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Earthquake · Sunday, October 18, 2026

Magnitude 4.7 earthquake 20 km SW of Sandy Point Town, Saint Kitts and Nevis

A magnitude 4.7 (light) earthquake struck 20 km SW of Sandy Point Town, Saint Kitts and Nevis on Sunday, October 18, 2026 at , at a depth of 150 km (intermediate).

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Magnitude
4.7Light
Depth
150km · intermediate
Time
Epicenter
17.25° N
63.01° W
Aftershocks so far
11within 250 km
Largest aftershock
3.8M

22 days ago · USGS id us6000u36d · 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 4.7 means

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

A magnitude 4.7 releases about 32 times the seismic energy of a magnitude 3.7, roughly the energy of 169 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

11 aftershocks and 14 earlier earthquakes within 250 km in the 30 days around this event. Aftershock rates fall off quickly in the first days (Omori's law); the largest aftershock is typically about one magnitude unit smaller than the mainshock (Båth's law), here around magnitude 3.5.

Time (UTC)MagnitudeDepthDistanceLocation
3.4 22 km 231 km 88 km NE of Cruz Bay, U.S. Virgin Islands
2.7 42 km 249 km 20 km N of Charlotte Amalie, U.S. Virgin Islands
2.7 3 km 219 km 44 km NE of Cruz Bay, U.S. Virgin Islands
3.8 20 km 230 km 92 km NE of Cruz Bay, U.S. Virgin Islands
2.6 13 km 210 km 23 km NNW of Saint Croix, U.S. Virgin Islands
2.8 36 km 246 km 64 km NNE of Cruz Bay, U.S. Virgin Islands
3.3 8 km 232 km 69 km NE of Cruz Bay, U.S. Virgin Islands
3.1 121 km 184 km 39 km ESE of Cruz Bay, U.S. Virgin Islands
3.4 13 km 143 km 85 km ENE of Christiansted, U.S. Virgin Islands
3.4 34 km 243 km 117 km NE of Cruz Bay, U.S. Virgin Islands
2.9 14 km 229 km 45 km NNE of Cruz Bay, U.S. Virgin Islands
before 2.9 18 km 170 km 61 km E of Cruz Bay, U.S. Virgin Islands
before 2.8 19 km 238 km 81 km NNE of Cruz Bay, U.S. Virgin Islands
before 2.4 22 km 231 km 71 km NE of Cruz Bay, U.S. Virgin Islands
before 3.2 76 km 226 km 79 km NE of Cruz Bay, U.S. Virgin Islands
before 3.0 14 km 238 km 66 km NNE of Cruz Bay, U.S. Virgin Islands
before 3.2 21 km 236 km 82 km NE of Cruz Bay, U.S. Virgin Islands
before 2.9 24 km 230 km 65 km NE of Cruz Bay, U.S. Virgin Islands
before 3.3 10 km 236 km 65 km NNE of Cruz Bay, U.S. Virgin Islands
before 2.9 43 km 225 km 58 km NE of Cruz Bay, U.S. Virgin Islands
before 3.3 81 km 172 km 66 km E of Cruz Bay, U.S. Virgin Islands
before 3.3 21 km 221 km 92 km NE of Cruz Bay, U.S. Virgin Islands
before 3.2 12 km 241 km 40 km SE of Esperanza, Puerto Rico
before 2.6 15 km 238 km 49 km NNE of Cruz Bay, U.S. Virgin Islands
before 2.9 11 km 238 km 63 km NNE 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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