones were formed about 6,500 years ago.

Wikipedia の要約

英語版の要約

Cherpuk Group is a group of two cinder cones located in the central part of Kamchatka Peninsula, Russia. It is a group of a few mostly dormant cinder cones.

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
4550 BCE~4550 BCE · 1件 · 最大 VEI ?4550 BCE4550 BCE4549 BCE4549 BCE4549 BCE

詳細タイムライン

  1. 紀元前 4550年VEI ?地質学的推定
    BCE 4550 ~ 進行中
    North and South Cherpuk

外部リンク

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