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 hieroglyphs aged some 700 years, was marginalized by competing alphabetic scripts and fell into oblivion. While almost all the preserved texts employing Anatolian hieroglyphs are written in the Luwian language, some features of the script suggest its earliest development within a bilingual Hittite-Luwian environment. For example, the sign which has the form of a "taking" or "grasping" hand has the value /ta/, which is precisely the Hittite word ta-/da- "to take," in contrast with the Luwian cognate of the same meaning which is la-. There was occasionally some use of Anatolian hieroglyphs to write foreign material like Hurrian theonyms, or glosses