West, a left lateralfault boundary with theAfrican plate called theDead Sea Transform (DST), and a divergent boundary with the African plate called theRed Sea Rift which runs the length of the Red Sea;
The Arabian plate was part of the African plate during most of thePhanerozoic Eon (Paleozoic–Cenozoic), until theOligocene Epoch of the Cenozoic Era. The Red Sea rifting began in theEocene, and the separation of Africa and Arabia occurred approximately25 million years ago in the Oligocene, and since then the Arabian plate has been moving toward the Eurasian plate.[5] The opening of the Red Sea rift led to volcanic activity. There are volcanic fields called the Older Harrats, such asHarrat Khaybar andHarrat Rahat, cover parts of the western Arabian plate. Some activity still continues especially aroundMedina,[6] and there are regular eruptions within the Red Sea.[7]
The collision between the Arabian plate and Eurasia is pushing up theZagros Mountains of Iran. Because the Arabian plate and Eurasian plate collide, some cities such as those in southeastern Turkey (which is on the Arabian plate) may undergo earthquakes, tsunamis, and volcanoes.
^Image Science and Analysis Laboratory, NASA-Johnson Space Center."Tectonics of the Arabian Plate".The Gateway to Astronaut Photography of Earth. NASA. Archived fromthe original on 6 July 2007. Retrieved21 July 2007.
^Unal, Bunyamin, Mucahit Eren, and M. Gurhan Yalcin. "Investigation of leakage at Ataturk dam and hydroelectric power plant by means of hydrometric measurements." Engineering Geology 93.1 (2007): 45-63.