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Korath

Korath Range

凝灰岩円錐丘 · Ethiopia · 912m

The fissure-controlled Korath Range is an isolated group of tuff cones and lava flows in southern Ethiopia that were erupted along the Turkana Rift. The lava flows traveled up to about 5 km with visible lobate margins, most prominently on the W flanks.
The fissure-controlled Korath Range is an isolated group of tuff cones and lava flows in southern Ethiopia that were erupted along the Turkana Rift. The lava flows traveled up to about 5 km with visible lobate margins, most prominently on the W flanks. · 写真: NASA Landsat 7 image (worldwind.arc.nasa.gov) · Wikimedia Commons
タイプ
凝灰岩円錐丘
Ethiopia
地域
Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
標高
912m
座標
5.117, 35.892
最終噴火
不明
テクトニクス環境
Rift zone / Intermediate crust (15-25 km)
火山地形
Cluster
主要岩石
Trachybasalt / Tephrite Basanite
地質学的概要

The Korath Range is an isolated group of about 20 tuff cones and lava flows in southern Ethiopia that were erupted along the Turkana Rift, which extends north from Kenya. Many of the cones issued lava flows from their flanks that traveled up to about 5 km. The apparent youngest flow issued from the central crater and flowed through a breach in its rim. The absolute age of the dominantly basanitic-tephritic lava flows is unknown, but a shell adhering to the youngest flow was radiocarbon dated at 7,900 years before present (BP) (Brown et al., 1969). Davidson (1983) indicated an age between 30,000 and 7,900-9,500 BP.

噴火履歴

詳細タイムライン

噴火記録はありません。

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。