Anatolian Plate the Eurasian Plate to its north is blocking motion in that direction. The African Plate is subducting beneath the Anatolian Plate along the Cyprus and Hellenic Arcs offshore in the Mediterranean Sea. Anatolian Plate The Anatolian Plate or the Turkish Plate is a continental tectonic plate comprising most of the Anatolia (Asia Minor) peninsula (and the country of Turkey). To the east, the East Anatolian Fault, a left lateral transform fault, forms a boundary with the Arabian Plate. To the south and southwest is a convergent boundary with the African Plate. This convergence manifests in compressive features within the oceanic
Proto-Anatolian language continue a special class of presents which had a complicated relationship with the Proto-Indo-European perfect. Proto-Anatolian language Proto-Anatolian is the proto-language from which Anatolian languages emerged. As with all other proto-languages, no attested writings have been found; the language has been reconstructed by applying the comparative method to all the attested Anatolian languages as well as other Indo-European languages. For the most part, Proto-Anatolian has been reconstructed on the basis of Hittite, the best-attested Anatolian language. However, the usage of Hittite cuneiform writing system limits the enterprise of understanding and reconstructing Anatolian phonology, partly from the deficiency of the adopted