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Earthquake · Tuesday, October 27, 2026

Magnitude 2.6 earthquake 7 km SW of Nelson, Nevada

A magnitude 2.6 (micro) earthquake struck 7 km SW of Nelson, Nevada on Tuesday, October 27, 2026 at , at a depth of 13 km (shallow).

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Magnitude
2.6Micro
Depth
13km · shallow
Time
Epicenter
35.65° N
114.88° W
Aftershocks so far
0within 250 km
Largest aftershock
—

13 days ago · USGS id nn00926320 · 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 2.6 means

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

A magnitude 2.6 releases about 30 times the seismic energy of a magnitude 1.6, 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 63 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 1.4.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.1 2 km 233 km 6 km N of Big Bear City, CA
before 1.0 6 km 245 km 17 km W of Searles Valley, CA
before 2.5 -1 km 216 km 34 km WNW of Desert Center, CA
before 2.5 0 km 216 km 33 km WNW of Desert Center, CA
before 1.6 2 km 238 km 14 km SE of Big Bear City, CA
before 1.0 7 km 236 km 13 km SW of Searles Valley, CA
before 1.1 2 km 245 km 17 km W of Searles Valley, CA
before 1.8 2 km 172 km 26 km SSW of Alamo, Nevada
before 2.2 12 km 169 km 27 km SSW of Alamo, Nevada
before 1.5 1 km 209 km 29 km NNW of Barstow, CA
before 1.6 7 km 238 km 9 km NNE of Indio, CA
before 1.3 4 km 235 km 5 km NNW of Big Bear City, CA
before 1.7 16 km 205 km 21 km SSE of Caliente, Nevada
before 1.6 9 km 170 km 50 km S of Caliente, Nevada
before 2.0 1 km 168 km 27 km SSW of Alamo, Nevada
before 2.0 2 km 167 km 29 km SSW of Alamo, Nevada
before 1.3 5 km 228 km 24 km S of Trona, CA
before 1.6 12 km 241 km 14 km WNW of Morongo Valley, CA
before 1.9 3 km 85 km 18 km NNE of Nellis Air Force Base, Nevada
before 2.5 7 km 136 km 17 km NNE of Indian Springs, Nevada
before 1.6 3 km 228 km 20 km N of Searles Valley, CA
before 1.2 2 km 228 km 23 km N of Searles Valley, CA
before 1.2 10 km 230 km 10 km N of Big Bear City, CA
before 1.6 16 km 50 km 7 km SSW of Enterprise, Nevada
before 1.2 0 km 234 km 10 km NNW of Big Bear City, CA
before 1.5 0 km 63 km 40 km SSE of Sandy Valley, Nevada
before 1.0 10 km 249 km 9 km S of Big Bear Lake, CA
before 1.1 8 km 238 km 9 km NNE of Indio, CA
before 1.1 5 km 244 km 16 km W of Searles Valley, CA
before 1.4 1 km 220 km 24 km S of Twentynine Palms, 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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