Anatolian Plate 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 crust beneath the Mediterranean as well as within the continental crust of Anatolia itself, and also by what are generally considered to be subduction zones along the Hellenic and Cyprus arcs. The
Anatolian rug examples of Anatolian rugs known today date from the thirteenth century. Distinct types of rugs have been woven ever since in court manufactures and provincial workshops, village homes, tribal settlements, or in the nomad's tent. Rugs were simultaneously produced at all different levels of society, mainly using sheep wool, cotton and natural dyes. Anatolian rugs are most often tied with symmetrical knots, which were so widely used in the area that Western rug dealers in the early 20th century adopted the term "Turkish" or "Ghiordes" knot for the technique. From the 1870s onwards, the Ottoman court manufactures also produced silk-piled