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 diagonal and land bridges intermittently formed across the Bosphorus and the Sea of Marmara. After the end of the most recent ice age, plants surviving to the west of the Anatolian diagonal could spread back into Europe while those to the east could spread into Syria, Iraq and the Near East. The Taurus Mountains provide a cool damp climate for species that cannot survive the hot dry summer climate on either side, and this could have encouraged survival and speciation, resulting in the many endemic species found here today. Anatolian diagonal The Anatolian diagonal is a theoretical dividing line which runs