EarthBrowser Open EarthBrowser

Earthquake · Saturday, October 3, 2026

Magnitude 1.5 earthquake 86 km W of Karluk, Alaska

A magnitude 1.5 (micro) earthquake struck 86 km W of Karluk, Alaska on Saturday, October 3, 2026 at , at a depth of 22 km (shallow).

Loading the live globe…
The epicenter (largest marker, center) on EarthBrowser’s globe with the other recent earthquakes in the region. Tap a marker to open its 3D cross-section; drag to look around.
Magnitude
1.5Micro
Depth
22km · shallow
Time
Epicenter
57.55° N
155.91° W
Aftershocks so far
0within 250 km
Largest aftershock
—

38 days ago · USGS id aka2026toiplx · last revised

Open in EarthBrowser Download on theApp Store

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 4.0 struck 154 km away on Sep 15, 14:32 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.0 5 km 88 km 85 km NNW of Karluk, Alaska
before 1.1 121 km 206 km 29 km NNW of Chignik Lagoon, Alaska
before 1.7 107 km 157 km 87 km SSE of Kokhanok, Alaska
before 1.8 8 km 97 km 73 km SSE of Ugashik, Alaska
before 2.4 52 km 184 km 49 km ESE of Chignik, Alaska
before 2.1 5 km 161 km 109 km E of Chignik, Alaska
before 1.3 67 km 51 km 36 km W of Karluk, Alaska
before 2.6 51 km 149 km 37 km WSW of Aleneva, Alaska
before 1.8 135 km 132 km 89 km S of Kokhanok, Alaska
before 2.3 55 km 223 km 40 km SSE of Chignik, Alaska
before 2.5 55 km 49 km 65 km SW of Karluk, Alaska
before 1.6 8 km 97 km 33 km W of Akhiok, Alaska
before 1.3 5 km 133 km 69 km SSW of Ugashik, Alaska
before 1.9 5 km 119 km 81 km SW of Akhiok, Alaska
before 1.3 5 km 123 km 95 km N of Karluk, Alaska
before 2.5 102 km 63 km 63 km SE of Ugashik, Alaska
before 1.7 26 km 73 km 16 km WSW of Karluk, Alaska
before 1.9 53 km 77 km 20 km SW of Karluk, Alaska
before 1.2 5 km 99 km 86 km NNW of Karluk, Alaska
before 1.7 5 km 247 km 60 km SE of Pedro Bay, Alaska
before 2.2 45 km 183 km 6 km S of Port Lions, Alaska
before 1.9 22 km 80 km 58 km W of Akhiok, Alaska
before 2.2 5 km 91 km 36 km SSE of Ugashik, Alaska
before 4.0 18 km 154 km 119 km E of Chignik, Alaska
before 2.0 5 km 183 km 35 km E of Chignik, Alaska
before 1.7 80 km 238 km 74 km WSW of Nanwalek, Alaska
before 1.2 5 km 248 km 60 km SE of Pedro Bay, Alaska
before 1.3 144 km 85 km 66 km SE of King Salmon, Alaska
before 1.3 79 km 62 km 28 km WNW of Karluk, Alaska
before 1.9 23 km 101 km 92 km SSE of Ugashik, 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.

More live views