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Earthquake · Sunday, September 20, 2026

Magnitude 2.4 earthquake 65 km NE of Nikolai, Alaska

A magnitude 2.4 (micro) earthquake struck 65 km NE of Nikolai, Alaska on Sunday, September 20, 2026 at , at a depth of 1 km (shallow).

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Magnitude
2.4Micro
Depth
1km · shallow
Time
Epicenter
63.42° N
153.44° W
Aftershocks so far
0within 250 km
Largest aftershock
—

50 days ago · USGS id aka2026srohda · 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 2.4 means

Micro earthquakes are generally not felt and are recorded only by seismographs.

A magnitude 2.4 releases about 32 times the seismic energy of a magnitude 1.4, roughly the energy of 0 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

This event is part of a sequence: a larger magnitude 3.9 struck 230 km away on Sep 12, 06:38 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.5 26 km 231 km 14 km SW of Susitna North, Alaska
before 1.8 5 km 106 km 49 km SSE of Denali National Park, Alaska
before 1.3 5 km 233 km 15 km SSE of Denali Park, Alaska
before 1.6 34 km 249 km 9 km N of Susitna, Alaska
before 2.1 72 km 214 km 44 km SSW of Cantwell, Alaska
before 1.2 10 km 234 km 37 km WNW of Four Mile Road, Alaska
before 1.7 56 km 236 km 13 km ENE of Susitna North, Alaska
before 2.3 0 km 107 km 48 km SSE of Denali National Park, Alaska
before 1.0 11 km 230 km 5 km SW of Susitna North, Alaska
before 1.8 5 km 117 km 66 km W of Petersville, Alaska
before 1.7 5 km 104 km 34 km SSE of Denali National Park, Alaska
before 1.2 75 km 218 km 29 km SE of Skwentna, Alaska
before 2.1 0 km 139 km 52 km E of Denali National Park, Alaska
before 3.9 77 km 230 km 62 km S of Cantwell, Alaska
before 1.6 6 km 219 km 16 km NNW of Cantwell, Alaska
before 2.2 56 km 233 km 53 km ENE of Chase, Alaska
before 1.2 5 km 245 km 56 km WNW of Beluga, Alaska
before 1.8 122 km 146 km 67 km ESE of Denali National Park, Alaska
before 2.0 130 km 206 km 57 km SW of Skwentna, Alaska
before 2.0 116 km 136 km 52 km N of Petersville, Alaska
before 1.2 16 km 243 km 36 km W of Susitna, Alaska
before 2.0 5 km 91 km 32 km S of Denali National Park, Alaska
before 2.3 134 km 139 km 63 km SE of Denali National Park, Alaska
before 1.8 5 km 77 km 29 km SSW of Denali National Park, Alaska
before 1.8 0 km 243 km 64 km S of Cantwell, Alaska
before 2.1 5 km 101 km 20 km SE of Denali National Park, Alaska
before 2.6 127 km 148 km 69 km ESE of Denali National Park, Alaska
before 1.3 49 km 246 km 35 km NNW of Beluga, Alaska
before 2.1 0 km 247 km 63 km SSE of Cantwell, Alaska
before 1.9 74 km 238 km 42 km NNW of Beluga, 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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