A magnitude-7.4 earthquake [1] struck western Colombia on Monday, killing at least 111 people [2] and destroying numerous buildings.
The disaster highlights the extreme vulnerability of Andean urban centers to tectonic activity, where steep terrain and aging infrastructure can amplify the lethality of seismic events.
The quake caused widespread destruction across western Colombia, with the cities of Manizales, Cali, and Pereira [4] reported as the hardest hit. In Manizales, the shaking damaged hundreds of buildings [2]. Reports said the quake toppled a cathedral tower in the city [5], while other video footage captured a building collapse near the Catholic University [5].
Death toll estimates vary among reporting agencies. While some reports said at least 47 deaths [5], other sources said the toll has reached at least 111 [2]. Rescue teams have worked to locate survivors trapped beneath the rubble of collapsed structures [2].
The tremors were not limited to Colombia. The earthquake was felt in neighboring Panama, Venezuela, and Ecuador [3]. Experts said the event was due to tectonic activity along the Andes [1], a region known for significant seismic volatility.
Local authorities continue to assess the full extent of the damage. The collapse of high-profile landmarks and university-adjacent buildings has complicated rescue efforts in densely populated areas of Manizales [5].
“A magnitude-7.4 earthquake struck western Colombia on Monday, killing at least 111 people.”
This event underscores the persistent risk posed by the Nazca and South American plate boundaries. The disparity in death toll reporting suggests a chaotic early recovery phase, while the collapse of significant structures like the cathedral tower indicates that even prominent landmarks in the region may not meet modern seismic resilience standards.
