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Earthquake · Thursday, September 10, 2026

Magnitude 3.8 earthquake 24 km W of Petrolia, CA

A magnitude 3.8 (minor) earthquake struck 24 km W of Petrolia, CA on Thursday, September 10, 2026 at , at a depth of 20 km (shallow).

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Magnitude
3.8Minor
Depth
20km · shallow
Time
Epicenter
40.29° N
124.57° W
Aftershocks so far
0within 250 km
Largest aftershock
—

61 days ago · USGS id nc75432947 · 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 3.8 means

Minor earthquakes are often felt by people nearby but almost never cause damage.

A magnitude 3.8 releases about 31 times the seismic energy of a magnitude 2.8, roughly the energy of 7 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 2.6.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.0 2 km 221 km 8 km W of Cobb, CA
before 1.8 3 km 232 km 3 km SE of The Geysers, CA
before 1.1 3 km 221 km 9 km WNW of The Geysers, CA
before 1.1 0 km 225 km 4 km WNW of The Geysers, CA
before 1.1 5 km 219 km 8 km ESE of Cloverdale, CA
before 1.1 2 km 225 km 5 km WNW of The Geysers, CA
before 1.0 2 km 222 km 8 km NW of The Geysers, CA
before 3.7 24 km 81 km 35 km E of Hydesville, CA
before 1.2 6 km 159 km 5 km NNW of Redwood Valley, CA
before 1.2 -1 km 232 km 2 km SE of The Geysers, CA
before 1.5 2 km 218 km 11 km WNW of Cobb, CA
before 2.3 15 km 15 km 11 km WSW of Petrolia, CA
before 1.3 6 km 219 km 7 km ESE of Cloverdale, CA
before 1.1 3 km 223 km 6 km WNW of The Geysers, CA
before 1.4 1 km 233 km 3 km SSE of The Geysers, CA
before 1.0 1 km 218 km 11 km NW of The Geysers, CA
before 1.4 6 km 219 km 7 km ESE of Cloverdale, CA
before 2.0 12 km 39 km 19 km SE of Petrolia, CA
before 1.1 2 km 223 km 5 km WNW of Cobb, CA
before 1.1 3 km 220 km 10 km WNW of The Geysers, CA
before 1.1 2 km 220 km 9 km WNW of The Geysers, CA
before 1.1 1 km 228 km 2 km N of The Geysers, CA
before 2.0 2 km 223 km 5 km WNW of Cobb, CA
before 2.0 7 km 150 km 8 km E of Willits, CA
before 2.3 2 km 229 km 3 km SSW of Cobb, CA
before 1.1 3 km 223 km 6 km NW of The Geysers, CA
before 1.9 1 km 231 km 2 km E of The Geysers, CA
before 1.0 1 km 228 km 2 km NNW of The Geysers, CA
before 0.9 1 km 222 km 7 km NW of The Geysers, CA
before 1.1 1 km 224 km 6 km W of Cobb, 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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