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 languages which distinguishes masculine and feminine; instead, it exhibits a noun-class system based upon an older animate/inanimate distinction. It should be noted, however, that the masculine/feminine distinction is still a matter of dispute since there are some, such Robert S. P. Beekes, who doubt that the feminine gender originated in PIE. Anatolian languages The Anatolian languages are an extinct family of Indo-European languages that were spoken in Asia Minor (ancient Anatolia), the best attested of them being the Hittite language. The list below gives the Anatolian languages in a relatively flat arrangement, following a summary of the Anatolian family tree by