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Earthquake · Monday, September 14, 2026

Magnitude 2.4 earthquake 18 km NNW of Nikiski, Alaska

A magnitude 2.4 (micro) earthquake struck 18 km NNW of Nikiski, Alaska on Monday, September 14, 2026 at , at a depth of 74 km (intermediate).

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Magnitude
2.4Micro
Depth
74km · intermediate
Time
Epicenter
60.84° N
151.40° W
Aftershocks so far
0within 250 km
Largest aftershock
—

56 days ago · USGS id aka2026sgjhoe · 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.

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 3.4 struck 144 km away on Sep 3, 23:21 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.8 105 km 170 km 61 km WNW of Nanwalek, Alaska
before 1.7 79 km 158 km 30 km SSW of Petersville, Alaska
before 1.9 63 km 237 km 47 km NE of Chase, Alaska
before 1.5 121 km 115 km 73 km E of Port Alsworth, Alaska
before 2.2 15 km 200 km 40 km NNE of Chenega, Alaska
before 1.0 42 km 166 km 23 km ESE of Knik River, Alaska
before 1.7 5 km 188 km 44 km E of Knik River, Alaska
before 1.5 2 km 233 km 43 km WNW of Valdez, Alaska
before 1.6 37 km 244 km 41 km NW of Eureka Roadhouse, Alaska
before 1.7 20 km 45 km 17 km ESE of Beluga, Alaska
before 2.5 78 km 26 km 16 km W of Salamatof, Alaska
before 2.6 66 km 139 km 32 km NW of Willow, Alaska
before 2.3 113 km 112 km 65 km WNW of Happy Valley, Alaska
before 1.8 79 km 57 km 33 km W of Cohoe, Alaska
before 2.0 74 km 147 km 39 km WSW of Anchor Point, Alaska
before 2.3 81 km 160 km 31 km SW of Petersville, Alaska
before 2.3 1 km 127 km 20 km NW of Willow, Alaska
before 1.3 4 km 79 km 78 km WNW of Tyonek, Alaska
before 2.2 80 km 110 km 36 km W of Happy Valley, Alaska
before 2.0 71 km 178 km 49 km W of Nanwalek, Alaska
before 2.8 123 km 248 km 61 km N of Petersville, Alaska
before 2.3 105 km 172 km 59 km WNW of Nanwalek, Alaska
before 2.2 115 km 158 km 64 km ESE of Pedro Bay, Alaska
before 2.0 119 km 136 km 61 km W of Anchor Point, Alaska
before 2.4 93 km 165 km 25 km SW of Petersville, Alaska
before 2.3 15 km 136 km 8 km N of Meadow Lakes, Alaska
before 1.8 132 km 155 km 48 km E of Pedro Bay, Alaska
before 2.0 91 km 159 km 31 km N of Skwentna, Alaska
before 1.5 30 km 112 km 3 km NE of Big Lake, Alaska
before 1.8 5 km 77 km 77 km WNW of Tyonek, 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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