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Earthquake · Wednesday, October 21, 2026

Magnitude 2.8 earthquake 12 km SW of Ugashik, Alaska

A magnitude 2.8 (micro) earthquake struck 12 km SW of Ugashik, Alaska on Wednesday, October 21, 2026 at , at a depth of 111 km (intermediate).

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Magnitude
2.8Micro
Depth
111km · intermediate
Time
Epicenter
57.44° N
157.55° W
Aftershocks so far
0within 250 km
Largest aftershock
—

19 days ago · USGS id aka2026uwcphn · 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 2.8 means

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

A magnitude 2.8 releases about 32 times the seismic energy of a magnitude 1.8, 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.

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

This event is part of a sequence: a larger magnitude 3.7 struck 164 km away on Sep 22, 08:48 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.7 1 km 106 km 81 km W of Karluk, Alaska
before 1.9 6 km 108 km 78 km W of Karluk, Alaska
before 3.4 5 km 104 km 83 km W of Karluk, Alaska
before 2.1 89 km 74 km 69 km NE of Chignik, Alaska
before 1.5 19 km 114 km 72 km W of Karluk, Alaska
before 2.7 14 km 234 km 70 km SE of Perryville, Alaska
before 1.0 5 km 145 km 89 km SE of King Salmon, Alaska
before 1.2 5 km 153 km 85 km NW of Karluk, Alaska
before 1.6 60 km 177 km 15 km NW of Karluk, Alaska
before 1.6 28 km 144 km 51 km WNW of Karluk, Alaska
before 2.5 28 km 237 km 60 km SSE of Perryville, Alaska
before 3.4 65 km 155 km 56 km W of Akhiok, Alaska
before 1.8 66 km 158 km 28 km W of Karluk, Alaska
before 1.3 35 km 104 km 90 km ESE of Egegik, Alaska
before 2.2 5 km 47 km 58 km SSW of Ugashik, Alaska
before 1.9 82 km 91 km 84 km ESE of Ugashik, Alaska
before 1.6 11 km 68 km 56 km ENE of Ugashik, Alaska
before 2.5 50 km 165 km 42 km SSE of Chignik, Alaska
before 2.8 68 km 178 km 36 km NNW of Karluk, Alaska
before 2.1 5 km 87 km 91 km SSE of Ugashik, Alaska
before 3.2 64 km 148 km 130 km E of Chignik, Alaska
before 1.4 5 km 135 km 71 km WNW of Karluk, Alaska
before 2.5 5 km 103 km 103 km SE of Ugashik, Alaska
before 1.5 22 km 99 km 86 km W of Karluk, Alaska
before 2.1 62 km 248 km 54 km WNW of Aleneva, Alaska
before 2.6 18 km 132 km 118 km E of Chignik, Alaska
before 2.1 11 km 114 km 116 km ENE of Chignik, Alaska
before 1.7 9 km 227 km 21 km WSW of Ivanof Bay, Alaska
before 2.2 14 km 218 km 17 km W of Ivanof Bay, Alaska
before 1.8 86 km 141 km 49 km WNW of Karluk, 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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