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 beyliks Madrassa" in Niğde (1409), all of which respect a new style that considers and incorporates the exterior surroundings also. One of the first examples of the Anatolian beylik architecture hinting at the forming of the Ottoman architecture that aims at uniting the interior space beneath one big dome and forming a monumental architectural structure is "Ulucami Mosque" in Manisa (1374) built by the Saruhan beylik. Also worth noting is the increase in constructions of madrassas that points at the beyliks' attaching greater importance to sciences. Anatolian beyliks Anatolian beyliks (, Ottoman Turkish: "Tavâif-i mülûk", "Beylik" ), sometimes known as Turkmen