EarthBrowser Open EarthBrowser

Earthquake · Tuesday, October 13, 2026

Magnitude 4.5 earthquake 18 km WNW of Río Grande, Panama

A magnitude 4.5 (light) earthquake struck 18 km WNW of Río Grande, Panama on Tuesday, October 13, 2026 at , at a depth of 10 km (shallow).

Loading the live globe…
The epicenter (largest marker, center) on EarthBrowser’s globe with the other recent earthquakes in the region. Tap a marker to open its 3D cross-section; drag to look around.
Magnitude
4.5Light
Depth
10km · shallow
Time
Epicenter
7.76° N
81.50° W
Aftershocks so far
23within 250 km
Largest aftershock
5.4M

28 days ago · USGS id us6000u21d · last revised

Open in EarthBrowser Download on theApp Store

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 4.5 means

Light earthquakes are widely felt near the epicenter, rattling windows and shelves, but rarely cause damage.

A magnitude 4.5 releases about 32 times the seismic energy of a magnitude 3.5, roughly the energy of 85 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 83 km away on Oct 9, 17:56 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
4.5 10 km 176 km 11 km ESE of Pedasí, Panama
4.4 10 km 174 km 10 km ESE of Pedasí, Panama
5.2 10 km 135 km 4 km E of La Miel, Panama
4.7 10 km 96 km 4 km SE of Pitaloza Arriba, Panama
5.0 10 km 14 km 29 km W of Río Grande, Panama
4.0 10 km 128 km 2 km S of Valle Rico, Panama
4.4 10 km 164 km 8 km W of Miramar, Panama
4.4 10 km 166 km 6 km SW of Punta Laurel, Panama
4.0 10 km 102 km 2 km N of El Cortezo, Panama
4.5 10 km 101 km 10 km S of La Mesa, Panama
4.5 10 km 225 km 215 km S of Burica, Panama
5.4 10 km 210 km 210 km S of Burica, Panama
4.5 10 km 20 km 2 km S of Río Grande, Panama
4.1 10 km 42 km 0 km SSW of Leones Arriba, Panama
4.4 10 km 154 km 14 km ESE of Cañas, Panama
4.2 10 km 131 km 1 km WSW of Nuario, Panama
4.6 10 km 60 km 7 km S of Tebario, Panama
4.4 10 km 29 km 8 km SSE of Guarumal, Panama
4.4 10 km 61 km 12 km S of Tebario, Panama
4.5 10 km 160 km 13 km SSE of Los Asientos, Panama
4.7 10 km 99 km 8 km SE of Pitaloza Arriba, Panama
4.2 10 km 146 km 1 km NNE of Oria Arriba, Panama
4.4 10 km 107 km 2 km S of Cedro Arriba, Panama
before 4.6 10 km 13 km 12 km NW of Río Grande, Panama
before 4.4 10 km 173 km 13 km SSE of Pedasí, Panama
before 4.6 10 km 21 km 14 km SW of Zapotillo, Panama
before 4.3 10 km 58 km 7 km S of Tebario, Panama
before 4.7 10 km 106 km 6 km S of Llano de Piedra, Panama
before 4.4 10 km 154 km 6 km WNW of Chiriquí Grande, Panama
before 4.6 10 km 1 km 18 km WNW of Río Grande, 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.

More live views