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A magnitude 6.0 earthquake struck 7 km north of La Tronosa, Panama at 04:14 UTC on 10th October 2026, according to the USGS. The quake occurred at a shallow depth of 10 km, making it capable of producing strong local shaking and noticeable ground movement across nearby provinces.
The USGS classified the event with a YELLOW PAGER alert, indicating limited casualties but the possibility of moderate damage to vulnerable structures.
Shallow earthquakes (0–20 km) typically generate stronger surface shaking, increasing the risk of structural damage.
At least 38 felt reports were submitted, mainly from western Panama, including Bocas del Toro and Cockley provinces. Residents described sharp jolts and short bursts of shaking.
Nearby areas most likely affected include:
The region experienced 48 possible foreshocks in the days leading up to the main event and 18 possible aftershocks within the following week. These smaller quakes are common in active tectonic zones and indicate ongoing stress adjustments along the fault.
Panama lies along the Cocos–Caribbean Plate boundary, one of the most active seismic zones in Central America. The earthquake occurred within the Limón–Panama deformation zone, where the Cocos Plate subducts beneath the Caribbean Plate at roughly 10 cm per year.
This region has a history of significant earthquakes, including:
The magnitude 6.0 rupture released an estimated 1.9 × 10¹⁸ joules of seismic energy — roughly equivalent to 450 kilotons of TNT. This level of energy is about 200 times stronger than a magnitude 5.0 earthquake.
Older masonry buildings and unreinforced concrete structures in rural western Panama are most vulnerable to shaking of this intensity.
The broader Los Santos region has experienced major earthquakes before, including a magnitude 7.0 event in 1943.
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