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Meidob Volcanic Field

Medan gunung api · 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
Tipe
Medan gunung api
Negara
Sudan
Wilayah
Northern Africa Volcanic Regions / Southeast Sahara Volcanic Province
Ketinggian
2000 m
Koordinat
15.320, 26.470
Letusan terakhir
-2950
Kondisi tektonik
Intraplate / Continental crust (> 25 km)
Bentuk lahan
Cluster
Batuan utama
Trachybasalt / Tephrite Basanite
Ringkasan geologi

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.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
6050 BCE~5856 BCE · 1 letusan · VEI maks. 45275 BCE~5081 BCE · 1 letusan · VEI maks. ?4306 BCE~4112 BCE · 1 letusan · VEI maks. 43144 BCE~2950 BCE · 3 letusan · VEI maks. 46050 BCE5275 BCE4500 BCE3919 BCE3144 BCE

Garis waktu rinci

  1. 2950 SM (±500 tahun)VEI 0Perkiraan geologi
    BCE 2950 – Berlangsung
    Vent VF 214
  2. 3000 SMVEI 4Perkiraan geologi
    BCE 3000 – Berlangsung
    Central Meidob volcanic field
  3. 3050 SMVEI 4Perkiraan geologi
    BCE 3050 – Berlangsung
    SW crater of vent VF 57
  4. 4150 SM (±1450 tahun)VEI 4Perkiraan geologi
    BCE 4150 – Berlangsung
    Central Meidob volcanic field
  5. 5250 SM (±500 tahun)VEI ?Perkiraan geologi
    BCE 5250 – Berlangsung
    Central Meidob volcanic field
  6. 6050 SM (±1600 tahun)VEI 4Perkiraan geologi
    BCE 6050 – Berlangsung
    NE crater of vent VF 57

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.