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Earthquake · Saturday, October 3, 2026

Magnitude 1.4 earthquake 71 km WNW of Karluk, Alaska

A magnitude 1.4 (micro) earthquake struck 71 km WNW of Karluk, Alaska on Saturday, October 3, 2026 at , at a depth of 5 km (shallow).

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Magnitude
1.4Micro
Depth
5km · shallow
Time
Epicenter
57.91° N
155.47° W
Aftershocks so far
0within 250 km
Largest aftershock
—

37 days ago · USGS id aka2026toqoaq · 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 1.4 means

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

A magnitude 1.4 releases about 32 times the seismic energy of a magnitude 0.4, 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 4.0 struck 201 km away on Sep 15, 14:32 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.9 22 km 108 km 58 km W of Akhiok, Alaska
before 2.2 5 km 134 km 36 km SSE of Ugashik, Alaska
before 4.0 18 km 201 km 119 km E of Chignik, Alaska
before 2.0 5 km 231 km 35 km E of Chignik, Alaska
before 1.7 80 km 191 km 74 km WSW of Nanwalek, Alaska
before 1.2 5 km 200 km 60 km SE of Pedro Bay, Alaska
before 1.3 69 km 212 km 52 km SSW of Nanwalek, Alaska
before 1.3 144 km 48 km 66 km SE of King Salmon, Alaska
before 1.3 79 km 44 km 28 km WNW of Karluk, Alaska
before 1.9 23 km 149 km 92 km SSE of Ugashik, Alaska
before 3.0 49 km 208 km 83 km S of Akhiok, Alaska
before 2.7 137 km 242 km 39 km E of Pedro Bay, Alaska
before 1.6 83 km 79 km 75 km WSW of Karluk, Alaska
before 1.3 32 km 97 km 43 km NNE of Larsen Bay, Alaska
before 1.9 79 km 14 km 61 km WNW of Karluk, Alaska
before 1.4 79 km 201 km 52 km NE of Chignik, Alaska
before 1.6 69 km 105 km 99 km W of Akhiok, Alaska
before 1.4 8 km 24 km 93 km ESE of Egegik, Alaska
before 1.6 128 km 232 km 37 km ESE of Pedro Bay, Alaska
before 1.7 57 km 63 km 9 km NNW of Karluk, Alaska
before 1.8 16 km 141 km 55 km WSW of Akhiok, Alaska
before 1.0 5 km 40 km 85 km NNW of Karluk, Alaska
before 1.6 96 km 249 km 60 km W of Anchor Point, Alaska
before 1.6 14 km 171 km 70 km S of Ugashik, Alaska
before 2.9 131 km 247 km 47 km E of Pedro Bay, Alaska
before 1.8 77 km 240 km 50 km WNW of Nanwalek, Alaska
before 1.9 104 km 191 km 70 km ESE of Pope-Vannoy Landing, Alaska
before 1.5 3 km 38 km 89 km ENE of Ugashik, Alaska
before 1.3 106 km 32 km 83 km W of Karluk, Alaska
before 3.2 15 km 240 km 107 km SE of Akhiok, 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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