“Earthquake doublet”: The rare phenomenon that struck Venezuela

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Venezuela has been hit by one of the strongest seismic events in more than a century after two powerful earthquakes struck within less than a minute of each other, raising concerns over damage, casualties and ongoing aftershocks. Early reports indicate building collapses and emergency response efforts are underway in affected areas.

According to the US Geological Survey (USGS), an initial earthquake measuring 7.2 magnitude struck near San Felipe, followed approximately 40 seconds later by a stronger 7.5 magnitude quake near Yumare. Experts have described the event as a rare “earthquake doublet”.

What is a earthquake doublet?

An earthquake doublet refers to two earthquakes of similar strength occurring close together in time and location.

Unlike a standard earthquake sequence, where a major earthquake is followed by smaller aftershocks, seismic doublets involve two significant and separate earthquakes that are causally linked but remain distinct events.

USGS data suggest the two earthquakes in Venezuela may have originated from different faults and different rupture mechanisms. Scientists believe movement triggered by the first earthquake may have increased stress on nearby fault systems, potentially initiating the second event.

Immediate risks after major earthquakes

Seismologists warn that the main threat following earthquakes of this scale comes from structural collapse and damage to infrastructure.

Strong shaking can also trigger secondary hazards such as fires caused by gas pipeline failures or electrical damage. Disruptions to water networks may further complicate emergency response operations.

Authorities have also warned of continued aftershocks, some of which may still be strong enough to cause additional damage.

No link to earthquakes elsewhere

Questions emerged after other earthquakes were recorded the same day in Japan and California.

However, experts say there is no evidence connecting the events. Seismic activity in those regions occurred along separate fault systems and tectonic boundaries, meaning one event did not trigger another.

Geologists note that such earthquakes are part of natural tectonic cycles that develop over decades or even centuries.

Venezuela’s seismic vulnerability

Venezuela lies in a highly active seismic zone where the Caribbean and South American tectonic plates interact.

USGS assessments indicate that the stronger earthquake resulted from shallow strike-slip fault movement near the plate boundary. Earthquakes of this magnitude involve movement across extensive fault surfaces rather than isolated points, making them capable of causing widespread damage.

The latest earthquake in Venezuela has also revived memories of the devastating 1967 Caracas earthquake, which killed more than 200 people and caused severe destruction in the capital. Initial reports from the current event indicate that some of the same districts have again experienced structural damage.


Also read: Venezuela earthquakes kill at least 32, with 700 injured
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