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Earthquake · Tuesday, October 27, 2026

Magnitude 2.5 earthquake 123 km SSE of Unalaska, Alaska

A magnitude 2.5 (micro) earthquake struck 123 km SSE of Unalaska, Alaska on Tuesday, October 27, 2026 at , at a depth of 10 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
2.5Micro
Depth
10km · shallow
Time
Epicenter
52.95° N
165.51° W
Aftershocks so far
0within 250 km
Largest aftershock
—

14 days ago · USGS id us7000ttgy · 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 146 km away on Oct 1, 14:46 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.4 3 km 227 km 42 km W of False Pass, Alaska
before 1.2 1 km 233 km 21 km WSW of False Pass, Alaska
before 1.1 1 km 233 km 21 km WSW of False Pass, Alaska
before 1.3 1 km 233 km 21 km WSW of False Pass, Alaska
before 1.0 1 km 231 km 24 km WSW of False Pass, Alaska
before 4.5 35 km 69 km 81 km SSE of Akutan, Alaska
before 2.3 109 km 119 km 20 km SW of Akutan, Alaska
before 2.7 32 km 95 km 94 km SSW of Unalaska, Alaska
before 1.3 8 km 184 km 65 km NE of Nikolski, Alaska
before 2.8 62 km 148 km 77 km E of Nikolski, Alaska
before 3.7 131 km 215 km 40 km SSE of Nikolski, Alaska
before 2.4 30 km 56 km 89 km SSE of Akutan, Alaska
before 4.0 10 km 131 km 153 km ESE of Akutan, Alaska
before 2.6 35 km 138 km 156 km S of False Pass, Alaska
before 2.2 29 km 96 km 97 km SSW of Unalaska, Alaska
before 1.4 3 km 122 km 4 km SW of Unalaska, Alaska
before 1.5 10 km 126 km 4 km WSW of Dutch Harbor, Alaska
before 2.0 7 km 136 km 24 km WSW of Dutch Harbor, Alaska
before 2.0 7 km 136 km 24 km WSW of Dutch Harbor, Alaska
before 2.2 3 km 137 km 25 km W of Dutch Harbor, Alaska
before 2.8 77 km 109 km 49 km SSW of Unalaska, Alaska
before 2.7 15 km 142 km 138 km S of False Pass, Alaska
before 1.3 2 km 203 km 59 km WSW of False Pass, Alaska
before 2.6 6 km 138 km 156 km S of False Pass, Alaska
before 2.1 21 km 130 km 97 km E of Nikolski, Alaska
before 2.5 26 km 141 km 142 km S of False Pass, Alaska
before 2.3 8 km 9 km 122 km SE of Unalaska, Alaska
before 2.1 87 km 223 km 5 km NNE of Nikolski, Alaska
before 3.1 35 km 145 km 161 km S of False Pass, Alaska
before 2.5 20 km 142 km 151 km S 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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