
A magnitude 7.4 earthquake struck western Colombia on Monday, shaking Ecuador and Panama. Injuries were reported in Quibdó; Pereira and Manizales sustained structural damage.
A magnitude 7.4 earthquake hit western Colombia on Monday morning, swaying buildings from Bogotá to Quito and triggering evacuations in three countries, the Colombian Geological Service, or SGC, reported.
The quake struck at 7:34 a.m. local time at a depth of between 51 and 66 miles. That depth, according to the SGC, reduced the intensity of surface shaking but still produced prolonged shaking across a wide area. The epicenter lay near the municipality of San José del Palmar in the western Chocó department.
Structural damage was reported in several Colombian cities. In Pereira, Risaralda Gov. Juan Diego Patiño Ochoa said homes and businesses suffered “severe damage,” including major structural failures, extensive cracking and collapsed sections of building facades. Matecaña International Airport sustained damage, he added. Video posted on social media showed at least one building partially collapsed in Pereira.
In Quibdó, the capital of Chocó, Gov. Nubia Carolina Córdoba confirmed that falling masonry and pieces of building facades injured several people. Debris fell from one of the towers of Manizales’ landmark cathedral, the newspaper El Tiempo reported. National authorities had not immediately confirmed any deaths.
The earthquake was felt across central and western Colombia, including Medellín, Cali, Popayán, Armenia and Bogotá. In Ecuador, the interruption came on the national holiday commemorating the First Cry of Independence. Residents in the provinces of Carchi, Pichincha, Guayas and Esmeraldas reported prolonged shaking, and major hospitals in Quito evacuated patients as a precaution. Panama’s National Civil Protection System said the earthquake was felt lightly in Panama City and Darién province, with no structural damage reported.
Emergency crews continued surveying rural areas near the epicenter as geological authorities warned of possible aftershocks.
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