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Earthquake · Saturday, October 31, 2026

Magnitude 3.8 earthquake 92 km NE of Cruz Bay, U.S. Virgin Islands

A magnitude 3.8 (minor) earthquake struck 92 km NE of Cruz Bay, U.S. Virgin Islands on Saturday, October 31, 2026 at , at a depth of 20 km (shallow).

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Magnitude
3.8Minor
Depth
20km · shallow
Time
Epicenter
18.97° N
64.23° W
Aftershocks so far
15within 250 km
Largest aftershock
3.4M

9 days ago · USGS id pr2026304000 · 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 3.8 means

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

A magnitude 3.8 releases about 29 times the seismic energy of a magnitude 2.8, roughly the energy of 7 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 4.7 struck 230 km away on Oct 18, 15:35 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
2.8 27 km 74 km 75 km N of Charlotte Amalie, U.S. Virgin Islands
2.2 14 km 247 km 1 km WNW of Mariano Colón, Puerto Rico
3.4 22 km 4 km 88 km NE of Cruz Bay, U.S. Virgin Islands
3.4 47 km 115 km 126 km NNW of Charlotte Amalie, U.S. Virgin Islands
3.1 71 km 135 km 33 km NNW of Culebra, Puerto Rico
2.7 53 km 135 km 46 km NNE of Luquillo, Puerto Rico
3.1 60 km 132 km 62 km NNE of Luquillo, Puerto Rico
2.9 44 km 88 km 37 km N of Charlotte Amalie, U.S. Virgin Islands
2.7 42 km 90 km 20 km N of Charlotte Amalie, U.S. Virgin Islands
2.8 35 km 245 km 3 km WNW of Orocovis, Puerto Rico
2.2 11 km 201 km 7 km ESE of Emajagua, Puerto Rico
2.5 33 km 235 km 25 km N of Tierras Nuevas Poniente, Puerto Rico
3.2 19 km 86 km 77 km N of Charlotte Amalie, U.S. Virgin Islands
2.7 3 km 49 km 44 km NE of Cruz Bay, U.S. Virgin Islands
2.8 68 km 236 km 18 km NNE of Tierras Nuevas Poniente, Puerto Rico
before 3.4 58 km 69 km 120 km N of Cruz Bay, U.S. Virgin Islands
before 3.2 34 km 87 km 36 km N of Charlotte Amalie, U.S. Virgin Islands
before 2.9 17 km 164 km 22 km SE of Esperanza, Puerto Rico
before 2.6 13 km 135 km 23 km NNW of Saint Croix, U.S. Virgin Islands
before 2.5 34 km 157 km 10 km ESE of Esperanza, Puerto Rico
before 3.3 14 km 60 km 56 km N of Cruz Bay, U.S. Virgin Islands
before 2.4 30 km 162 km 16 km SE of Esperanza, Puerto Rico
before 4.1 25 km 163 km 21 km SE of Esperanza, Puerto Rico
before 3.8 33 km 163 km 21 km SE of Esperanza, Puerto Rico
before 2.8 36 km 39 km 64 km NNE of Cruz Bay, U.S. Virgin Islands
before 3.0 36 km 166 km 49 km N of Suárez, Puerto Rico
before 2.7 45 km 166 km 53 km N of Suárez, Puerto Rico
before 3.0 31 km 195 km 66 km N of San Juan, Puerto Rico
before 3.3 8 km 25 km 69 km NE of Cruz Bay, U.S. Virgin Islands
before 3.1 121 km 92 km 39 km ESE of Cruz Bay, U.S. Virgin Islands

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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