Search results
Results from the WOW.Com Content Network
Between and , the Somali plate began rifting from the African plate along the East African Rift. [2] Since the continent of Africa consists of crust from both the African and the Somali plates, some literature refers to the African plate as the Nubian plate to distinguish it from the continent as a whole. [3]
Since a reorganisation of the involved tectonic plates c., the AOC moves in discrete steps westward along the Aden Ridge. West of the southern termination of the Owen fracture zone, the Beautemps-Beaupré Basin, a new plate boundary develops and the basin will be transferred from the Arabian plate to the Indian plate in a near future. [2]
This file has multiple extracted images: Arabia, Egypt, Nubia and Abyssinia 1883 map (cropped-El Hassa).jpg Arabia, Egypt, Nubia and Abyssinia 1883 map (cropped).jpg
The triple junction is at , inside the Afar Triangle (at center shadedFault lines are in black, and red triangles show historically active volcanoes. The Afar triple junction (also called the Afro-Arabian rift system) is located along a divergent plate boundary dividing the Nubian, Somali, and Arabian plates.
The Arabian plate is a minor tectonic plate in the Northern and Eastern Hemispheres.. It is one of the three continental plates (along with the African and Indian plates) that have been moving northward in geological history and colliding with the Eurasian plate.
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.
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 Alpine orogeny is caused by the continents Africa, Arabia and India and the small Cimmerian Plate colliding (from the south) with Eurasia in the north. Convergent movements between the tectonic plates (the African Plate, the Arabian Plate and the Indian Plate from the south, the Eurasian Plate and the Anatolian Sub-Plate from the north, and many smaller plates and microplates) had already ...