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Earthquake · Thursday, October 15, 2026

Magnitude 5.6 earthquake 43 km NNW of Lake Minchumina, Alaska

A magnitude 5.6 (moderate) earthquake struck 43 km NNW of Lake Minchumina, Alaska on Thursday, October 15, 2026 at , at a depth of 5 km (shallow).

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Magnitude
5.6Moderate
Depth
5km · shallow
Time
Epicenter
64.22° N
152.75° W
Aftershocks so far
0within 250 km
Largest aftershock
—

26 days ago · USGS id aka2026ukynnb · 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 5.6 means

Moderate earthquakes are felt by everyone nearby and can cause minor to moderate damage close to the epicenter, mostly to weaker structures.

A magnitude 5.6 releases about 32 times the seismic energy of a magnitude 4.6, roughly the energy of 4 thousand 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

0 aftershocks and 100 earlier earthquakes within 250 km in the 30 days around this event. Aftershock rates fall off quickly in the first days (Omori's law); the largest aftershock is typically about one magnitude unit smaller than the mainshock (Båth's law), here around magnitude 4.4.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.9 131 km 152 km 66 km ESE of Denali National Park, Alaska
before 1.3 7 km 80 km 55 km SW of Manley Hot Springs, Alaska
before 2.6 66 km 236 km 48 km NE of Chase, Alaska
before 2.2 90 km 189 km 33 km WNW of Petersville, Alaska
before 1.3 5 km 223 km 53 km WNW of Skwentna, Alaska
before 1.2 5 km 185 km 20 km N of Four Mile Road, Alaska
before 1.6 5 km 229 km 102 km W of Skwentna, Alaska
before 1.3 5 km 248 km 59 km E of Denali Park, Alaska
before 1.5 18 km 91 km 47 km SSW of Manley Hot Springs, Alaska
before 1.9 122 km 153 km 67 km ESE of Denali National Park, Alaska
before 2.0 81 km 213 km 3 km NW of Petersville, Alaska
before 1.9 78 km 243 km 15 km NNW of Skwentna, Alaska
before 2.0 5 km 242 km 11 km W of Trapper Creek, Alaska
before 2.9 68 km 201 km 43 km N of Chase, Alaska
before 2.0 124 km 161 km 55 km NNW of Petersville, Alaska
before 2.2 0 km 98 km 7 km SE of Denali National Park, Alaska
before 4.2 5 km 98 km 7 km SE of Denali National Park, Alaska
before 3.1 114 km 200 km 7 km ENE of Denali Park, Alaska
before 1.4 7 km 195 km 52 km NW of Rampart, Alaska
before 2.3 70 km 221 km 13 km SW of Petersville, Alaska
before 1.4 11 km 212 km 23 km WSW of Petersville, Alaska
before 2.6 62 km 243 km 37 km ENE of Chase, Alaska
before 2.6 112 km 166 km 73 km NNE of Petersville, Alaska
before 3.0 5 km 178 km 71 km WNW of Petersville, Alaska
before 1.1 16 km 200 km 31 km SE of Minto, Alaska
before 2.3 1 km 125 km 55 km E of Denali National Park, Alaska
before 1.5 1 km 233 km 60 km ENE of Ferry, Alaska
before 2.1 3 km 237 km 11 km SW of South Van Horn, Alaska
before 2.1 5 km 236 km 44 km NE of Chase, Alaska
before 1.3 14 km 213 km 21 km NE of Minto, 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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