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Meidob Volcanic Field

화산대지 · 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. · 사진: NASA Space Shuttle image STS073-713-87, 1995 (http://eol.jsc.nasa.gov/). · Wikimedia Commons
화산 유형
화산대지
국가
Sudan
지역
Northern Africa Volcanic Regions / Southeast Sahara Volcanic Province
해발
2000m
좌표
15.320, 26.470
마지막 분화
-2950년
판구조 환경
Intraplate / Continental crust (> 25 km)
화산 지형
Cluster
주요 암석
Trachybasalt / Tephrite Basanite
지질학적 요약

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.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
6050 BCE~5856 BCE · 1건 · 최고 VEI 45275 BCE~5081 BCE · 1건 · 최고 VEI ?4306 BCE~4112 BCE · 1건 · 최고 VEI 43144 BCE~2950 BCE · 3건 · 최고 VEI 46050 BCE5275 BCE4500 BCE3919 BCE3144 BCE

상세 타임라인

  1. 기원전 2950년 (±500년)VEI 0지질학적 추정
    BCE 2950 ~ 진행 중
    Vent VF 214
  2. 기원전 3000년VEI 4지질학적 추정
    BCE 3000 ~ 진행 중
    Central Meidob volcanic field
  3. 기원전 3050년VEI 4지질학적 추정
    BCE 3050 ~ 진행 중
    SW crater of vent VF 57
  4. 기원전 4150년 (±1450년)VEI 4지질학적 추정
    BCE 4150 ~ 진행 중
    Central Meidob volcanic field
  5. 기원전 5250년 (±500년)VEI ?지질학적 추정
    BCE 5250 ~ 진행 중
    Central Meidob volcanic field
  6. 기원전 6050년 (±1600년)VEI 4지질학적 추정
    BCE 6050 ~ 진행 중
    NE crater of vent VF 57

외부 링크

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