Explained: Why was the Turkey-Syria earthquake so bad?

LONDON: The magnitude 7.8 earthquake that struck Turkey and Syria on Monday is likely one of the deadliest this decade, seismologists said, with a rupture more than 100km (62 miles) between the Anatolian and Arabian plates.
Turkey-Syria earthquake: follow updates in real time
Here’s what scientists have said happened beneath the earth’s surface, and what to expect next:
Where did the earthquake originate?
The epicenter was about 26 km east of the Turkish city of Nurdagi at a depth of about 18 km on the East Anatolian Fault. The quake radiated to the northeast, wreaking havoc in central Turkey and Syria.

7.8 magnitude earthquake shakes Turkey, strong aftershocks were also felt

7.8 magnitude earthquake shakes Turkey, strong aftershocks were also felt

During the 20th century, the East Anatolian Fault produced little major seismic activity. “If we were just going by the (big) earthquakes that have been recorded by seismometers, it would look more or less empty,” said Roger Musson, an honorary research fellow at the British Geological Survey.

Only three earthquakes have registered above 6.0 on the Richter scale since 1970 in the area, according to the US Geological Survey. But in 1822 a magnitude 7.0 earthquake struck the region, killing an estimated 20,000 people.

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A powerful earthquake hits Turkey and Syria

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Earthquakes hit Syria and Turkey

How bad was this earthquake?
On average, there are fewer than 20 magnitude 7.0 earthquakes a year, making Monday’s event severe.
Compared to the 6.2 magnitude earthquake that hit central Italy in 2016 and killed about 300 people, the Turkey-Syria earthquake released 250 times more energy, according to Joanna Faure Walker, head of the University College London Institute for Risk and Disaster Reduction.

Powerful earthquakes rock Turkey and Syria, relief efforts continue

Powerful earthquakes rock Turkey and Syria, relief efforts continue

Only two of the deadliest earthquakes from 2013 to 2022 were of the same magnitude as Monday’s quake.
Why was it so bad?
The East Anatolian Fault is a strike-slip fault.
In those, slabs of solid rock push against each other across a vertical fault line, building up stress until one finally slides in a horizontal motion, releasing a huge amount of tension that can trigger an earthquake.
The San Andreas Fault in California is perhaps the most famous fault in the world, with scientists warning that a catastrophic earthquake is long overdue.

The initial rupture of the Turkey-Syria earthquake started at a relatively shallow depth. “The shaking at the ground surface will have been more severe than a deeper earthquake of the same magnitude at the source,” said David Rothery, a planetary geoscientist at the Open University in Great Britain.
What kind of aftershocks can you expect?
Eleven minutes after the initial quake, the region was hit by a magnitude 6.7 aftershock. A 7.5 magnitude earthquake struck hours later, followed by another 6.0 spasm in the afternoon.

The third major earthquake measuring 6.0 hit Turkey

The third major earthquake measuring 6.0 hit Turkey

“What we’re seeing now is activity spreading to nearby faults,” Musson said. “We expect the seismicity to continue for a while.”
After the deadly event of 1822, the aftershocks continued into the following year.
What could be the final death toll?
Earthquakes of similar magnitude in populated areas have killed thousands. The 7.8 magnitude Nepal earthquake in 2015 claimed nearly 9,000 lives.
“It’s not going to go well,” Musson said. “It will be in the thousands and it could be in the tens of thousands.”

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