East Anatolian Fault 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 plates is manifest in the left lateral motion along the fault. The East and North Anatolian faults together accommodate the westward motion of the Anatolian Plate as it is squeezed out by the ongoing collision with the Eurasian Plate. The East Anatolian Fault runs in a northeasterly direction, starting from the Maras Triple Junction at the northern end of
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