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Meidob Volcanic Field

Campo vulcanico · Sudan · 2000 m

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. · Foto: NASA Space Shuttle image STS073-713-87, 1995 (http://eol.jsc.nasa.gov/). · Wikimedia Commons
Tipo
Campo vulcanico
Paese
Sudan
Regione
Northern Africa Volcanic Regions / Southeast Sahara Volcanic Province
Altitudine
2000 m
Coordinate
15.320, 26.470
Ultima eruzione
-2950
Contesto tettonico
Intraplate / Continental crust (> 25 km)
Forma vulcanica
Cluster
Roccia principale
Trachybasalt / Tephrite Basanite
Sintesi geologica

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.

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
6050 BCE~5856 BCE · 1 eruzioni · VEI max. 45275 BCE~5081 BCE · 1 eruzioni · VEI max. ?4306 BCE~4112 BCE · 1 eruzioni · VEI max. 43144 BCE~2950 BCE · 3 eruzioni · VEI max. 46050 BCE5275 BCE4500 BCE3919 BCE3144 BCE

Cronologia dettagliata

  1. 2950 a.C. (±500 anni)VEI 0Stima geologica
    BCE 2950 – In corso
    Vent VF 214
  2. 3000 a.C.VEI 4Stima geologica
    BCE 3000 – In corso
    Central Meidob volcanic field
  3. 3050 a.C.VEI 4Stima geologica
    BCE 3050 – In corso
    SW crater of vent VF 57
  4. 4150 a.C. (±1450 anni)VEI 4Stima geologica
    BCE 4150 – In corso
    Central Meidob volcanic field
  5. 5250 a.C. (±500 anni)VEI ?Stima geologica
    BCE 5250 – In corso
    Central Meidob volcanic field
  6. 6050 a.C. (±1600 anni)VEI 4Stima geologica
    BCE 6050 – In corso
    NE crater of vent VF 57

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.