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In the western Mediterranean, the relative motions of the Eurasian and African plates produce a combination of lateral and compressive forces, concentrated in a zone known as the Azores–Gibraltar Fault Zone. Along its northeast margin, the African plate is bounded by the Red Sea Rift where the Arabian plate is moving away from the African plate.
The Arabian plate was part of the African plate during most of the Phanerozoic Eon (Paleozoic–Cenozoic), until the Oligocene Epoch of the Cenozoic Era. The Red Sea rifting began in the Eocene , and the separation of Africa and Arabia occurred approximately 25 million years ago in the Oligocene, and since then the Arabian plate has been moving ...
Red Sea Rift between the African (Nubian) Plate and the Arabian plate The Red Sea Rift is a mid-ocean ridge between two tectonic plates , the African plate and the Arabian plate . It extends from the Dead Sea Transform fault system, and ends at an intersection with the Aden Ridge and the East African Rift , forming the Afar triple junction in ...
The Aden Ridge is a divergent plate boundary that divides the African (or Somali) and Arabian plate. It extends from the triple junction eastward to the Owen fracture zone, where it meets the Aden–Owen–Carlsberg triple junction between the African, Arabian, and Indo-Australian plates. The spreading rate for Aden Ridge is about 17 ...
The Maraş triple junction is found where the side-by-side African and Arabian plates, both drifting north and demarcated by the north–south trending Dead Sea Transform (itself an extension of the African Rift Valleys), come up against the Anatolian plate lying across their path at the East Anatolian Fault.
A map of East Africa showing some of the historically active volcanoes (as red triangles) and the Afar Triangle (shaded at the center), which is a so-called triple junction (or triple point) where three plates are pulling away from one another: the Arabian plate and two parts of the African plate—the Nubian and Somali—splitting along the East African Rift Zone Main rift faults, plates ...
The Karliova triple junction is a geological intersection point located in eastern Turkey, where the boundaries of the Arabian plate, the Eurasian plate, and the African plate meet. It is a complex structure with multiple faults and fractures, resulting from the collision and convergence of these tectonic plates.
Map of the Dead Sea Transform showing the main fault segments and motion of the Arabian plate relative to the African plate, [1] from GPS data The Dead Sea Transform (DST) fault system, also sometimes referred to as the Dead Sea Rift, is a series of faults that run for about 1,000 km from the Marash triple junction (a junction with the East Anatolian Fault in southeastern Turkey) to the ...
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