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Earthquake · Saturday, October 24, 2026

Magnitude 4.6 earthquake 208 km WSW of Pistol River, Oregon

A magnitude 4.6 (light) earthquake struck 208 km WSW of Pistol River, Oregon on Saturday, October 24, 2026 at , at a depth of 10 km (shallow).

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Magnitude
4.6Light
Depth
10km · shallow
Time
Epicenter
41.88° N
126.85° W
Aftershocks so far
12within 250 km
Largest aftershock
5.0M

19 days ago · USGS id us6000u4q4 · 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 4.6 means

Light earthquakes are widely felt near the epicenter, rattling windows and shelves, but rarely cause damage.

A magnitude 4.6 releases about 32 times the seismic energy of a magnitude 3.6, roughly the energy of 120 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 5.0 struck 195 km away on Nov 5, 04:56 UTC, so this is most likely one of its foreshocks.

Time (UTC)MagnitudeDepthDistanceLocation
3.8 10 km 111 km 246 km W of Ferndale, California
3.1 10 km 138 km 210 km W of Port Orford, Oregon
5.0 10 km 195 km 111 km W of Petrolia, CA
1.6 12 km 244 km 10 km NNW of Bandon, Oregon
2.7 10 km 213 km 79 km W of Petrolia, CA
2.8 13 km 228 km 61 km W of Petrolia, CA
2.8 17 km 236 km 52 km W of Petrolia, CA
2.8 10 km 194 km 102 km W of Petrolia, CA
2.6 10 km 188 km 70 km WNW of Bayview, CA
2.0 23 km 242 km 14 km WNW of Bayview, CA
2.8 10 km 156 km 236 km W of Ferndale, California
2.1 5 km 165 km 51 km WSW of Port Orford, Oregon
before 2.6 10 km 24 km 186 km W of Pistol River, Oregon
before 2.8 10 km 18 km 193 km WSW of Pistol River, Oregon
before 2.2 6 km 242 km 19 km WNW of Ferndale, CA
before 2.2 5 km 241 km 20 km WNW of Ferndale, CA
before 1.7 4 km 212 km 1 km NW of Brookings, Oregon
before 3.0 23 km 210 km 60 km W of Ferndale, CA
before 1.6 1 km 157 km 58 km W of Nesika Beach, Oregon
before 2.8 10 km 160 km 238 km W of Ferndale, California
before 1.6 -1 km 222 km 11 km NNE of Nesika Beach, Oregon
before 3.1 24 km 181 km 80 km W of Bayview, CA
before 2.7 10 km 216 km 74 km W of Petrolia, CA
before 2.6 10 km 53 km 186 km WSW of Port Orford, Oregon
before 1.5 13 km 195 km 25 km WNW of Crescent City, California
before 2.9 4 km 219 km 75 km W of Petrolia, CA
before 2.8 25 km 234 km 44 km WNW of Petrolia, CA
before 2.8 10 km 136 km 235 km W of Ferndale, California
before 4.7 2 km 199 km 100 km W of Petrolia, CA

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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