A magnitude 7.4 earthquake struck western Colombia on Monday morning, killing at least 20 people [1, 2] and triggering mass evacuations [1, 3].

The disaster highlights the extreme vulnerability of Andean urban centers to seismic activity. Because the tremor was felt across national borders, it underscores the regional risk posed by the Pacific-South American plate boundary [2, 4].

The epicentre was reported in San José del Palmar [2, 4]. While the strongest shaking occurred in western Colombia, the tremor was felt as far away as Bogotá and in neighboring Ecuador [1, 2].

In Bogotá, residents evacuated homes and office buildings as the ground shook [1, 2]. Emergency responders moved into affected areas to assist evacuees and assess structural damage to city infrastructure [1].

Reports on the strength of the quake varied slightly between agencies. While some reports indicated a magnitude of 6.7 [4], other data confirmed a magnitude of 7.4 [2].

Casualties have reached at least 20 deaths [2]. Local authorities continue to search for survivors among the debris in the hardest-hit regions of western Colombia [1, 3].

Tectonic activity on the plate boundary caused the shift [2, 4]. This region remains one of the most seismically active zones in South America due to the ongoing subduction of the Nazca plate beneath the South American plate.

A magnitude 7.4 earthquake struck western Colombia on Monday morning.

The scale of this event demonstrates the persistent threat posed by the Pacific-South American plate boundary. The fact that a quake centered in San José del Palmar caused significant panic and evacuations in Bogotá suggests that existing building codes and emergency protocols in major Colombian cities will face renewed scrutiny to prevent higher casualty rates in future events.