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Earthquake · Sunday, October 11, 2026

Magnitude 3.4 earthquake 61 km ESE of King Salmon, Alaska

A magnitude 3.4 (minor) earthquake struck 61 km ESE of King Salmon, Alaska on Sunday, October 11, 2026 at , at a depth of 153 km (intermediate).

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Magnitude
3.4Minor
Depth
153km · intermediate
Time
Epicenter
58.46° N
155.69° W
Aftershocks so far
0within 250 km
Largest aftershock
—

29 days ago · USGS id aka2026udjcmd · 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 3.4 means

Minor earthquakes are often felt by people nearby but almost never cause damage.

A magnitude 3.4 releases about 32 times the seismic energy of a magnitude 2.4, roughly the energy of 2 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

0 aftershocks and 100 earlier earthquakes within 250 km in the 30 days around this event. Aftershock rates fall off quickly in the first days (Omori's law); the largest aftershock is typically about one magnitude unit smaller than the mainshock (Båth's law), here around magnitude 2.2.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.5 55 km 231 km 25 km S of Port Graham, Alaska
before 1.0 27 km 56 km 81 km WNW of Karluk, Alaska
before 1.4 18 km 68 km 77 km WNW of Karluk, Alaska
before 2.0 10 km 69 km 76 km WNW of Karluk, Alaska
before 1.6 17 km 69 km 76 km WNW of Karluk, Alaska
before 2.6 99 km 216 km 55 km W of Anchor Point, Alaska
before 2.6 68 km 226 km 33 km NW of Nanwalek, Alaska
before 1.0 6 km 71 km 92 km N of Karluk, Alaska
before 1.2 7 km 72 km 92 km N of Karluk, Alaska
before 2.6 5 km 71 km 90 km N of Karluk, Alaska
before 1.7 11 km 137 km 88 km ESE of Ugashik, Alaska
before 1.0 4 km 71 km 92 km N of Karluk, Alaska
before 1.6 86 km 221 km 49 km W of Anchor Point, Alaska
before 2.0 141 km 202 km 39 km E of Pedro Bay, Alaska
before 1.7 28 km 143 km 84 km WSW of Karluk, Alaska
before 1.0 5 km 39 km 87 km SSE of Igiugig, Alaska
before 1.6 74 km 247 km 21 km W of Anchor Point, Alaska
before 2.4 43 km 219 km 12 km ESE of Kodiak, Alaska
before 1.7 76 km 117 km 15 km W of Karluk, Alaska
before 1.5 55 km 110 km 27 km NNE of Karluk, Alaska
before 2.1 64 km 102 km 21 km NNW of Karluk, Alaska
before 2.3 56 km 124 km 47 km WSW of Karluk, Alaska
before 1.5 91 km 198 km 61 km WNW of Nanwalek, Alaska
before 1.0 5 km 155 km 50 km ESE of Pope-Vannoy Landing, Alaska
before 1.0 5 km 39 km 85 km NNW of Karluk, Alaska
before 2.0 27 km 243 km 51 km ENE of Kodiak, Alaska
before 2.0 105 km 225 km 54 km W of Anchor Point, Alaska
before 1.7 107 km 84 km 87 km SSE of Kokhanok, Alaska
before 1.8 8 km 189 km 73 km SSE of Ugashik, Alaska
before 1.3 5 km 229 km 62 km ENE of Pedro Bay, 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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