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 every colour and shade can be obtained so that it is nearly impossible to identify, in a finished carpet, whether natural or artificial dyes were used. Modern carpets can be woven with carefully selected synthetic colours, and provide artistic and utilitarian value. The Anatolian rug is distinct from carpets of other provenience in that it makes more pronounced use of primary colours. Western Anatolian carpets prefer red and blue colours, whereas Central Anatolian use more red and yellow, with sharp contrasts set in white. A variety of tools are needed in the construction of a handmade rug. A loom, a