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Earthquake · Tuesday, October 27, 2026

Magnitude 2.5 earthquake 73 km SW of Unalaska, Alaska

A magnitude 2.5 (micro) earthquake struck 73 km SW of Unalaska, Alaska on Tuesday, October 27, 2026 at , at a depth of 2 km (shallow).

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Magnitude
2.5Micro
Depth
2km · shallow
Time
Epicenter
53.33° N
167.15° W
Aftershocks so far
0within 250 km
Largest aftershock
—

15 days ago · USGS id aka2026vghxtu · 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 4.8 struck 231 km away on Oct 1, 14:46 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.6 18 km 238 km 151 km S of False Pass, Alaska
before 3.3 21 km 238 km 151 km S of False Pass, Alaska
before 3.2 11 km 236 km 159 km S of False Pass, Alaska
before 4.5 20 km 245 km 158 km S of False Pass, Alaska
before 2.5 18 km 106 km 94 km SE of Unalaska, Alaska
before 4.0 28 km 248 km 195 km SE of Akutan, Alaska
before 2.5 7 km 184 km 85 km SSW of Nikolski, Alaska
before 2.2 21 km 40 km 98 km SSW of Unalaska, Alaska
before 3.6 35 km 101 km 82 km SE of Unalaska, Alaska
before 2.1 36 km 144 km 68 km SE of Akutan, Alaska
before 2.5 14 km 87 km 77 km SE of Unalaska, Alaska
before 2.2 32 km 83 km 75 km ESE of Nikolski, Alaska
before 3.0 198 km 164 km 56 km WNW of Nikolski, Alaska
before 1.4 6 km 63 km 24 km W of Dutch Harbor, Alaska
before 2.8 10 km 222 km 114 km SSW of Nikolski, Alaska
before 3.7 10 km 226 km 123 km SSW of Nikolski, Alaska
before 2.2 32 km 123 km 40 km SSE of Nikolski, Alaska
before 2.2 22 km 123 km 45 km SSE of Nikolski, Alaska
before 2.3 30 km 35 km 95 km SSW of Unalaska, Alaska
before 1.1 9 km 213 km 85 km NE of Akutan, Alaska
before 4.0 10 km 219 km 161 km S of Nikolski, Alaska
before 2.6 3 km 183 km 102 km S of Nikolski, Alaska
before 1.7 19 km 237 km 60 km WSW of False Pass, Alaska
before 2.8 8 km 199 km 103 km SSW of Nikolski, Alaska
before 2.4 23 km 216 km 114 km SSW of False Pass, Alaska
before 2.5 10 km 126 km 124 km SE of Unalaska, Alaska
before 2.3 28 km 35 km 96 km SSW of Unalaska, Alaska
before 2.3 34 km 35 km 95 km SSW of Unalaska, Alaska
before 3.8 41 km 22 km 87 km SSW of Unalaska, Alaska
before 3.0 35 km 145 km 67 km SE of Akutan, 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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