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ティティーラ山

Titila

楯状火山 · Russia · 1523m

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
Russia
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
Subduction zone / Continental crust (> 25 km)
火山地形
Shield
主要岩石
Basalt / Picro-Basalt
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.

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
550 BCE~550 BCE · 1件 · 最大 VEI ?550 BCE550 BCE549 BCE549 BCE549 BCE

詳細タイムライン

  1. 紀元前 550年VEI ?地質学的推定
    BCE 550 ~ 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。