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Earthquake · Saturday, October 31, 2026

Magnitude 4.5 earthquake 121 km SE of Atka, Alaska

A magnitude 4.5 (light) earthquake struck 121 km SE of Atka, Alaska on Saturday, October 31, 2026 at , at a depth of 1 km (shallow).

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The epicenter (largest marker, center) on EarthBrowser’s globe with the other recent earthquakes in the region. Tap a marker to open its 3D cross-section; drag to look around.
Magnitude
4.5Light
Depth
1km · shallow
Time
Epicenter
51.52° N
172.81° W
Aftershocks so far
0within 250 km
Largest aftershock
—

10 days ago · USGS id aka2026vpcige · 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 4.5 means

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

A magnitude 4.5 releases about 32 times the seismic energy of a magnitude 3.5, roughly the energy of 85 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 229 km away on Oct 15, 13:16 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.7 76 km 140 km 52 km SW of Atka, Alaska
before 3.4 35 km 110 km 57 km SSW of Atka, Alaska
before 3.5 63 km 115 km 40 km SSW of Atka, Alaska
before 2.6 35 km 225 km 76 km SSE of Adak, Alaska
before 2.9 66 km 108 km 35 km S of Atka, Alaska
before 3.4 2 km 78 km 106 km E of Atka, Alaska
before 3.5 206 km 126 km 11 km NNE of Atka, Alaska
before 2.8 199 km 150 km 29 km WNW of Atka, Alaska
before 3.0 10 km 135 km 177 km WSW of Nikolski, Alaska
before 3.7 35 km 190 km 79 km ESE of Adak, Alaska
before 2.3 14 km 236 km 92 km SSW of Nikolski, Alaska
before 2.8 13 km 226 km 89 km SW of Nikolski, Alaska
before 2.0 38 km 220 km 64 km SE of Adak, Alaska
before 1.9 12 km 215 km 80 km SE of Adak, Alaska
before 3.1 19 km 158 km 163 km SW of Nikolski, Alaska
before 2.3 149 km 107 km 35 km ENE of Atka, Alaska
before 2.6 22 km 215 km 72 km SE of Adak, Alaska
before 2.9 17 km 228 km 121 km SSW of Nikolski, Alaska
before 2.4 10 km 121 km 87 km SSW of Atka, Alaska
before 2.2 22 km 147 km 84 km SW of Atka, Alaska
before 2.3 6 km 64 km 59 km SE of Atka, Alaska
before 2.3 12 km 120 km 87 km SSW of Atka, Alaska
before 2.0 27 km 233 km 68 km SSE of Adak, Alaska
before 2.3 4 km 121 km 92 km SSW of Atka, Alaska
before 2.5 75 km 71 km 54 km ESE of Atka, Alaska
before 2.6 10 km 223 km 179 km SSE of Adak, Alaska
before 2.6 27 km 237 km 54 km SSE of Adak, Alaska
before 2.6 71 km 65 km 65 km ESE of Atka, Alaska
before 3.1 11 km 202 km 177 km W of Nikolski, Alaska
before 2.6 10 km 160 km 191 km S of Atka, Alaska

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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