Meidob Volcanic Field
火山原 · Sudan · 2000m
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- タイプ
- 火山原
- 国
- Sudan
- 地域
- 北アフリカ / 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.
Wikipedia の要約
英語版の要約Meidob volcanic field is a Holocene volcanic field in Darfur, Sudan. It is one of several volcanic fields in Africa whose origin is explained by the activity of mantle plumes and their interaction with crustal structures. Meidob lies at the southern margin of the Sahara.
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噴火履歴
詳細タイムライン
- 紀元前 2950年 (±500年)VEI 0地質学的推定BCE 2950 ~ 進行中Vent VF 214
- 紀元前 3000年VEI 4地質学的推定BCE 3000 ~ 進行中Central Meidob volcanic field
- 紀元前 3050年VEI 4地質学的推定BCE 3050 ~ 進行中SW crater of vent VF 57
- 紀元前 4150年 (±1450年)VEI 4地質学的推定BCE 4150 ~ 進行中Central Meidob volcanic field
- 紀元前 5250年 (±500年)VEI ?地質学的推定BCE 5250 ~ 進行中Central Meidob volcanic field
- 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。