In the early morning of February 6, a devastating magnitude 7.8 earthquake struck southern Turkey, near the border with Syria. Numerous aftershocks followed, the strongest nearly rivaling the power of the main quake, at magnitude 7.5. By evening, the death toll had climbed to more than 3,700 across both countries, according to Reuters, and was expected to continue to rise.
Most of Turkey sits on a small tectonic plate that is sandwiched between two slowly colliding behemoths: the vast Eurasian Plate to the north and the Arabian Plate to the south. As those two plates push together, Turkey is being squeezed out sideways, like a watermelon seed snapped between two fingers, says seismologist Susan Hough of the U.S. Geological Survey.
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The entire country is hemmed in by strike-slip, or sideways-sliding, fault zones: the North Anatolian Fault that runs roughly parallel to the Black Sea, and the East Anatolian Fault, near the border with Syria. As a result, Turkey is highly seismically active. Even so, Monday’s quake, which occurred on the East Anatolian Fault, was the strongest to strike the region since 1939, when a magnitude 7.8 quake killed 30,000 people.
Science News talked with Hough, who is based in Pasadena, Calif., about the quake, its aftershocks and building codes. The conversation has been edited for length and clarity.
SN: You say on Twitter that this was a powerful quake for a strike-slip fault. Can you explain?
Hough: The world has seen bigger earthquakes. Subduction zones generate the biggest earthquakes, as much as magnitude 9 (SN: 1/13/21). But quakes close to magnitude 8 are not common on strike-slip faults. But because they’re on land and tend to be shallow, you can get severe…
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