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Earthquake · Tuesday, October 20, 2026

Magnitude 5.4 earthquake 192 km S of Burica, Panama

A magnitude 5.4 (moderate) earthquake struck 192 km S of Burica, Panama on Tuesday, October 20, 2026 at , at a depth of 10 km (shallow).

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Magnitude
5.4Moderate
Depth
10km · shallow
Time
Epicenter
6.32° N
82.57° W
Aftershocks so far
3within 250 km
Largest aftershock
5.0M

20 days ago · USGS id us6000u3nl · last revised

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The full globe opens the 3D cross-section: the hypocenter at depth, the plate boundary and subducting slab where there is one, the aftershock sequence as it grows, and the sea floor around an offshore epicenter.

What a magnitude 5.4 means

Moderate earthquakes are felt by everyone nearby and can cause minor to moderate damage close to the epicenter, mostly to weaker structures.

A magnitude 5.4 releases about 32 times the seismic energy of a magnitude 4.4, roughly the energy of 2 thousand tonnes of TNT. Magnitude measures the energy released at the source; how hard the ground shook at any one place depends on distance, depth and local geology, and is reported separately as intensity.

Shallow earthquakes (under 70 km) release their energy close to the surface, so shaking is stronger and more damaging near the epicenter than for a deeper quake of the same size.

Nearby earthquakes and aftershocks

This event is part of a sequence: a larger magnitude 7.7 struck 243 km away on Oct 9, 17:56 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
5.0 10 km 188 km 27 km W of Río Grande, Panama
4.0 10 km 248 km 2 km N of El Cortezo, Panama
5.0 10 km 192 km south of Panama
before 4.1 10 km 224 km 2 km S of Leones Arriba, Panama
before 4.6 10 km 230 km 12 km SSE of Tebario, Panama
before 4.4 10 km 214 km 8 km SSE of Guarumal, Panama
before 4.4 10 km 229 km 12 km SSE of Tebario, Panama
before 4.7 10 km 203 km 14 km WNW of Río Grande, Panama
before 4.8 10 km 195 km 21 km W of Río Grande, Panama
before 6.1 10 km 194 km 18 km W of Río Grande, Panama
before 4.5 10 km 218 km 7 km WSW of Calidonia, Panama
before 4.5 10 km 204 km 19 km SW of Calidonia, Panama
before 4.8 10 km 191 km 25 km W of Río Grande, Panama
before 4.3 10 km 248 km 6 km NNW of El Cortezo, Panama
before 4.5 10 km 238 km 7 km ESE of Tebario, Panama
before 4.8 10 km 186 km 31 km W of Río Grande, Panama
before 4.6 10 km 205 km 18 km WNW of Río Grande, Panama
before 4.8 10 km 225 km 11 km SSW of Tebario, Panama
before 4.3 10 km 231 km 3 km SSW of Tebario, Panama
before 4.8 10 km 211 km 4 km NE of Río Grande, Panama
before 4.4 10 km 188 km 21 km SSW of Río Grande, Panama
before 4.5 10 km 202 km 18 km SSE of Río Grande, Panama
before 4.6 10 km 200 km 10 km S of Río Grande, Panama
before 4.9 10 km 197 km 9 km SW of Río Grande, Panama
before 4.6 10 km 211 km 4 km NNE of Río Grande, Panama
before 4.9 10 km 199 km 13 km W of Río Grande, Panama
before 6.6 10 km 197 km 14 km W of Río Grande, Panama
before 4.9 10 km 223 km 12 km SSW of Tebario, Panama
before 5.2 10 km 205 km 11 km SE of Río Grande, Panama
before 4.8 26 km 221 km 14 km SSW of Tebario, Panama

Frequently asked questions

How is earthquake magnitude measured?

Modern magnitudes are moment magnitudes (Mw), computed from the seismic moment: the area of the fault that slipped, how far it slipped and the rigidity of the rock. Each whole step up the scale is about 32 times more energy, so a magnitude 7 releases roughly a thousand times the energy of a magnitude 5.

What is the difference between magnitude and intensity?

Magnitude is one number for the whole earthquake, describing the energy released at the source. Intensity describes the shaking at a particular place, on the Modified Mercalli scale from I (not felt) to X+ (extreme), and falls off with distance from the epicenter.

What is an aftershock?

An aftershock is a smaller earthquake in the same area after a larger one, as the crust around the ruptured fault adjusts to the new stresses. They are most frequent in the first hours and days and fade over weeks to months, though a large mainshock can produce aftershocks for years.

Why do the magnitude and location change?

The first solution uses the nearest stations only. As recordings arrive from more seismographs around the world, USGS revises the magnitude, depth and epicenter, sometimes several times in the first hours. This page reflects the latest revision.

Where does this earthquake data come from?

From the U.S. Geological Survey’s real-time earthquake feeds, which combine the USGS National Earthquake Information Center with regional seismic networks worldwide. EarthBrowser ingests the feed every minute.

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