Dilek Peninsula-Büyük Menderes Delta National Park Aegean Region in general. The peninsula was shaped into its current form over several geological eras with the tectonic merging of Paleozoic schist formations, Mesozoic limestone and marble deposits, and finally the accretion of large clays and other sediments during the Neogene period. This is partly because of Turkey's unstable fault block terrain, and because of the close proximity of the Anatolian-Aegean plate boundary, which generates massifs of mountains all across western Turkey. This includes the peninsula and the mountains surrounding the Büyük Menderes River, known collectively as the Menderes Massif. The peninsula is highly mountainous, with most of its
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