Vibrations from Monday’s deadly earthquake in Turkey traveled almost 7,200 miles to Tucson in just 14 minutes and 10 seconds.
The unmistakable signal from the magnitude-7.8 quake was recorded by the U.S. Geological Survey’s seismic station at the base of Catalina Mountains near Sabino Canyon.
“We have a nice record of that in Tucson,” said seismologist Susan Beck, a professor and director of the graduate program at the University of Arizona’s Department of Geosciences.
But there’s nothing nice about the death and destruction caused by the quake and its aftershocks, Beck said.
The “terrible, terrible devastation” in Turkey and Syria is especially hard to watch because she has spent time in the region and gotten to know some of the people living there, she said. “I’ve been in many of the towns that they’re talking about on the news right now.”
From 2011-18, Beck was part of a team studying the tectonic forces at work in south central Turkey. They deployed about 65 seismic stations on and around the same East Anatolian Fault that ruptured on Monday, killing thousands of people and displacing tens of thousands more, including many already left homeless by the Syrian civil war.
All of Turkey sits in a seismically active region where the Eurasian, African and Arabian tectonic plates collide.
The documented history of deadly earthquakes there stretches back to the year 17 A.D. and includes a 1939 quake that killed nearly 33,000 people and a 1999 quake that killed more than 17,000.
That’s what makes it such an important place for scientists to study and try to understand, Beck said. “My colleagues and I are still working with the seismic data we collected.”
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