EAGLE: The Ethiopia Afar Geoscientific Lithospheric Experiment

The EAGLE logoThe Sierra Nevada

The Miocene–Recent East African rift in Ethiopia is unique worldwide because it exposes subaerially the transition between continental rifting and sea-floor spreading within a young continental flood basalt province. As such, it is an ideal study locale for continental breakup processes and hotspot tectonism. Here we review the results of a recent multi-disciplinary, multi-institutional effort to understand geological processes in the region: The Ethiopia Afar Geoscientific Lithospheric Experiment (EAGLE). In 2001–3 dense broadband seismological networks probed the structure of the upper-mantle, while controlled source wide-angle profiles illuminated both along-axis and across-rift crustal structure of the Main Ethiopian rift (MER). These seismic experiments, complemented by gravity and magnetotelluric surveys, have provided important constraints on variations in rift structure, deformation mechanisms, and melt distribution prior to break-up. Quaternary magmatic zones at the surface within the MER are underlain by high-velocity, dense gabbroic intrusions that accommodate extension without marked crustal thinning. A magnetotelluric study illuminated partial melt in the Ethiopian crust, consistent with an overarching hypothesis of magma assisted rifting. Mantle tomographic images reveal a ~500 km wide low-velocity zone at ≥75 km depth in the upper-mantle that extends from close to the eastern edge of the MER westwards beneath the uplifted and flood basalt-capped NW Plateau. The low-velocity zone does not interact simply with the Miocene–Recent (rifting-related) base of lithosphere topography, but provides an abundant source of partially molten material that assists extension of the seismically and volcanically active MER to the present day.

Some of my Publications Related to Project EAGLE

Return to Ian Bastow's Home Page
Last updated on 27/10/2011