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Earthquake · Sunday, October 11, 2026

Magnitude 3.6 earthquake 39 km N of Petersville, Alaska

A magnitude 3.6 (minor) earthquake struck 39 km N of Petersville, Alaska on Sunday, October 11, 2026 at , at a depth of 104 km (intermediate).

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Magnitude
3.6Minor
Depth
104km · intermediate
Time
Epicenter
62.85° N
150.69° W
Aftershocks so far
0within 250 km
Largest aftershock
—

29 days ago · USGS id aka2026udsseu · 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.

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 3.9 struck 83 km away on Sep 12, 06:38 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.4 32 km 160 km 3 km NNW of Knik, Alaska
before 1.8 51 km 188 km 27 km NNE of Point Possession, Alaska
before 2.0 5 km 218 km 82 km ENE of Lime Village, Alaska
before 1.9 55 km 134 km 81 km N of Chickaloon, Alaska
before 1.4 124 km 24 km 60 km N of Petersville, Alaska
before 2.3 111 km 45 km 70 km WSW of Cantwell, Alaska
before 1.9 122 km 39 km 69 km ESE of Denali National Park, Alaska
before 1.4 18 km 189 km 26 km SSE of Chickaloon, Alaska
before 2.4 75 km 76 km 50 km SSW of Cantwell, Alaska
before 2.4 87 km 9 km 30 km N of Petersville, Alaska
before 2.0 9 km 217 km 45 km WSW of Manley Hot Springs, Alaska
before 1.9 5 km 51 km 43 km SE of Denali National Park, Alaska
before 1.8 0 km 50 km 43 km SE of Denali National Park, Alaska
before 2.1 53 km 93 km 7 km ESE of Susitna North, Alaska
before 1.8 89 km 69 km 39 km N of Skwentna, Alaska
before 1.1 6 km 243 km 23 km S of South Van Horn, Alaska
before 1.7 16 km 139 km 78 km NW of Eureka Roadhouse, Alaska
before 1.7 32 km 234 km 20 km SW of Hope, Alaska
before 2.0 110 km 79 km 32 km W of Cantwell, Alaska
before 1.1 5 km 204 km 44 km SSE of Manley Hot Springs, Alaska
before 2.5 25 km 249 km 18 km N of Cooper Landing, Alaska
before 2.8 8 km 196 km 10 km SE of Anchorage, Alaska
before 1.2 14 km 223 km 13 km NNE of Four Mile Road, Alaska
before 2.0 28 km 150 km 4 km NW of Big Lake, Alaska
before 1.8 21 km 137 km 63 km N of Chickaloon, Alaska
before 2.2 21 km 149 km 27 km N of Chickaloon, Alaska
before 1.9 77 km 122 km 54 km SE of Cantwell, Alaska
before 1.7 15 km 227 km 50 km SE of Knik River, Alaska
before 2.4 24 km 181 km 31 km WSW of Point MacKenzie, Alaska
before 1.1 5 km 242 km 50 km NNW of Paxson, 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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