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 peoples Anatolian peoples Anatolians were Indo-European peoples of the Near East identified by their use of the Anatolian languages. These peoples were among the oldest Indo-European ethnolinguistic groups, one of the most archaic, because Anatolians were the first or among the first branches of Indo-European peoples to separate from the initial Proto-Indo-European community that gave origin to the individual Indo-European peoples. Together with the Proto-Tocharians, who migrated eastward, the Anatolian peoples constituted the first known waves of Indo-European emigrants out of the Eurasian steppe. It is likely that they reached the Near East from the north, via the Balkans or the