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Earthquake · Thursday, October 15, 2026

Magnitude 3.6 earthquake 40 km NNE of Beaver, Alaska

A magnitude 3.6 (minor) earthquake struck 40 km NNE of Beaver, Alaska on Thursday, October 15, 2026 at , at a depth of 1 km (shallow).

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Magnitude
3.6Minor
Depth
1km · shallow
Time
Epicenter
66.66° N
146.91° W
Aftershocks so far
0within 250 km
Largest aftershock
—

25 days ago · USGS id aka2026ulpwbm · 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 3.6 means

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

A magnitude 3.6 releases about 32 times the seismic energy of a magnitude 2.6, roughly the energy of 4 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

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 2.4.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.7 10 km 247 km 36 km WNW of Four Mile Road, Alaska
before 1.0 5 km 177 km 24 km NE of Minto, Alaska
before 1.3 5 km 191 km 7 km E of Fox, Alaska
before 2.6 5 km 122 km 36 km WNW of Central, Alaska
before 1.7 5 km 179 km 28 km N of Rampart, Alaska
before 1.4 9 km 246 km 37 km WNW of Four Mile Road, Alaska
before 1.0 5 km 177 km 26 km NE of Minto, Alaska
before 1.6 5 km 188 km 14 km E of Fox, Alaska
before 1.1 8 km 213 km 16 km SSE of Pleasant Valley, Alaska
before 1.3 5 km 180 km 22 km NE of Minto, Alaska
before 1.3 11 km 214 km 30 km W of Ester, Alaska
before 1.1 4 km 226 km 25 km N of Four Mile Road, Alaska
before 1.1 16 km 247 km 38 km WNW of Four Mile Road, Alaska
before 1.2 5 km 179 km 26 km SSE of Central, Alaska
before 1.2 5 km 190 km 6 km E of Fox, Alaska
before 2.4 5 km 246 km 38 km NW of Four Mile Road, Alaska
before 1.5 1 km 249 km 39 km WNW of Four Mile Road, Alaska
before 1.3 16 km 222 km 30 km ENE of Manley Hot Springs, Alaska
before 1.2 2 km 188 km 7 km ENE of Fox, Alaska
before 1.9 0 km 189 km 55 km SSW of Central, Alaska
before 1.1 11 km 206 km 14 km SE of Minto, Alaska
before 1.3 16 km 228 km 24 km N of Four Mile Road, Alaska
before 1.3 5 km 244 km 6 km NNE of Manley Hot Springs, Alaska
before 1.6 14 km 247 km 9 km NW of Four Mile Road, Alaska
before 1.7 5 km 240 km 25 km SW of Eielson Air Force Base, Alaska
before 1.8 7 km 243 km 6 km SW of Salcha, Alaska
before 2.3 6 km 244 km 6 km SSW of Salcha, Alaska
before 1.3 12 km 215 km 35 km W of Ester, Alaska
before 1.0 2 km 140 km 7 km NE of Livengood, Alaska
before 1.2 5 km 137 km 39 km E of Livengood, 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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