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ロシア · 楯状火山

ティティーラ山

Titila

タイプ
楯状火山
標高
1523m
最終噴火
-550年
Titila volcano is viewed looking towards the SE. It started to erupt in the late Pleistocene and was active about 10,000-8,000 and 3,000-2,500 years ago. A flank vent (forming the peak to the right) formed during the early Holocene. Its lava flows dammed a river to form Glubokoye Lake to the right.
Titila volcano is viewed looking towards the SE. It started to erupt in the late Pleistocene and was active about 10,000-8,000 and 3,000-2,500 years ago. A flank vent (forming the peak to the right) formed during the early Holocene. Its lava flows dammed a river to form Glubokoye Lake to the right. · 写真: Copyrighted photo by Maxim Portnyagin (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
タイプ
楯状火山
国
ロシア
地域
北西太平洋 / Central Kamchatka Volcanic Arc
標高
1523m
座標
57.406, 160.108
最終噴火
-550年
テクトニクス環境
沈み込み帯 / 大陸地殻 (> 25 km)
火山地形
楯状火山
主要岩石
玄武岩 / ピクライト質玄武岩
地質学的概要

Titila is a small basaltic shield volcano NW of Lake Glubokoye, west of the crest of the central Sredinny Range. Lava flows radiate from two summit craters, and cinder cones are prominent on its southern flank. Titila overlaps to the W with another small shield volcano, Rassoshina, along with other features in the Sedanka Lava Field to the south. The latest known eruption took place about 2,500 years ago.

Wikipedia の要約

英語版の要約

Titila is a shield volcano located in the northern part of Kamchatka Peninsula, Russia. It comprises two shield volcanoes: Titila and Rassoshina, from which Titila is the higher one.

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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
紀元前 550~紀元前 550 · 1件 · 最大 VEI ?紀元前 550紀元前 550紀元前 549紀元前 549紀元前 549

詳細タイムライン

  1. 紀元前 550年VEI ?地質学的推定
    紀元前 550 ~ 終了日不明

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