The Anatolian Fault is a major geological fault line located in northwestern Turkey. It is part of the complex boundary between the Eurasian and Arabian tectonic plates. The fault is known for its significant seismic activity, which can lead to powerful earthquakes. Stretching approximately 1,200 kilometers, the Anatolian Fault is characterized by a right-lateral strike-slip motion, meaning that the two sides of the fault move horizontally past each other. This movement is responsible for the frequent earthquakes in the region, making it a critical area for geological studies and earthquake preparedness.