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Meidob Volcanic Field

Volcanic field · 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. · Photo: NASA Space Shuttle image STS073-713-87, 1995 (http://eol.jsc.nasa.gov/). · Wikimedia Commons
Type
Volcanic field
Country
Sudan
Region
Northern Africa Volcanic Regions / Southeast Sahara Volcanic Province
Elevation
2000m
Coordinates
15.320, 26.470
Last eruption
-2950
Tectonic setting
Intraplate / Continental crust (> 25 km)
Landform
Cluster
Major rock type
Trachybasalt / Tephrite Basanite
Geological summary

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.

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
6050 BCE~5856 BCE · 1 eruptions · max VEI 45275 BCE~5081 BCE · 1 eruptions · max VEI ?4306 BCE~4112 BCE · 1 eruptions · max VEI 43144 BCE~2950 BCE · 3 eruptions · max VEI 46050 BCE5275 BCE4500 BCE3919 BCE3144 BCE

Detailed timeline

  1. 2950 BCE (±500 yrs)VEI 0Geological estimate
    BCE 2950 – Ongoing
    Vent VF 214
  2. 3000 BCEVEI 4Geological estimate
    BCE 3000 – Ongoing
    Central Meidob volcanic field
  3. 3050 BCEVEI 4Geological estimate
    BCE 3050 – Ongoing
    SW crater of vent VF 57
  4. 4150 BCE (±1450 yrs)VEI 4Geological estimate
    BCE 4150 – Ongoing
    Central Meidob volcanic field
  5. 5250 BCE (±500 yrs)VEI ?Geological estimate
    BCE 5250 – Ongoing
    Central Meidob volcanic field
  6. 6050 BCE (±1600 yrs)VEI 4Geological estimate
    BCE 6050 – Ongoing
    NE crater of vent VF 57

External links

⚠ For reference only. Not for emergency response.