Two earthquakes struck Costa Rica early Monday morning, including a magnitude 5.4 quake followed shortly by a strong aftershock [1], [2].

The events caused widespread panic across the country, particularly in densely populated urban centers. Because the tremors occurred during the early morning hours, many residents were awakened by the shaking, highlighting the region's ongoing vulnerability to seismic activity.

The primary earthquake measured 5.4 in magnitude [1]. While some reports indicated a magnitude of 5.3 [3], the higher estimate of 5.4 is widely cited by regional financial and news outlets [1], [4]. The tremor was felt most intensely in the Central Valley and the San José area [2], [4].

Just two minutes after the initial quake, a second tremor struck the region [2], [3]. This aftershock was measured at magnitude 4.8 [1], [3]. The rapid succession of the two events intensified the alarm among the local population, as residents had little time to recover from the first shock before the second began.

Local authorities and residents reported significant panic throughout the Central Valley [3], [5]. Despite the strength of the tremors and the fear they induced, there have been zero reported injuries [3].

Videos circulating on social media and news platforms show the impact of the shaking in residential areas [1], [5]. The tremors occurred on Monday, Aug. 24 [3], [5]. Authorities said they continue to monitor the region for further seismic activity as the population remains on alert.

A magnitude 5.4 earthquake followed two minutes later by a magnitude 4.8 aftershock.

Costa Rica is situated on the Pacific Ring of Fire, making it prone to frequent seismic activity. The occurrence of a significant aftershock only two minutes after a magnitude 5.4 event demonstrates the volatility of the local fault systems. While the lack of injuries in this instance suggests effective building standards or a lack of structural collapse, the panic reported in the Central Valley underscores the psychological impact of sudden seismic events in high-density areas.