Were Mexico’s Recent Earthquakes Related?

Over the past two weeks, Mexico has experienced a lot of shaking.

On Sept. 8, a magnitude-8.1 earthquake struck 54 miles (87 kilometers) southwest of Pijijiapan, which sits just above the Mexico-Guatemala border. Eleven days later, a magnitude-7.1 quake struck 3 miles (5 km) east of Raboso, near Mexico City. And today (Sept. 21), another quake — a magnitude 4.8 — hit just outside Pijijiapan.

While Mexico’s position along major tectonic fault lines makes it a hotbed of seismic activity, the frequency of these powerful earthquakes begs the question: Are these quakes happening more often? [The 10 Biggest Earthquakes in History]

Not likely, said Gavin Hayes, a research geophysicist at the U.S. Geological Survey’s National Earthquake Information Center.

“Mexico is very prone to earthquakes,” he said, “so earthquakes of this size in Mexico are not unusual. Getting two in a row of this size so close together is unusual but not unexpected.”

In the grand, slow-moving world of tectonic plates, Mexico is situated at an unfortunate location: It rests at the southern edge of the North American Plate, putting it right at the point where it meets the Pacific Plate, the Cocos Plate and the Caribbean Plate.

The quakes occur because all of these plates are moving in different directions, and as they collide or rub against each other, this movement can unleash destructive forces. While these tectonic events usually occur along coastlines, like near Pijijiapan, the Cocos Plate has a unique conformation that explains why so many earthquakes are hitting Mexico City, which lies farther inland, according to the U.S. Geological Survey (USGS).

Mexico has been hit by several moderate earthquakes in the past week, but the one that struck Mexico City was several orders of magnitude stronger. USGS

While the North American landmass is slowly moving west, the Cocos Plate is traveling northeast. As they push against each other, the Cocos Plate, which carries the seafloor and is denser than plates carrying land, is forced underneath, into the Earth’s mantle, according to the USGS.

But Hayes said that although most of these above-below collisions, called subduction zones, involve one point of descent, the Cocos Plate sinks a bit and then flattens out for a long expanse before it begins to sink again. Because the location at which it sinks is spread out, the resulting earthquakes often occur farther inland than they would at a typical subduction zone.

“I think this perhaps facilitated the…

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