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ロシア · マール

Kinenin

タイプ
マール
標高
583m
最終噴火
850年
Kinenin maar is seen in this near-vertical aerial photo, with the lake reaching 1 km in diameter. The maar was named after the Kinenin River seen to the south, and was formed during an explosive eruption about 1,100 years ago. The NE crater wall is significantly higher and coincides with the dominant direction of the tephra dispersal.
Kinenin maar is seen in this near-vertical aerial photo, with the lake reaching 1 km in diameter. The maar was named after the Kinenin River seen to the south, and was formed during an explosive eruption about 1,100 years ago. The NE crater wall is significantly higher and coincides with the dominant direction of the tephra dispersal. · 写真: Photo from Holocene Kamchataka volcanoes (http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
タイプ
マール
国
ロシア
地域
北西太平洋 / Central Kamchatka Volcanic Arc
標高
583m
座標
57.350, 160.970
最終噴火
850年
テクトニクス環境
沈み込み帯 / 大陸地殻 (> 25 km)
火山地形
小規模
主要岩石
玄武岩 / ピクライト質玄武岩
地質学的概要

Kinenin maar lies at the eastern foot of the Sredinny Range, about 80 km NNW of Sheveluch volcano. The 2.5-km-wide, funnel-shaped maar was formed along the Kinenin River, a tributary of the Elovka. It is partially filled by a 1-km-wide lake whose surface is at 400 m elevation. The eastern rim at about 580 m is the high point of the crater. The eruption of Kinenin took place about 1,100 years ago, making it the youngest known maar in Kamchatka. Both silicic pyroclastic flows and mafic pyroclastic ejecta were produced, which were distributed primarily to the ENE. The location is north of the active Kamchatka subduction zone.

噴火履歴

1件の記録用語集
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 · 矢印キーで棒を移動、Enterで表示
850~850 · 1件 · 最大 VEI 4850850851851851

詳細タイムライン

  1. 850年 (±50年)VEI 4地質学的推定
    850 ~ 終了日不明

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