Turkey as a country is very prone to earthquakes. The view to the right in the main view panel shows several major earthquakes that have occurred in the region in the past 100 years.
The historical location of the earthquakes clearly seems to indicate a definite pattern and area within which earthquakes occur in this region.
In addition to the two large earthquakes, a number of smaller earthquakes also occurred on Feb. 6.
The size of the circle corresponds to the magnitude of the earthquake.
These earthquakes are clustered around a region known as the East Anatolian Fault.
So why is this fault here? The East Anatolian Fault is actually the boundary between two tectonic plates that are interacting.
The East Anatolian Fault is a 700 km (435 mi.) long transform fault. The earthquakes on February 6, 2023 were the result of the Arabian Plate sliding horizontally past the Anatolian Plate.
Although the Feb. 6 earthquakes were the result of tectonic stresses between the Anatolian and the African Plates, a nearby third tectonic plate has also contributed to earthquakes in the past in Turkey.
The African Plate forms a convergent boundary where it meets the Anatolian and the Arabian Plates. The point where all three plates meet is known as a “triple point”.