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Earthquake · Thursday, September 17, 2026

Magnitude 6.4 earthquake 163 km WSW of Nikolski, Alaska

A magnitude 6.4 (strong) earthquake struck 163 km WSW of Nikolski, Alaska on Thursday, September 17, 2026 at , at a depth of 115 km (intermediate).

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Magnitude
6.4Strong
Depth
115km · intermediate
Time
Epicenter
52.54° N
171.19° W
Aftershocks so far
8within 250 km
Largest aftershock
4.7M

53 days ago · USGS id aka2026slmipb · 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 6.4 means

Strong earthquakes can damage buildings near the epicenter, especially older or poorly built ones, and are felt over a wide area.

A magnitude 6.4 releases about 32 times the seismic energy of a magnitude 5.4, roughly the energy of 60 thousand 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.

Intermediate-depth earthquakes (70 to 300 km) occur inside subducting slabs. The extra distance to the surface spreads the shaking over a wider area at lower intensity.

Nearby earthquakes and aftershocks

This event is part of a sequence: a larger magnitude 6.5 struck 26 km away on Sep 17, 14:19 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
4.7 10 km 125 km 114 km SSW of Nikolski, Alaska
1.5 2 km 97 km 66 km W of Nikolski, Alaska
1.3 10 km 92 km 70 km WSW of Nikolski, Alaska
1.6 8 km 92 km 71 km WSW of Nikolski, Alaska
2.5 74 km 202 km 40 km E of Nikolski, Alaska
3.9 111 km 36 km 169 km WSW of Nikolski, Alaska
3.9 20 km 82 km 187 km SW of Nikolski, Alaska
4.0 20 km 88 km 187 km SW of Nikolski, Alaska
before 6.5 112 km 26 km 165 km W of Nikolski, Alaska
before 6.3 83 km 31 km 167 km W of Nikolski, Alaska
before 3.6 19 km 131 km 89 km SSW of Nikolski, Alaska
before 4.9 35 km 130 km 80 km SSW of Nikolski, Alaska
before 3.4 17 km 139 km 71 km SSW of Nikolski, Alaska
before 3.8 36 km 135 km 100 km SSW of Nikolski, Alaska
before 4.1 21 km 140 km 104 km SSW of Nikolski, Alaska
before 4.2 35 km 121 km 88 km SSW of Nikolski, Alaska
before 3.4 9 km 141 km 84 km SSW of Nikolski, Alaska
before 5.2 8 km 140 km 93 km SSW of Nikolski, Alaska
before 5.5 10 km 150 km 100 km S of Nikolski, Alaska
before 5.3 10 km 141 km 93 km SSW of Nikolski, Alaska
before 5.3 10 km 145 km 104 km SSW of Nikolski, Alaska
before 3.5 14 km 139 km 94 km SSW of Nikolski, Alaska
before 4.8 35 km 123 km 81 km SSW of Nikolski, Alaska
before 3.6 1 km 151 km 93 km S of Nikolski, Alaska
before 3.9 7 km 137 km 95 km SSW of Nikolski, Alaska
before 3.7 9 km 134 km 94 km SSW of Nikolski, Alaska
before 5.3 17 km 131 km 85 km SSW of Nikolski, Alaska
before 5.2 35 km 157 km 93 km S of Nikolski, Alaska
before 5.2 10 km 146 km 100 km SSW of Nikolski, Alaska
before 5.3 27 km 114 km 84 km SSW of Nikolski, 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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