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 High School Diyarbakır, in 1955, based on a special law enacted by the Turkish Parliament. The name was changed to "Anatolian High Schools" in 1975. These schools admitted students based on an academic test administered at the end of grade 5, which was the basic elementary education back then. The schools offered a year of foreign language education as a preparatory year followed by foreign-language medium of instruction seven years of middle and high school grades. Several private schools followed the Anatolian School model particularly as an alternative to foreign-based American, French and German schools. There is also one Anatolian School in