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Earthquake · Thursday, October 29, 2026

Magnitude 5.0 earthquake 143 km S of False Pass, Alaska

A magnitude 5.0 (moderate) earthquake struck 143 km S of False Pass, Alaska on Thursday, October 29, 2026 at , at a depth of 16 km (shallow).

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Magnitude
5.0Moderate
Depth
16km · shallow
Time
Epicenter
53.58° N
163.03° W
Aftershocks so far
5within 250 km
Largest aftershock
4.8M

11 days ago · USGS id us7000tu3j · 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 5.0 means

Moderate earthquakes are felt by everyone nearby and can cause minor to moderate damage close to the epicenter, mostly to weaker structures.

A magnitude 5.0 releases about 32 times the seismic energy of a magnitude 4.0, roughly the energy of 477 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

5 aftershocks and 17 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 3.8.

Time (UTC)MagnitudeDepthDistanceLocation
4.7 28 km 8 km 139 km SSE of False Pass, Alaska
3.5 12 km 13 km 146 km SSE of False Pass, Alaska
4.6 16 km 6 km 147 km SSE of False Pass, Alaska
2.6 14 km 211 km 105 km SSE of Sand Point, Alaska
4.8 9 km 8 km 139 km SSE of False Pass, Alaska
before 4.6 35 km 139 km 81 km SSE of Akutan, Alaska
before 4.3 35 km 144 km 81 km SSE of Akutan, Alaska
before 4.2 15 km 134 km 84 km SE of Akutan, Alaska
before 4.6 35 km 141 km 82 km SSE of Akutan, Alaska
before 4.5 0 km 135 km 89 km SSE of Akutan, Alaska
before 4.5 35 km 137 km 81 km SSE of Akutan, Alaska
before 4.2 37 km 248 km 99 km SSE of Sand Point, Alaska
before 3.2 27 km 210 km 44 km SW of Sand Point, Alaska
before 3.9 10 km 114 km 203 km SSE of King Cove, Alaska
before 5.0 51 km 217 km 80 km SSE of Sand Point, Alaska
before 5.0 35 km 210 km 81 km S of Sand Point, Alaska
before 2.8 50 km 137 km 60 km SE of Akutan, Alaska
before 3.0 35 km 133 km 72 km SE of Akutan, Alaska
before 3.7 142 km 127 km 35 km SW of False Pass, Alaska
before 3.4 49 km 231 km 38 km S of Sand Point, Alaska
before 3.5 35 km 226 km 105 km SSE of Sand Point, Alaska
before 4.8 35 km 48 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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