본문으로 건너뛰기

Mega Basalt Field

Mega Volcanic Field

화산대지 · Ethiopia · 1500m

Cones, maars, lava flows, and craters of the Mega Basalt Field located along the Ethiopia-Kenya border are visible across this December 2020 Planet Labs satellite image mosaic (N at the top). It is located near the villages Mega and Megado and covers an area of approximately 1,400 km2. Large lava flows were produced from scoria cones and spatter ramparts, and the largest Maar is El Sod (top right), reaching 2.3 km in diameter and 0.41 km deep.
Cones, maars, lava flows, and craters of the Mega Basalt Field located along the Ethiopia-Kenya border are visible across this December 2020 Planet Labs satellite image mosaic (N at the top). It is located near the villages Mega and Megado and covers an area of approximately 1,400 km2. Large lava flows were produced from scoria cones and spatter ramparts, and the largest Maar is El Sod (top right), reaching 2.3 km in diameter and 0.41 km deep. · 사진: Satellite image courtesy of Planet Labs Inc., 2020 (https://www.planet.com/). · Wikimedia Commons
화산 유형
화산대지
국가
Ethiopia
지역
Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
해발
1500m
좌표
3.971, 38.213
마지막 분화
미확인
판구조 환경
Rift zone / Intermediate crust (15-25 km)
화산 지형
Cluster
지질학적 요약

The Mega Volcanic Field in southern Ethiopia is present on both sides of the 100-km-long NW-SE Mega escarpment, and covers about 1,400 km2. Franceschini et al. (2020) provides an excellent review of this field, from which most of this summary is taken. The field includes 114 monogenetic centers, primarily cinder cones and some maars; the largest maar is the 2.3-km-diameter El Sod. Uneroded lava flows often partially overly deeply eroded lava flows. Large lava flows are usually associated with cinder cones, but fissure-fed flows in the Megado area exhibit oriented spatter ramparts. One of the largest lava flows extends more than 10 km SW from the Mega escarpment and covers about 25 km2; it has a very fresh, black, glassy appearance of the surface, and minimal vegetation. Two samples analyzed by Franceschini et al. (2020) yielded 40Ar/39Ar ages of 0.116 ± 0.005 and 0.044 ± 0.008 Ma; two other samples indicated very recent Holocene ages. These are the first age dates available for this field, and are in agreement with the morphological interpretation of some young cinder cones and lava flows.

분화 이력

상세 타임라인

분화 기록이 없습니다.

외부 링크

⚠ 참고용 정보입니다. 재난 대응에 사용하지 마세요.