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Earthquake · Tuesday, October 6, 2026

Magnitude 5.5 earthquake 92 km NNW of Aleneva, Alaska

A magnitude 5.5 (moderate) earthquake struck 92 km NNW of Aleneva, Alaska on Tuesday, October 6, 2026 at , at a depth of 88 km (intermediate).

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Magnitude
5.5Moderate
Depth
88km · intermediate
Time
Epicenter
58.80° N
153.61° W
Aftershocks so far
0within 250 km
Largest aftershock
—

34 days ago · USGS id aka2026tuxgky · 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 5.5 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 5.5 releases about 32 times the seismic energy of a magnitude 4.5, roughly the energy of 3 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

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 4.3.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.7 80 km 45 km 74 km WSW of Nanwalek, Alaska
before 1.2 5 km 64 km 60 km SE of Pedro Bay, Alaska
before 1.2 5 km 158 km 51 km E of Port Alsworth, Alaska
before 1.0 12 km 156 km 72 km WNW of Happy Valley, Alaska
before 1.2 106 km 165 km 45 km WNW of Ninilchik, Alaska
before 1.3 69 km 71 km 52 km SSW of Nanwalek, Alaska
before 1.1 75 km 161 km 15 km WNW of Happy Valley, Alaska
before 1.3 144 km 137 km 66 km SE of King Salmon, Alaska
before 1.3 79 km 147 km 28 km WNW of Karluk, Alaska
before 2.7 137 km 113 km 39 km E of Pedro Bay, Alaska
before 1.6 83 km 210 km 75 km WSW of Karluk, Alaska
before 2.1 82 km 127 km 20 km SW of Anchor Point, Alaska
before 1.6 70 km 205 km 14 km ESE of Clam Gulch, Alaska
before 1.3 32 km 99 km 43 km NNE of Larsen Bay, Alaska
before 1.4 83 km 143 km 33 km WNW of Anchor Point, Alaska
before 1.8 15 km 141 km 92 km SSE of Port Graham, Alaska
before 1.9 79 km 154 km 61 km WNW of Karluk, Alaska
before 1.6 69 km 240 km 99 km W of Akhiok, Alaska
before 1.4 8 km 163 km 93 km ESE of Egegik, Alaska
before 1.6 128 km 103 km 37 km ESE of Pedro Bay, Alaska
before 2.8 104 km 235 km 51 km WNW of Nikiski, Alaska
before 1.7 57 km 140 km 9 km NNW of Karluk, Alaska
before 1.2 61 km 123 km 6 km N of Port Graham, Alaska
before 1.5 5 km 191 km 76 km NW of Ninilchik, Alaska
before 2.4 76 km 160 km 5 km SW of Happy Valley, Alaska
before 1.2 86 km 215 km 39 km W of Salamatof, Alaska
before 1.8 16 km 248 km 55 km WSW of Akhiok, Alaska
before 2.0 91 km 135 km 55 km WNW of Anchor Point, Alaska
before 1.0 5 km 110 km 85 km NNW of Karluk, Alaska
before 1.6 96 km 110 km 60 km W of Anchor Point, 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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