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Earthquake · Wednesday, October 28, 2026

Magnitude 2.5 earthquake 103 km E of Nikolski, Alaska

A magnitude 2.5 (micro) earthquake struck 103 km E of Nikolski, Alaska on Wednesday, October 28, 2026 at , at a depth of 65 km (shallow).

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Magnitude
2.5Micro
Depth
65km · shallow
Time
Epicenter
52.95° N
167.32° W
Aftershocks so far
0within 250 km
Largest aftershock
—

14 days ago · USGS id aka2026vilxmg · 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 2.5 means

Micro earthquakes are generally not felt and are recorded only by seismographs.

A magnitude 2.5 releases about 32 times the seismic energy of a magnitude 1.5, roughly the energy of 0 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 194 km away on Oct 15, 13:16 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.2 3 km 104 km 25 km W of Dutch Harbor, Alaska
before 2.8 77 km 66 km 49 km SSW of Unalaska, Alaska
before 3.1 19 km 250 km 163 km SW of Nikolski, Alaska
before 2.1 21 km 16 km 97 km E of Nikolski, Alaska
before 2.3 8 km 129 km 122 km SE of Unalaska, Alaska
before 2.1 87 km 102 km 5 km NNE of Nikolski, Alaska
before 1.2 8 km 104 km 22 km WSW of Dutch Harbor, Alaska
before 2.9 17 km 189 km 121 km SSW of Nikolski, Alaska
before 2.3 27 km 230 km 102 km ESE of Akutan, Alaska
before 2.3 0 km 129 km 42 km SSW of Nikolski, Alaska
before 2.3 165 km 150 km 49 km WNW of Nikolski, Alaska
before 2.5 3 km 65 km 139 km S of Unalaska, Alaska
before 2.5 18 km 123 km 94 km SE of Unalaska, Alaska
before 2.5 7 km 148 km 85 km SSW of Nikolski, Alaska
before 2.2 21 km 32 km 98 km SSW of Unalaska, Alaska
before 3.6 35 km 121 km 82 km SE of Unalaska, Alaska
before 2.1 36 km 172 km 68 km SE of Akutan, Alaska
before 2.5 14 km 107 km 77 km SE of Unalaska, Alaska
before 2.2 32 km 43 km 75 km ESE of Nikolski, Alaska
before 3.0 198 km 155 km 56 km WNW of Nikolski, Alaska
before 1.4 6 km 107 km 24 km W of Dutch Harbor, Alaska
before 2.8 10 km 188 km 114 km SSW of Nikolski, Alaska
before 3.7 10 km 190 km 123 km SSW of Nikolski, Alaska
before 2.2 32 km 91 km 40 km SSE of Nikolski, Alaska
before 2.2 22 km 90 km 45 km SSE of Nikolski, Alaska
before 2.3 30 km 29 km 95 km SSW of Unalaska, Alaska
before 4.0 10 km 176 km 161 km S of Nikolski, Alaska
before 2.6 3 km 143 km 102 km S of Nikolski, Alaska
before 2.8 8 km 162 km 103 km SSW of Nikolski, Alaska
before 2.4 23 km 243 km 114 km SSW of False Pass, 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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