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Earthquake · Monday, November 2, 2026

Magnitude 1.1 earthquake 107 km S of McCarthy, Alaska

A magnitude 1.1 (micro) earthquake struck 107 km S of McCarthy, Alaska on Monday, November 2, 2026 at , at a depth of 5 km (shallow).

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Magnitude
1.1Micro
Depth
5km · shallow
Time
Epicenter
60.48° N
143.05° W
Aftershocks so far
0within 250 km
Largest aftershock
—

7 days ago · USGS id aka2026vsvjpx · 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 1.1 means

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

A magnitude 1.1 releases about 32 times the seismic energy of a magnitude 0.1, 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 167 km away on Oct 24, 01:00 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.0 18 km 209 km 78 km ESE of Chenega, Alaska
before 1.7 5 km 238 km 43 km NW of Tatitlek, Alaska
before 1.3 5 km 115 km 56 km E of McCarthy, Alaska
before 1.8 1 km 91 km 124 km NW of Yakutat, Alaska
before 1.2 5 km 88 km 125 km NW of Yakutat, Alaska
before 1.9 3 km 238 km 43 km NW of Tatitlek, Alaska
before 1.3 9 km 238 km 43 km NW of Tatitlek, Alaska
before 1.1 19 km 117 km 66 km ESE of McCarthy, Alaska
before 1.0 21 km 55 km 84 km SSE of McCarthy, Alaska
before 1.4 8 km 147 km 102 km E of McCarthy, Alaska
before 2.8 5 km 159 km 88 km ENE of McCarthy, Alaska
before 1.7 5 km 236 km 43 km WNW of Valdez, Alaska
before 1.7 5 km 147 km 98 km E of McCarthy, Alaska
before 1.3 36 km 226 km 39 km SSE of Nelchina, Alaska
before 1.7 5 km 159 km 88 km ENE of McCarthy, Alaska
before 2.2 5 km 160 km 88 km ENE of McCarthy, Alaska
before 1.8 5 km 30 km 94 km S of McCarthy, Alaska
before 1.3 5 km 116 km 59 km ESE of McCarthy, Alaska
before 1.5 18 km 150 km 66 km NW of Yakutat, Alaska
before 1.3 0 km 105 km 110 km NW of Yakutat, Alaska
before 1.2 18 km 108 km 105 km NW of Yakutat, Alaska
before 1.1 5 km 238 km 44 km NW of Tatitlek, Alaska
before 1.9 20 km 240 km 37 km W of Tatitlek, Alaska
before 1.0 13 km 9 km 110 km S of McCarthy, Alaska
before 2.4 4 km 147 km 70 km NW of Yakutat, Alaska
before 1.1 12 km 118 km 56 km E of McCarthy, Alaska
before 1.6 15 km 238 km 41 km WSW of Tatitlek, Alaska
before 1.4 5 km 148 km 100 km E of McCarthy, Alaska
before 1.8 2 km 219 km 43 km SE of Nelchina, Alaska
before 1.7 10 km 121 km 93 km WNW 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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