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Earthquake · Tuesday, November 10, 2026

Magnitude 3.4 earthquake 11 km NE of Boca de Yuma, Dominican Republic

A magnitude 3.4 (minor) earthquake struck 11 km NE of Boca de Yuma, Dominican Republic on Tuesday, November 10, 2026 at , at a depth of 52 km (shallow).

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Magnitude
3.4Minor
Depth
52km · shallow
Time
Epicenter
18.45° N
68.52° W
Aftershocks so far
0within 250 km
Largest aftershock
—

4 days ago · USGS id pr71538948 · 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 3.4 means

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

A magnitude 3.4 releases about 33 times the seismic energy of a magnitude 2.4, roughly the energy of 2 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 3.9 struck 39 km away on Oct 13, 15:55 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.5 33 km 221 km 25 km N of Tierras Nuevas Poniente, Puerto Rico
before 2.0 14 km 233 km 15 km S of Santa Isabel, Puerto Rico
before 2.0 16 km 234 km 13 km S of Santa Isabel, Puerto Rico
before 2.2 13 km 233 km 14 km S of Santa Isabel, Puerto Rico
before 1.9 11 km 186 km 6 km SE of Maria Antonia, Puerto Rico
before 1.7 15 km 148 km 2 km W of Cabo Rojo, Puerto Rico
before 2.5 12 km 231 km 10 km S of Santa Isabel, Puerto Rico
before 2.3 14 km 233 km 15 km S of Santa Isabel, Puerto Rico
before 3.5 28 km 167 km 104 km NNW of San Antonio, Puerto Rico
before 1.7 11 km 230 km 9 km SSW of Santa Isabel, Puerto Rico
before 2.0 11 km 232 km 8 km S of Santa Isabel, Puerto Rico
before 3.3 14 km 232 km 10 km S of Santa Isabel, Puerto Rico
before 2.2 14 km 182 km 5 km SSE of Guánica, Puerto Rico
before 2.3 13 km 186 km 9 km SSE of Maria Antonia, Puerto Rico
before 2.3 9 km 187 km 11 km SSE of Maria Antonia, Puerto Rico
before 2.4 11 km 187 km 9 km SSE of Maria Antonia, Puerto Rico
before 1.8 16 km 182 km 3 km S of Maria Antonia, Puerto Rico
before 2.8 68 km 221 km 18 km NNE of Tierras Nuevas Poniente, Puerto Rico
before 3.1 15 km 183 km 4 km SSE of Maria Antonia, Puerto Rico
before 1.7 10 km 173 km 4 km W of Fuig, Puerto Rico
before 2.1 14 km 187 km 0 km SE of Indios, Puerto Rico
before 2.0 16 km 187 km 0 km SSW of Indios, Puerto Rico
before 3.2 76 km 58 km 60 km ESE of Boca de Yuma, Dominican Republic
before 2.1 15 km 185 km 2 km WNW of Indios, Puerto Rico
before 1.9 15 km 186 km 1 km NNW of Indios, Puerto Rico
before 3.0 8 km 132 km 45 km NNW of San Antonio, Puerto Rico
before 2.1 15 km 183 km 2 km S of Yauco, Puerto Rico
before 2.1 15 km 186 km 1 km W of Indios, Puerto Rico
before 3.9 83 km 35 km 26 km S of Boca de Yuma, Dominican Republic
before 3.4 10 km 160 km 31 km N of Isabela, 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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