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The
Ethiopian Rift Valley
The African rift valley is one
of the most fascinating natural wonders, known for its unique biodiversity
and for being considered -for the important paleoanthropologic discoveries-
the "cradle of mankind", i.e. the place where our species
has evolved and diversified in the last millions of years. Characterized
by a system of linear valleys extending for thousands of kilometers,
the rift valley is a huge fracture on the surface of our planet
that progressively widens with time, tearing the eastern portion
of the African continent apart. It represents a geological wonder
where volcanism, earthquakes and fracturing of the Earth's crust
are the surface expressions of the enormous forces that shape our
planet. These web pages are dedicated to the analysis of the Ethiopian
sector of the African rift valley, an ideal natural laboratory to
analyze the evolution and dynamics of continental extension and
the rupture of lithospheric plates.
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NEWS


Our new work "Quaternary volcano-tectonic activity in the Soddo region, western margin of the Southern Main Ethiopian Rift" has been accepted for publication in Tectonics
New paper of interest: Mantle upwelling and initiation of rift segmentation beneath the Afar Depression by Hammond et al. Geology, 41, 635–638.
New paper of interest: Controls on magmatic cycles and development of rift topography of the Manda Hararo segment (Afar, Ethiopia) by Medynski et al. Earth Planet Sci Letters, 367, 133–146
New paper of interest: Seismic anisotropy in eastern Africa, mantle flow, and the African
superplume by Bagley and Nyblade, GRL, 40, 1–6
Our new paper "Re-orientation of the extension direction and pure extensional faulting at oblique rift margins: comparison between the Main Ethiopian Rift and laboratory experiments" is in press on Terra Nova
News
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