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Earthquake · Thursday, November 5, 2026

Magnitude 1.4 earthquake 129 km S of McCarthy, Alaska

A magnitude 1.4 (micro) earthquake struck 129 km S of McCarthy, Alaska on Thursday, November 5, 2026 at , at a depth of 5 km (shallow).

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Magnitude
1.4Micro
Depth
5km · shallow
Time
Epicenter
60.29° N
143.35° W
Aftershocks so far
0within 250 km
Largest aftershock
—

4 days ago · USGS id aka2026vxzvxg · 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 3.4 struck 150 km away on Oct 24, 01:00 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.3 16 km 214 km 26 km NW of Valdez, Alaska
before 1.5 24 km 131 km 88 km WNW of Yakutat, Alaska
before 1.6 5 km 182 km 92 km E of McCarthy, Alaska
before 2.3 22 km 193 km 37 km SSW of Tatitlek, Alaska
before 2.0 18 km 188 km 78 km ESE of Chenega, Alaska
before 1.7 5 km 231 km 43 km NW of Tatitlek, Alaska
before 1.3 5 km 142 km 56 km E of McCarthy, Alaska
before 1.8 1 km 105 km 124 km NW of Yakutat, Alaska
before 1.2 5 km 99 km 125 km NW of Yakutat, Alaska
before 1.4 22 km 244 km 40 km NNE of Chenega, Alaska
before 1.9 3 km 231 km 43 km NW of Tatitlek, Alaska
before 1.3 9 km 231 km 43 km NW of Tatitlek, Alaska
before 1.1 19 km 144 km 66 km ESE of McCarthy, Alaska
before 1.0 21 km 81 km 84 km SSE of McCarthy, Alaska
before 1.4 8 km 174 km 102 km E of McCarthy, Alaska
before 2.8 5 km 186 km 88 km ENE of McCarthy, Alaska
before 1.7 5 km 230 km 43 km WNW of Valdez, Alaska
before 1.7 5 km 173 km 98 km E of McCarthy, Alaska
before 1.3 36 km 227 km 39 km SSE of Nelchina, Alaska
before 1.7 5 km 186 km 88 km ENE of McCarthy, Alaska
before 2.2 5 km 187 km 88 km ENE of McCarthy, Alaska
before 1.8 5 km 55 km 94 km S of McCarthy, Alaska
before 1.3 5 km 143 km 59 km ESE of McCarthy, Alaska
before 1.5 18 km 161 km 66 km NW of Yakutat, Alaska
before 1.3 0 km 117 km 110 km NW of Yakutat, Alaska
before 1.2 18 km 120 km 105 km NW of Yakutat, Alaska
before 1.1 5 km 231 km 44 km NW of Tatitlek, Alaska
before 1.9 20 km 230 km 37 km W of Tatitlek, Alaska
before 1.0 13 km 30 km 110 km S of McCarthy, Alaska
before 2.4 4 km 158 km 70 km NW of Yakutat, 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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