The Main Ethiopian Rift is a key sector of the East African Rift System that connects the Afar
depression, at Red Sea–Gulf of Aden junction, with the Turkana depression and Kenya Rift …

This review paper presents a series of time reconstruction maps of the 'East African Rift
System'('EARS'), illustrating the progressive development of fault trends, subsidence …

Reconstructions of the relative positions of the India and Eurasia plates, using recently
revised histories of movement between India and Somalia and between North America and …

Many continental rifts are subjected to volcanism in tandem with rifting, which has raised a
long-standing debate about whether magmatism is the cause or the consequence of plate …

The evolution and characteristics of narrow continental rifting are illustrated in this paper
through a review of recent lithospheric-scale analog models of continental extension …

The Ethiopian region records about one billion years of geological history. The first event
was the closure of the Mozambique ocean between West and East Gondwana with the …

Inherited rheological structures in the lithosphere are expected to have large impact on the
architecture of continental rifts. The Turkana depression in the East African Rift connects the …

The lack of valuable baseline information about groundwater availability hinders the robust
decision-making process of water management in humid, arid, and semi-arid climate …

The main Ethiopian rift is an active rift in the break-up stage, and it marks the incipient
boundary between the Nubia and Somalia plates. Rifting started with the activation of large …

Abstract The Ethiopia Afar Geoscientific Lithospheric Experiment (EAGLE) was undertaken
to provide a snapshot of lithospheric break-up above a mantle upwelling at the transition …