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 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