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Earthquake · Tuesday, September 29, 2026

Magnitude 3.0 earthquake 17 km E of Eagle Village, Alaska

A magnitude 3.0 (minor) earthquake struck 17 km E of Eagle Village, Alaska on Tuesday, September 29, 2026 at , at a depth of 9 km (shallow).

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The epicenter (largest marker, center) on EarthBrowser’s globe with the other recent earthquakes in the region. Tap a marker to open its 3D cross-section; drag to look around.
Magnitude
3.0Minor
Depth
9km · shallow
Time
Epicenter
64.79° N
140.75° W
Aftershocks so far
16within 250 km
Largest aftershock
2.6M

42 days ago · USGS id us6000ty9x · 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 3.0 means

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

A magnitude 3.0 releases about 32 times the seismic energy of a magnitude 2.0, 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

16 aftershocks and 10 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 1.8.

Time (UTC)MagnitudeDepthDistanceLocation
1.6 12 km 216 km 56 km SSW of Central, Alaska
2.1 2 km 226 km 61 km SSW of Central, Alaska
1.7 1 km 225 km 60 km SSW of Central, Alaska
2.2 0 km 169 km 40 km ESE of Central, Alaska
1.4 8 km 226 km 25 km N of Deltana, Alaska
1.3 5 km 206 km 17 km SSE of Tok, Alaska
2.6 5 km 244 km 36 km WNW of Central, Alaska
1.5 23 km 234 km 31 km SW of Tetlin, Alaska
1.2 5 km 194 km 26 km SSE of Central, Alaska
1.9 0 km 215 km 55 km SSW of Central, Alaska
1.4 3 km 210 km 2 km NW of Central, Alaska
1.8 5 km 184 km 65 km SE of Chalkyitsik, Alaska
1.1 19 km 200 km 19 km SE of Dot Lake Village, Alaska
1.2 5 km 201 km 13 km S of Central, Alaska
1.4 2 km 210 km 20 km S of Tok, Alaska
1.7 2 km 36 km 22 km NNW of Eagle, Alaska
before 1.6 5 km 226 km 66 km ENE of Pleasant Valley, Alaska
before 1.9 3 km 224 km 15 km WNW of Central, Alaska
before 1.8 5 km 250 km 37 km NE of Harding-Birch Lakes, Alaska
before 1.5 5 km 174 km 79 km SSE of Central, Alaska
before 1.6 5 km 234 km 18 km NE of Fort Greely, Alaska
before 2.4 0 km 181 km 29 km SE of Central, Alaska
before 1.7 0 km 137 km 73 km SE of Central, Alaska
before 1.1 5 km 227 km 32 km WSW of Tanacross, Alaska
before 1.3 5 km 234 km 55 km E of Pleasant Valley, Alaska
before 2.4 1 km 235 km 54 km E of Pleasant Valley, 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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