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Earthquake · Wednesday, November 4, 2026

Magnitude 3.2 earthquake 75 km E of Cantwell, Alaska

A magnitude 3.2 (minor) earthquake struck 75 km E of Cantwell, Alaska on Wednesday, November 4, 2026 at , at a depth of 5 km (shallow).

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Magnitude
3.2Minor
Depth
5km · shallow
Time
Epicenter
63.50° N
147.46° W
Aftershocks so far
0within 250 km
Largest aftershock
—

6 days ago · USGS id aka2026vvrwqb · 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 3.2 means

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

A magnitude 3.2 releases about 32 times the seismic energy of a magnitude 2.2, roughly the energy of 1 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

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 2.0.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.4 16 km 220 km 16 km N of Meadow Lakes, Alaska
before 1.9 5 km 146 km 63 km N of Chase, Alaska
before 2.1 1 km 152 km 44 km N of Chase, Alaska
before 2.0 3 km 9 km 66 km E of Cantwell, Alaska
before 1.4 5 km 230 km 11 km WSW of Manley Hot Springs, Alaska
before 1.8 28 km 168 km 36 km N of Sutton-Alpine, Alaska
before 1.2 9 km 103 km 12 km W of Harding-Birch Lakes, Alaska
before 1.1 16 km 184 km 38 km WNW of Four Mile Road, Alaska
before 1.6 38 km 173 km 1 km NW of Eureka Roadhouse, Alaska
before 1.5 23 km 238 km 31 km SW of Tetlin, Alaska
before 1.8 15 km 239 km 6 km NW of Houston, Alaska
before 1.2 5 km 244 km 26 km SSE of Central, Alaska
before 1.6 0 km 9 km 71 km ESE of Denali Park, Alaska
before 3.1 113 km 192 km 43 km NNW of Petersville, Alaska
before 1.2 5 km 164 km 6 km E of Fox, Alaska
before 2.4 5 km 184 km 38 km NW of Four Mile Road, Alaska
before 1.8 0 km 229 km 13 km SW of Manley Hot Springs, Alaska
before 1.5 1 km 183 km 39 km WNW of Four Mile Road, Alaska
before 1.7 5 km 230 km 12 km WSW of Manley Hot Springs, Alaska
before 1.0 23 km 222 km 24 km ENE of Knik River, Alaska
before 1.4 5 km 192 km 1 km SE of Susitna North, Alaska
before 1.3 16 km 220 km 30 km ENE of Manley Hot Springs, Alaska
before 2.0 91 km 220 km 29 km WNW of Petersville, Alaska
before 2.2 23 km 243 km 6 km SE of Houston, Alaska
before 1.4 3 km 20 km 56 km ENE of Cantwell, Alaska
before 1.8 86 km 224 km 31 km W of Petersville, Alaska
before 2.5 16 km 172 km 27 km WNW of Four Mile Road, Alaska
before 2.3 5 km 90 km 9 km ESE of Ferry, Alaska
before 1.2 2 km 166 km 7 km ENE of Fox, Alaska
before 2.9 5 km 204 km 46 km SSE of Denali National Park, 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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