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Earthquake · Friday, October 9, 2026

Magnitude 2.8 earthquake 32 km SE of Bodie, CA

A magnitude 2.8 (micro) earthquake struck 32 km SE of Bodie, CA on Friday, October 9, 2026 at , at a depth of 16 km (shallow).

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Magnitude
2.8Micro
Depth
16km · shallow
Time
Epicenter
38.03° N
118.73° W
Aftershocks so far
0within 250 km
Largest aftershock
—

32 days ago · USGS id nc75446746 · 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 2.8 means

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

A magnitude 2.8 releases about 33 times the seismic energy of a magnitude 1.8, 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

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 1.6.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.0 5 km 223 km 31 km N of Kernville, CA
before 1.0 5 km 59 km 18 km WSW of Toms Place, CA
before 1.1 1 km 164 km 58 km S of Kingston, Nevada
before 1.7 13 km 192 km 63 km ESE of Tonopah, Nevada
before 1.7 12 km 135 km 36 km N of Tonopah, Nevada
before 1.0 10 km 247 km 16 km E of Little Lake, CA
before 1.5 0 km 132 km 3 km WNW of Goldfield, Nevada
before 1.6 4 km 148 km 20 km ESE of Silver Springs, Nevada
before 1.9 3 km 148 km 20 km ESE of Silver Springs, Nevada
before 1.5 16 km 238 km 26 km NW of Kernville, CA
before 2.7 19 km 165 km 1 km S of Orange Cove, CA
before 1.1 3 km 59 km 15 km SSE of Mammoth Lakes, CA
before 1.5 1 km 213 km 15 km WSW of Firebaugh, CA
before 1.7 0 km 201 km 77 km ENE of Tonopah, Nevada
before 1.8 4 km 148 km 20 km ESE of Silver Springs, Nevada
before 1.1 2 km 231 km 10 km ENE of Coso Junction, CA
before 1.9 5 km 198 km 1 km WNW of Sun Valley, Nevada
before 1.9 5 km 163 km 58 km S of Kingston, Nevada
before 2.7 3 km 69 km 25 km SW of Toms Place, CA
before 2.6 13 km 198 km 1 km WNW of Sun Valley, Nevada
before 1.7 3 km 130 km 53 km S of Silver Peak, Nevada
before 1.8 4 km 130 km 52 km S of Silver Peak, Nevada
before 1.7 4 km 226 km 8 km SE of Porterville, CA
before 1.8 5 km 198 km 1 km WNW of Sun Valley, Nevada
before 1.9 6 km 128 km 50 km S of Silver Peak, Nevada
before 1.6 1 km 158 km 33 km SSE of Goldfield, Nevada
before 2.5 8 km 78 km 23 km NE of Hawthorne, Nevada
before 1.4 4 km 229 km 27 km NNE of Kernville, CA
before 1.8 0 km 155 km 58 km WNW of Beatty, Nevada
before 2.1 9 km 147 km 18 km SE of Silver Springs, Nevada

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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