What changed
A magnitude-7.7 earthquake struck south-central Panama shortly before 15:00 local time on 9 October, damaging buildings and causing widespread shaking. Its epicentre was about 10km from Pitaloza Arriba, at a shallow depth of 12km. About 4.6 million people experienced moderate to severe tremors; no casualties have been reported so far.
Buildings or parts of buildings collapsed in Penonomé and Soná, including a cathedral wall and spire and a local hotel. Residents in Panama City evacuated buildings, while several large aftershocks complicated the response.
Why it matters
The shallow depth helps explain why the quake was felt so widely and why buildings were damaged far from the epicentre. In Las Minas, resident Ricardo Brown said cracks had appeared in several homes and that he and his wife feared their house could collapse.
The immediate picture is serious but incomplete. Panama’s government has mobilised, and authorities are still assessing damaged structures. The uncertainty matters because aftershocks can turn already weakened buildings into fresh hazards.
Panama City, roughly 200km away, appears to have suffered limited damage from falling roof debris. The Panama Canal was unaffected, according to the authority overseeing marine traffic, preserving the operation of a vital link between the Atlantic and Pacific.
Tsunami warnings issued for 11 neighbouring countries were later withdrawn after the US Tsunami Warning System confirmed there was no threat. A national earthquake evacuation drill had been scheduled for three days after the quake, giving the government an unusually immediate test of its emergency planning.
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