본문으로 건너뛰기

Gabillema

성층화산 · Ethiopia · 1459m

Gabillema is located along the axis of the Addado graben. The summit of the volcano lies below and to the left of the center of this Landsat image. Rhyolitic lava domes are on the flanks of the volcano and a 5 x 17 km basaltic lava field covers the Ado Bad Plain (Ado Lake) N of the volcano, originating from a broad area of fissure vents and spatter cones on the N side.
Gabillema is located along the axis of the Addado graben. The summit of the volcano lies below and to the left of the center of this Landsat image. Rhyolitic lava domes are on the flanks of the volcano and a 5 x 17 km basaltic lava field covers the Ado Bad Plain (Ado Lake) N of the volcano, originating from a broad area of fissure vents and spatter cones on the N side. · 사진: NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology). · Wikimedia Commons
화산 유형
성층화산
국가
Ethiopia
지역
Eastern Africa Volcanic Regions / Main Ethiopian Rift Volcanic Province
해발
1459m
좌표
11.080, 41.270
마지막 분화
미확인
판구조 환경
Rift zone / Intermediate crust (15-25 km)
화산 지형
Composite
주요 암석
Rhyolite
지질학적 요약

Gabillema is a rhyolitic stratovolcano along the axis of the Addado graben. The volcano was constructed at the intersection of the central Afar rift zone with the northern end of the Main Ethiopian Rift. Rhyolitic lava domes are located on the flanks, and a 5 x 17 km basaltic lava field that covers the Ado Bad plain north of the volcano originated from a broad area of fissure vents and spatter cones on the north side of Gabillema. Young lava flows also occur south and east of the volcano, the latter along E-W fissures. This period of rejuvenation, perhaps not directly related to Gabillema, has included rhyolitic as well as basaltic volcanism.

분화 이력

상세 타임라인

분화 기록이 없습니다.

외부 링크

⚠ 참고용 정보입니다. 재난 대응에 사용하지 마세요.