An earthquake occurred in Eastern and Southeastern Anatolia: Characteristics of the Eastern Anatolian Fault Line and the provinces it passes through

The earthquake was felt in Eastern and Southeastern Anatolia. It was reported that the earthquake was felt in many provinces. Kandilli Observatory announced the magnitude of the earthquake as 5.8. AFAD reported the magnitude of the earthquake as 5.4. So, which provinces does the Eastern Anatolian fault line pass through? Eastern Anatolian fault line length and features

WHAT IS THE EASTERN ANATOLIA FAULT LINE?

Eastern Anatolian Fault Line: The Eastern Anatolian Fault Line is a large fracture in the east of Türkiye. The fault lies along the border between the Anatolian Plate and the Arabian Plate.

The Eastern Anatolian Fault Line starts from the Maraş Triple Conjunction at the northern end of the Dead Sea Crack, runs in the northeast direction and ends at the Karlıova Triple Concatenation, where it meets the North Anatolian Fault Line.

WHICH PROVINCES DOES THE EASTERN ANATOLIA FAULT LINE PASS THROUGH?

Eastern Anatolian Fault Line; It continues to Kahramanmaraş, Hatay, Gaziantep, Osmaniye, Adıyaman, Elazığ, Bingöl and Muş and meets the North Anatolian Fault Line.

HOW LONG IS THE EASTERN ANATOLIA FAULT LINE?

The length of the Eastern Anatolian Fault Zone can be given differently depending on the definition used and which sections of the fault zone are included. In a study published in MTA Magazine, it is stated that the distance between Karlıova and Hatay is approximately 600 kilometers, while some public institutions' reports give a length of approximately 580 kilometers.

CHARACTERISTICS OF THE EASTERN ANATOLIA FAULT LINE

The Eastern Anatolian Fault Zone generally extends in the northeast-southwest direction and is a left-lateral strike-slip fault system. The fault is associated with tectonic movements between the Arabian Plate moving northward and the Anatolian block moving westward.

According to scientific studies, EAFZ is a fault zone consisting of segments of different lengths rather than a single and uninterrupted fracture. It is stated in MTA Magazine that the lengths of the segments in question vary between approximately 50 and 145 kilometers.

It is stated that the fault zone has been active for the last few million years and tectonic movements continue today. Studies indicate that the annual slip rate for the EAFZ is approximately 5-8 millimeters.