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Earthquake · Tuesday, September 29, 2026

Magnitude 4.0 earthquake 64 km SE of King Cove, Alaska

A magnitude 4.0 (light) earthquake struck 64 km SE of King Cove, Alaska on Tuesday, September 29, 2026 at , at a depth of 50 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
4.0Light
Depth
50km · shallow
Time
Epicenter
54.66° N
161.59° W
Aftershocks so far
33within 250 km
Largest aftershock
5.0M

41 days ago · USGS id us6000tybl · 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 4.0 means

Light earthquakes are widely felt near the epicenter, rattling windows and shelves, but rarely cause damage.

A magnitude 4.0 releases about 32 times the seismic energy of a magnitude 3.0, roughly the energy of 15 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 5.0 struck 81 km away on Oct 20, 10:40 UTC, so this is most likely one of its foreshocks.

Time (UTC)MagnitudeDepthDistanceLocation
4.2 37 km 126 km 99 km SSE of Sand Point, Alaska
1.7 24 km 185 km 72 km SSE of Perryville, Alaska
3.2 27 km 59 km 44 km SW of Sand Point, Alaska
3.9 10 km 149 km 203 km SSE of King Cove, Alaska
2.2 94 km 247 km 6 km W of Chignik Lake, Alaska
5.0 51 km 88 km 80 km SSE of Sand Point, Alaska
5.0 35 km 81 km 81 km S of Sand Point, Alaska
1.8 5 km 171 km 21 km SW of Ivanof Bay, Alaska
2.3 8 km 176 km 25 km W of Ivanof Bay, Alaska
3.3 176 km 155 km 46 km WSW of Ivanof Bay, Alaska
1.7 49 km 187 km 45 km S of Perryville, Alaska
2.8 50 km 248 km 60 km SE of Akutan, Alaska
3.7 142 km 142 km 35 km SW of False Pass, Alaska
2.4 9 km 178 km 26 km W of Ivanof Bay, Alaska
2.1 83 km 228 km 19 km NE of Perryville, Alaska
3.4 5 km 236 km 92 km SE of Perryville, Alaska
2.7 14 km 168 km 69 km S of Perryville, Alaska
1.6 7 km 174 km 20 km WSW of Ivanof Bay, Alaska
1.8 65 km 177 km 37 km SSE of Ivanof Bay, Alaska
3.4 49 km 84 km 38 km S of Sand Point, Alaska
2.5 18 km 166 km 57 km S of Ivanof Bay, Alaska
3.5 35 km 111 km 105 km SSE of Sand Point, Alaska
2.5 25 km 186 km 63 km SSE of Perryville, Alaska
3.0 20 km 223 km 68 km SE of Perryville, Alaska
1.3 5 km 200 km 15 km NNW of Ivanof Bay, Alaska
2.7 14 km 215 km 70 km SE of Perryville, Alaska
2.5 28 km 199 km 60 km SSE of Perryville, Alaska
1.7 9 km 171 km 21 km WSW of Ivanof Bay, Alaska
2.2 14 km 180 km 17 km W of Ivanof Bay, Alaska
4.8 35 km 174 km 127 km S of False Pass, 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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