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Earthquake · Saturday, September 26, 2026

Magnitude 1.5 earthquake 8 km NW of Harding-Birch Lakes, Alaska

A magnitude 1.5 (micro) earthquake struck 8 km NW of Harding-Birch Lakes, Alaska on Saturday, September 26, 2026 at , at a depth of 5 km (shallow).

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Magnitude
1.5Micro
Depth
5km · shallow
Time
Epicenter
64.43° N
146.70° W
Aftershocks so far
0within 250 km
Largest aftershock
—

44 days ago · USGS id aka2026tbwtfi · 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 1.5 means

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

A magnitude 1.5 releases about 32 times the seismic energy of a magnitude 0.5, 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 4.2 struck 219 km away on Sep 10, 05:18 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 3.4 1 km 158 km 45 km WNW of Central, Alaska
before 1.1 2 km 192 km 10 km ESE of Rampart, Alaska
before 1.2 10 km 151 km 37 km WNW of Four Mile Road, Alaska
before 1.5 0 km 185 km 19 km SSE of Rampart, Alaska
before 2.1 0 km 215 km 52 km E of Denali National Park, Alaska
before 3.9 77 km 212 km 62 km S of Cantwell, Alaska
before 1.6 6 km 151 km 16 km NNW of Cantwell, Alaska
before 2.2 56 km 234 km 53 km ENE of Chase, Alaska
before 1.0 4 km 68 km 16 km ENE of Fox, Alaska
before 1.8 122 km 230 km 67 km ESE of Denali National Park, Alaska
before 1.9 19 km 125 km 20 km N of Four Mile Road, Alaska
before 1.1 15 km 114 km 12 km NNE of Four Mile Road, Alaska
before 2.3 134 km 240 km 63 km SE of Denali National Park, Alaska
before 1.4 11 km 142 km 31 km NE of Paxson, Alaska
before 1.8 0 km 207 km 64 km S of Cantwell, Alaska
before 1.2 5 km 69 km 8 km E of Fox, Alaska
before 2.6 127 km 228 km 69 km ESE of Denali National Park, Alaska
before 1.7 72 km 186 km 61 km SSE of Cantwell, Alaska
before 1.2 2 km 117 km 11 km NNE of Four Mile Road, Alaska
before 2.1 0 km 202 km 63 km SSE of Cantwell, Alaska
before 1.7 0 km 173 km 73 km SE of Central, Alaska
before 1.5 13 km 60 km 14 km S of South Van Horn, Alaska
before 4.2 12 km 219 km 67 km WNW of Lake Louise, Alaska
before 2.0 87 km 193 km 33 km SW of Cantwell, Alaska
before 1.3 5 km 183 km 28 km S of Rampart, Alaska
before 1.3 5 km 185 km 30 km S of Rampart, Alaska
before 2.3 11 km 153 km 38 km WNW of Four Mile Road, Alaska
before 1.6 5 km 101 km 25 km NE of Ferry, Alaska
before 1.6 5 km 241 km 35 km SE of Tanana, Alaska
before 2.3 10 km 152 km 37 km WNW of Four Mile Road, 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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