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Earthquake · Saturday, September 12, 2026

Magnitude 3.9 earthquake 62 km S of Cantwell, Alaska

A magnitude 3.9 (minor) earthquake struck 62 km S of Cantwell, Alaska on Saturday, September 12, 2026 at , at a depth of 77 km (intermediate).

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Magnitude
3.9Minor
Depth
77km · intermediate
Time
Epicenter
62.83° N
149.05° W
Aftershocks so far
0within 250 km
Largest aftershock
—

58 days ago · USGS id aka2026sbqvff · 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 3.9 means

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

A magnitude 3.9 releases about 32 times the seismic energy of a magnitude 2.9, roughly the energy of 11 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 2.7.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.4 4 km 96 km 55 km ENE of Cantwell, Alaska
before 1.2 5 km 219 km 36 km WNW of Four Mile Road, Alaska
before 2.3 81 km 124 km 31 km SW of Petersville, Alaska
before 1.6 13 km 206 km 37 km NE of Paxson, Alaska
before 2.3 1 km 126 km 20 km NW of Willow, Alaska
before 2.0 79 km 36 km 53 km SW of Cantwell, Alaska
before 1.3 4 km 248 km 78 km WNW of Tyonek, Alaska
before 2.8 123 km 84 km 61 km N of Petersville, Alaska
before 1.2 10 km 219 km 36 km WNW of Four Mile Road, Alaska
before 1.2 2 km 136 km 35 km W of Ferry, Alaska
before 2.4 93 km 119 km 25 km SW of Petersville, Alaska
before 1.3 5 km 211 km 44 km S of Manley Hot Springs, Alaska
before 2.8 18 km 196 km 46 km N of Valdez, Alaska
before 2.3 15 km 128 km 8 km N of Meadow Lakes, Alaska
before 2.6 14 km 195 km 48 km SSE of Nelchina, Alaska
before 1.1 5 km 224 km 27 km N of Four Mile Road, Alaska
before 1.8 119 km 81 km 70 km WSW of Cantwell, Alaska
before 2.0 91 km 133 km 31 km N of Skwentna, Alaska
before 1.3 47 km 192 km 48 km SSE of Nelchina, Alaska
before 1.0 5 km 218 km 35 km WNW of Four Mile Road, Alaska
before 1.1 8 km 220 km 38 km WNW of Four Mile Road, Alaska
before 1.2 6 km 219 km 37 km WNW of Four Mile Road, Alaska
before 1.5 30 km 150 km 3 km NE of Big Lake, Alaska
before 1.8 5 km 248 km 77 km WNW of Tyonek, Alaska
before 1.1 11 km 221 km 38 km WNW of Four Mile Road, Alaska
before 1.3 46 km 86 km 41 km NNE of Chickaloon, Alaska
before 1.8 129 km 95 km 64 km SE of Denali National Park, Alaska
before 1.6 75 km 228 km 4 km S of Tyonek, Alaska
before 1.3 7 km 209 km 44 km S of Manley Hot Springs, Alaska
before 1.0 5 km 242 km 8 km WSW of Two Rivers, 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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