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 hypothesis 2014: Bayesian analysis has been criticized on account of its inferring the lifespan of a language from that of some of its words; the idiosyncratic outcome of, for example, the Albanian language raises doubts about the method and the data. Furthermore, other lexicostatistical (and some glottochronological) studies have produced results different from the results produced by Gray and Atkinson., as has a 2015 phylogenetic analysis which instead supports the Kurgan hypothesis. However, the main objection to the Anatolian hypothesis is that it requires an unrealistically early date. Most estimates date Proto-Indo-European between 4500 and 2500 BC, with the most probable