North Anatolian Fault the chain is not complete, and that an earthquake will soon strike further west along the fault – perhaps near the heavily populated city of Istanbul. North Anatolian Fault The North Anatolian Fault (NAF) () is an active right-lateral strike-slip fault in northern Anatolia which runs along the transform boundary between the Eurasian Plate and the Anatolian Plate. The fault extends westward from a junction with the East Anatolian Fault at the Karliova Triple Junction in eastern Turkey, across northern Turkey and into the Aegean Sea for a length of 1500 kilometers. It runs about 20 km south of Istanbul.
Anatolian languages 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 Robert Beekes (2010). This model recognizes only one clear subgroup, the Luwic languages. Modifications and updates of the branching order continue, however. A second version opposes Hittite to Western Anatolian, and divides the latter node into Lydian, Palaic, and a Luwian group (instead of Luwic). Hittite ("nešili") was the language