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Earthquake · Wednesday, October 7, 2026

Magnitude 1.7 earthquake 92 km SE of Kokhanok, Alaska

A magnitude 1.7 (micro) earthquake struck 92 km SE of Kokhanok, Alaska on Wednesday, October 7, 2026 at , at a depth of 82 km (intermediate).

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Magnitude
1.7Micro
Depth
82km · intermediate
Time
Epicenter
58.81° N
153.73° W
Aftershocks so far
0within 250 km
Largest aftershock
—

33 days ago · USGS id aka2026twrvhm · 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 1.7 means

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

A magnitude 1.7 releases about 32 times the seismic energy of a magnitude 0.7, 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 2.9 struck 68 km away on Sep 11, 02:56 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.7 26 km 156 km 16 km WSW of Karluk, Alaska
before 1.9 53 km 164 km 20 km SW of Karluk, Alaska
before 2.4 53 km 85 km 52 km SSW of Nanwalek, Alaska
before 1.2 5 km 93 km 86 km NNW of Karluk, Alaska
before 1.7 53 km 205 km 16 km ESE of Fox River, Alaska
before 2.2 82 km 220 km 31 km WSW of Salamatof, Alaska
before 2.4 54 km 197 km 18 km SE of Fox River, Alaska
before 1.7 5 km 64 km 60 km SE of Pedro Bay, Alaska
before 2.2 45 km 122 km 6 km S of Port Lions, Alaska
before 2.7 82 km 129 km 35 km W of Anchor Point, Alaska
before 1.9 22 km 222 km 58 km W of Akhiok, Alaska
before 2.5 100 km 141 km 56 km WNW of Anchor Point, Alaska
before 1.9 86 km 242 km 19 km W of Nikiski, Alaska
before 1.7 91 km 159 km 53 km WNW of Happy Valley, Alaska
before 1.7 80 km 49 km 74 km WSW of Nanwalek, Alaska
before 1.2 5 km 64 km 60 km SE of Pedro Bay, Alaska
before 1.2 5 km 158 km 51 km E of Port Alsworth, Alaska
before 1.0 12 km 157 km 72 km WNW of Happy Valley, Alaska
before 1.2 106 km 167 km 45 km WNW of Ninilchik, Alaska
before 1.3 69 km 77 km 52 km SSW of Nanwalek, Alaska
before 1.1 75 km 164 km 15 km WNW of Happy Valley, Alaska
before 1.3 144 km 131 km 66 km SE of King Salmon, Alaska
before 1.3 79 km 144 km 28 km WNW of Karluk, Alaska
before 2.7 137 km 113 km 39 km E of Pedro Bay, Alaska
before 1.6 83 km 207 km 75 km WSW of Karluk, Alaska
before 2.1 82 km 131 km 20 km SW of Anchor Point, Alaska
before 1.6 70 km 209 km 14 km ESE of Clam Gulch, Alaska
before 1.3 32 km 99 km 43 km NNE of Larsen Bay, Alaska
before 1.4 83 km 146 km 33 km WNW of Anchor Point, Alaska
before 1.8 15 km 147 km 92 km SSE of Port Graham, 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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