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Earthquake · Saturday, October 31, 2026

Magnitude 3.2 earthquake 60 km ESE of Boca de Yuma, Dominican Republic

A magnitude 3.2 (minor) earthquake struck 60 km ESE of Boca de Yuma, Dominican Republic on Saturday, October 31, 2026 at , at a depth of 76 km (intermediate).

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Magnitude
3.2Minor
Depth
76km · intermediate
Time
Epicenter
18.08° N
68.13° W
Aftershocks so far
0within 250 km
Largest aftershock
—

9 days ago · USGS id pr71538018 · 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 3.2 means

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

A magnitude 3.2 releases about 33 times the seismic energy of a magnitude 2.2, 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.

Intermediate-depth earthquakes (70 to 300 km) occur inside subducting slabs. The extra distance to the surface spreads the shaking over a wider area at lower intensity.

Nearby earthquakes and aftershocks

This event is part of a sequence: a larger magnitude 3.9 struck 82 km away on Oct 3, 10:35 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 3.2 33 km 104 km 77 km ENE of Punta Cana, Dominican Republic
before 1.8 13 km 147 km 3 km W of Tallaboa, Puerto Rico
before 1.9 9 km 126 km 4 km WSW of Guánica, Puerto Rico
before 2.0 6 km 126 km 4 km WSW of Guánica, Puerto Rico
before 2.1 10 km 135 km 8 km SSE of Maria Antonia, Puerto Rico
before 2.1 11 km 128 km 0 km WSW of Fuig, Puerto Rico
before 1.9 8 km 140 km 4 km NNW of Guayanilla, Puerto Rico
before 2.3 13 km 136 km 5 km SE of Maria Antonia, Puerto Rico
before 3.3 26 km 214 km 53 km N of Brenas, Puerto Rico
before 2.8 8 km 128 km 1 km W of Fuig, Puerto Rico
before 2.6 14 km 145 km 24 km SSE of Maria Antonia, Puerto Rico
before 2.2 11 km 126 km 2 km WNW of Fuig, Puerto Rico
before 1.8 14 km 139 km 2 km WSW of Guayanilla, Puerto Rico
before 1.3 12 km 117 km 3 km NE of La Parguera, Puerto Rico
before 2.0 16 km 138 km 1 km SW of Indios, Puerto Rico
before 2.0 8 km 131 km 8 km S of Guánica, Puerto Rico
before 2.9 6 km 76 km 25 km WNW of Puerto Real, Puerto Rico
before 2.7 10 km 175 km 61 km NNE of Miches, Dominican Republic
before 1.9 14 km 196 km 2 km NNW of Aibonito, Puerto Rico
before 2.6 35 km 109 km 56 km NNE of Punta Cana, Dominican Republic
before 2.2 14 km 162 km 6 km SSE of Ponce, Puerto Rico
before 2.1 14 km 136 km 5 km SE of Maria Antonia, Puerto Rico
before 2.2 8 km 127 km 4 km SW of Guánica, Puerto Rico
before 2.0 6 km 129 km 1 km WSW of Guánica, Puerto Rico
before 2.7 13 km 162 km 7 km SSE of Ponce, Puerto Rico
before 2.4 15 km 162 km 6 km SSE of Ponce, Puerto Rico
before 2.4 13 km 162 km 7 km SSE of Ponce, Puerto Rico
before 2.3 14 km 163 km 7 km SSE of Ponce, Puerto Rico
before 2.3 14 km 162 km 7 km SSE of Ponce, Puerto Rico
before 2.4 8 km 125 km 5 km WSW of Guánica, 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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