The displacement occurred at exactly **00:22:50 UTC**, sending ripples through the local geological infrastructure.
At the time of the event, the region was blanketed by overcast clouds with a steady temperature of 17.3°C recorded at local weather stations.
Urban centers near the epicenter experienced brief shaking, though the muted atmospheric conditions provided a somber backdrop to the late-night event.
Geological Analysis
The tremor originated within a high-seismicity zone defined by the subduction of the Cocos Plate beneath the Caribbean and North American plates.
Scientific sensors indicate the **4.9** magnitude rupture reflects typical crustal stress release common to this complex transboundary fault system.
Seismologists noted that the depth of the event was consistent with regional subduction patterns.
Monitoring stations continue to track the area following the **00:22:50 UTC** event to assess any potential for significant aftershocks.
Our editorial team carefully monitors seismic data to provide in-depth analysis. Explore our real-time interactive Live Map for more details.