East Anatolian Fault the Dead Sea Transform, and ending at the Karliova Triple Junction where it meets the North Anatolian Fault. From 1939 to 1999 a series of earthquakes progressed westwards along the North Anatolian Fault. But since 2003 there have been a series on the East Anatolian Fault. These started with the 2003 Bingöl earthquake and include the 2010 Elâzığ earthquake. East Anatolian Fault The East Anatolian Fault is a major strike-slip fault zone in eastern Turkey. It forms the transform type tectonic boundary between the Anatolian Plate and the northward-moving Arabian Plate. The difference in the relative motions of the two
Anatolian beyliks with the Battle of Köse Dağ in 1243 which had the indirect consequence of extending the Turkic territory in Western Anatolia toward the end of the 13th century. Three Anatolian regions remained Christian until their defeat and Ottoman conquest: Combined with the Seljuqs and the immigration of Turkic tribes into the Anatolian mainland the Anatolian Beyliks spread Turkish and Islamic influence in Anatolia. Unlike the Seljuqs, whose language of administration was Persian, the Anatolian emirates adopted spoken Turkish as their formal literary language. The Turkish language achieved widespread use in these principalities and reached its highest sophistication during the Ottoman