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Meidob Volcanic Field

火山原 · Sudan · 2000m

The dark-colored area in the center of this Space Shuttle view is the alkaline Meidob volcanic field in western Sudan. This broad volcanic field covers an area of 5,000 km2 with nearly 700 Pliocene-to-Holocene vents. The margins of the field are dominated by basaltic scoria cones and associated lava flows, but the lava domes, tuff rings, and maars that are concentrated along the central E-W-trending axis of the volcanic field are among the youngest features. The latest dated eruptions took place about 5,000 years ago.
The dark-colored area in the center of this Space Shuttle view is the alkaline Meidob volcanic field in western Sudan. This broad volcanic field covers an area of 5,000 km2 with nearly 700 Pliocene-to-Holocene vents. The margins of the field are dominated by basaltic scoria cones and associated lava flows, but the lava domes, tuff rings, and maars that are concentrated along the central E-W-trending axis of the volcanic field are among the youngest features. The latest dated eruptions took place about 5,000 years ago. · 写真: NASA Space Shuttle image STS073-713-87, 1995 (http://eol.jsc.nasa.gov/). · Wikimedia Commons
タイプ
火山原
Sudan
地域
Northern Africa Volcanic Regions / Southeast Sahara Volcanic Province
標高
2000m
座標
15.320, 26.470
最終噴火
-2950年
テクトニクス環境
Intraplate / Continental crust (> 25 km)
火山地形
Cluster
主要岩石
Trachybasalt / Tephrite Basanite
地質学的概要

The alkaline Meidob volcanic field in western Sudan, at the NE end of the Darfur volcanic province, covers an area of 5,000 km2 with nearly 700 Pliocene-to-Holocene vents. The field was constructed over an uplifted Precambrian igneous and metamorphic basement and is elongated in an E-W direction. Basaltic scoria cones and associated lava flows dominate, but trachytic-phonolitic lava domes, tuff rings, and maars are among the youngest volcanic products. Basaltic scoria cones are scattered throughout the field; their lavas have produced a broad lava plateau. The central part of the field consists of younger phonolitic lava flows, trachytic pumice-fall deposits, ignimbrites, and maars. The youngest dated eruptions about 5,000 years ago produced a tuff ring and a lava flow.

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
6050 BCE~5856 BCE · 1件 · 最大 VEI 45275 BCE~5081 BCE · 1件 · 最大 VEI ?4306 BCE~4112 BCE · 1件 · 最大 VEI 43144 BCE~2950 BCE · 3件 · 最大 VEI 46050 BCE5275 BCE4500 BCE3919 BCE3144 BCE

詳細タイムライン

  1. 紀元前 2950年 (±500年)VEI 0地質学的推定
    BCE 2950 ~ 進行中
    Vent VF 214
  2. 紀元前 3000年VEI 4地質学的推定
    BCE 3000 ~ 進行中
    Central Meidob volcanic field
  3. 紀元前 3050年VEI 4地質学的推定
    BCE 3050 ~ 進行中
    SW crater of vent VF 57
  4. 紀元前 4150年 (±1450年)VEI 4地質学的推定
    BCE 4150 ~ 進行中
    Central Meidob volcanic field
  5. 紀元前 5250年 (±500年)VEI ?地質学的推定
    BCE 5250 ~ 進行中
    Central Meidob volcanic field
  6. 紀元前 6050年 (±1600年)VEI 4地質学的推定
    BCE 6050 ~ 進行中
    NE crater of vent VF 57

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。