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Earthquake · Friday, October 9, 2026

Magnitude 3.3 earthquake 56 km SE of Boca de Yuma, Dominican Republic

A magnitude 3.3 (minor) earthquake struck 56 km SE of Boca de Yuma, Dominican Republic on Friday, October 9, 2026 at , at a depth of 60 km (shallow).

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Magnitude
3.3Minor
Depth
60km · shallow
Time
Epicenter
18.02° N
68.23° W
Aftershocks so far
0within 250 km
Largest aftershock
—

31 days ago · USGS id pr71536213 · 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 3.3 means

Minor earthquakes are often felt by people nearby but almost never cause damage.

A magnitude 3.3 releases about 27 times the seismic energy of a magnitude 2.3, roughly the energy of 1 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 4.8 struck 137 km away on Sep 18, 13:19 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.6 16 km 148 km 2 km SSE of Yauco, Puerto Rico
before 2.7 35 km 119 km 74 km NE of Punta Cana, Dominican Republic
before 3.4 25 km 137 km 87 km NE of Punta Cana, Dominican Republic
before 2.3 7 km 138 km 6 km SSW of Guánica, Puerto Rico
before 2.2 8 km 138 km 3 km SW of Guánica, Puerto Rico
before 2.5 7 km 136 km 3 km WSW of Fuig, Puerto Rico
before 2.3 24 km 122 km 1 km NNW of Sabana Eneas, Puerto Rico
before 2.2 15 km 139 km 1 km NW of Guánica, Puerto Rico
before 2.4 11 km 148 km 2 km SW of Indios, Puerto Rico
before 3.0 8 km 136 km 4 km WSW of Guánica, Puerto Rico
before 3.1 35 km 61 km 77 km S of Boca de Yuma, Dominican Republic
before 2.4 2 km 142 km 3 km SSE of Guánica, Puerto Rico
before 3.0 14 km 173 km 6 km SSE of Ponce, Puerto Rico
before 2.1 7 km 136 km 4 km SW of Fuig, Puerto Rico
before 2.0 5 km 136 km 3 km WNW of Fuig, Puerto Rico
before 3.1 11 km 242 km 75 km N of Brenas, Puerto Rico
before 2.0 9 km 138 km 4 km SW of Guánica, Puerto Rico
before 2.5 7 km 136 km 3 km WSW of Fuig, Puerto Rico
before 2.3 8 km 135 km 4 km WSW of Fuig, Puerto Rico
before 2.6 9 km 137 km 4 km SW of Guánica, Puerto Rico
before 2.4 9 km 136 km 4 km WSW of Guánica, Puerto Rico
before 2.5 17 km 151 km 11 km N of Quebradillas, Puerto Rico
before 1.8 8 km 139 km 7 km SSW of Guánica, Puerto Rico
before 2.2 7 km 136 km 3 km W of Fuig, Puerto Rico
before 2.8 8 km 138 km 2 km SW of Fuig, Puerto Rico
before 2.4 5 km 135 km 4 km W of Fuig, Puerto Rico
before 1.9 6 km 137 km 2 km WNW of Fuig, Puerto Rico
before 2.2 6 km 136 km 4 km WSW of Guánica, Puerto Rico
before 2.1 8 km 138 km 2 km W of Guánica, Puerto Rico
before 1.8 7 km 134 km 6 km WSW of Fuig, Puerto Rico

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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