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 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