The North Anatolian Fault is a major geological fault line located in northern Turkey. It stretches approximately 1,200 kilometers (about 750 miles) from the Aegean Sea in the west to the Eastern Anatolia region in the east. This fault is known for its significant seismic activity, making it one of the most studied fault lines in the world. The fault marks the boundary between the Anatolian Plate and the Eurasian Plate. As these tectonic plates move past each other, they can cause powerful earthquakes. Notable earthquakes along the North Anatolian Fault have had a substantial impact on nearby cities and communities, highlighting the importance of monitoring this geological feature.