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Earthquake · Friday, October 9, 2026

Magnitude 1.9 earthquake 54 km S of Silver Peak, Nevada

A magnitude 1.9 (micro) earthquake struck 54 km S of Silver Peak, Nevada on Friday, October 9, 2026 at , at a depth of 6 km (shallow).

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The epicenter (largest marker, center) on EarthBrowser’s globe with the other recent earthquakes in the region. Tap a marker to open its 3D cross-section; drag to look around.
Magnitude
1.9Micro
Depth
6km · shallow
Time
Epicenter
37.28° N
117.52° W
Aftershocks so far
0within 250 km
Largest aftershock
—

31 days ago · USGS id nn00925541 · 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 1.9 means

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

A magnitude 1.9 releases about 27 times the seismic energy of a magnitude 0.9, 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

This event is part of a sequence: a larger magnitude 2.5 struck 179 km away on Sep 21, 23:39 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 2.5 8 km 179 km 23 km NE of Hawthorne, Nevada
before 1.5 8 km 220 km 18 km WSW of Johannesburg, CA
before 1.4 4 km 161 km 27 km NNE of Kernville, CA
before 1.5 9 km 219 km 18 km WSW of Johannesburg, CA
before 1.0 10 km 221 km 18 km WSW of Johannesburg, CA
before 1.3 2 km 174 km 15 km WSW of Searles Valley, CA
before 1.8 0 km 20 km 58 km WNW of Beatty, Nevada
before 1.2 -1 km 250 km 5 km NW of Boron, CA
before 1.4 3 km 132 km 13 km S of Olancha, CA
before 1.3 1 km 133 km 10 km NE of Coso Junction, CA
before 1.0 1 km 131 km 11 km N of Coso Junction, CA
before 1.7 16 km 225 km 20 km E of McFarland, CA
before 1.8 1 km 156 km 74 km ENE of Tonopah, Nevada
before 1.5 8 km 113 km 34 km SW of Independence, CA
before 2.3 4 km 112 km 10 km SW of Toms Place, CA
before 1.0 2 km 169 km 16 km W of Searles Valley, CA
before 1.6 2 km 240 km 13 km SE of Markleeville, CA
before 0.9 2 km 140 km 15 km E of Coso Junction, CA
before 1.0 8 km 185 km 18 km SSW of Searles Valley, CA
before 1.0 5 km 156 km 20 km ESE of Little Lake, CA
before 2.0 0 km 240 km 14 km SE of Markleeville, CA
before 1.1 6 km 213 km 14 km W of Johannesburg, CA
before 1.5 6 km 176 km 11 km NE of Ridgecrest, CA
before 1.5 8 km 225 km 36 km NNW of Nellis Air Force Base, Nevada
before 1.8 7 km 218 km 16 km WSW of Johannesburg, CA
before 1.6 6 km 116 km 10 km W of Toms Place, CA
before 1.4 9 km 95 km 15 km ENE of Toms Place, CA
before 1.3 3 km 217 km 26 km SE of Bodfish, CA
before 1.4 5 km 137 km 6 km NE of Coso Junction, CA
before 1.3 3 km 179 km 10 km ENE of Ridgecrest, 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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