At 18:04 local time on a Wednesday national holiday, two powerful earthquakes struck seconds apart near Venezuela’s capital, Caracas, collapsing buildings and killing at least 235 people. Rescuers are digging through rubble in a race to find survivors, but officials fear the death toll could rise to thousands, with around 40,000 people reported missing and at least 4,300 injured.
Earthquakes happen when tectonic plates – the giant slabs of rock that make up the Earth’s crust – suddenly slip past each other along a fault line. The energy released travels in waves, shaking the ground. The severity of damage depends on magnitude, depth, and local building quality. The first quake registered 7.2 on the Richter scale; a second, stronger one of 7.5 followed less than 40 seconds later. Both were shallow – the first 20.3km below the surface, the second at just 10km – making the shaking more violent at ground level. The second quake was the strongest to hit Venezuela since 1900, according to Channel 4 News.
“Why two shallow quakes seconds apart killed at least 235 and left thousands missing in Venezuela.”
Venezuela lies on the Caribbean plate boundary, where the South American and Caribbean plates meet. The US Geological Survey (USGS) warned there was a 44 per cent probability that fatalities could exceed 10,000. The worst damage occurred along the northern coast near La Guaira and Catia La Mar, where a 10‑storey hotel was reduced to rubble. In Caracas, the Altamira and Los Palos Grandes neighbourhoods saw multiple building collapses. The Simón Bolívar international airport was badly damaged, hampering initial relief efforts. Acting President Delcy Rodríguez declared a state of emergency and appealed for international help.
For UK readers, the disaster matters for several reasons. First, it highlights the devastating human cost of earthquakes in densely populated urban areas – a risk that exists in many parts of the world, including the UK (though British earthquakes are usually too small to cause such destruction). Second, the UK government may contribute to international aid efforts; the US has already pledged $150 million and military transport for search‑and‑rescue. Third, thousands of British‑Venezuelan dual nationals live in the affected region, and the Foreign Office may issue travel advice. Finally, understanding why shallow, double shocks are so destructive can help people in earthquake‑prone zones prepare.
Q: What is an earthquake and why are shallow earthquakes more dangerous? An earthquake is the sudden shaking of the ground caused by the release of stress along a fault line. A shallow earthquake (less than 70 km deep) concentrates energy near the surface, causing stronger shaking and more damage to buildings than deeper ones.
Q: How did two earthquakes happen in less than a minute? The first 7.2‑magnitude quake may have triggered the second, even larger 7.5‑magnitude event on a nearby fault segment. This phenomenon, called an earthquake doublet, is relatively rare but can cause prolonged destruction, as each tremor compounds the damage.
Q: Why was the death toll so high in Venezuela? Several factors combined: the quakes struck on a public holiday, so many people were at home in poorly constructed buildings; the shallow depths intensified shaking; and the 40‑second gap meant few could escape between shocks. Many structures were not designed to withstand such force.
What happens next depends on the coming hours. The US and other countries are sending search‑and‑rescue teams, with the US military deploying transport ships and aircraft. The UN’s humanitarian agency has pledged to “surge in search and rescue support”. Rescuers are working through the “golden 72 hours” – the critical window to find survivors under rubble. Authorities will also need to house tens of thousands of homeless people and rebuild damaged infrastructure. Aftershocks continue, and many residents are too afraid to return to damaged buildings, sleeping in parks and squares.