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Manda-Inakir

割れ目火口 · Ethiopia-Djibouti · 600m

The dark-colored lava flows extending diagonally across the center of this Landsat image were erupted from pyroclastic cones of Manda-Inakir volcano. These NNW-trending fissure vents and cones are located along the Ethiopia-Djibouti border and represent an uplifted mid-ocean ridge spreading center now exposed above sea level. An eruption in 1928 or 1929 at the SE end of the Manda-Inakir rift near the town of Korili (in Djibouti) produced the Kammourta cinder cone and a lava flow.
The dark-colored lava flows extending diagonally across the center of this Landsat image were erupted from pyroclastic cones of Manda-Inakir volcano. These NNW-trending fissure vents and cones are located along the Ethiopia-Djibouti border and represent an uplifted mid-ocean ridge spreading center now exposed above sea level. An eruption in 1928 or 1929 at the SE end of the Manda-Inakir rift near the town of Korili (in Djibouti) produced the Kammourta cinder cone and a lava flow. · 写真: NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology). · Wikimedia Commons
タイプ
割れ目火口
国
Ethiopia-Djibouti
地域
Eastern Africa Volcanic Regions / Afar Rift Volcanic Province
標高
600m
座標
12.380, 42.200
最終噴火
1928年
テクトニクス環境
Rift zone / Intermediate crust (15-25 km)
火山地形
Cluster
主要岩石
Basalt / Picro-Basalt
地質学的概要

Manda-Inakir consists of a series of NW-trending fissure vents and pyroclastic cones along the Ethiopia-Djibouti border. The elongated complex represents an uplifted mid-ocean ridge spreading center now exposed above sea level. An elongated dome of basement rocks is cut by two axial rifts, the northern of which was active during historical time. Basaltic cinder cones along the rift's marginal faults have produced lava flows on the flanks of the structural dome, yielding a shield-like morphology. An eruption in 1928 or 1929 at the SE end near the town of Korili (in Djibouti) produced the Kammourta cinder cone and a lava flow.

Wikipedia の要約

英語版の要約

Manda-Inakir is a system of fissure vents and cinder cones located along the borders between Djibouti, Eritrea and Ethiopia. Last erupting in 1928, it produced a cinder cone called Kammourta. It has an elevation of over 600 metres.

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
1928~1928 · 1件 · 最大 VEI 219281928192919291929

詳細タイムライン

  1. 1928年VEI 2観測記録
    1928-12-31 ~ 進行中
    Kammourta

外部リンク

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