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Gabillema

Stratovulcano · Ethiopia · 1459 m

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. · Foto: NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Ethiopia
Regione
Eastern Africa Volcanic Regions / Main Ethiopian Rift Volcanic Province
Altitudine
1459 m
Coordinate
11.080, 41.270
Ultima eruzione
Sconosciuto
Contesto tettonico
Rift zone / Intermediate crust (15-25 km)
Forma vulcanica
Composite
Roccia principale
Rhyolite
Sintesi geologica

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.

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