Earthquake · Monday, October 26, 2026
Magnitude 1.1 earthquake 12 km ENE of Ridgecrest, CA
A magnitude 1.1 (micro) earthquake struck 12 km ENE of Ridgecrest, CA on Monday, October 26, 2026 at , at a depth of 4 km (shallow).
- Magnitude
- 1.1Micro
- Depth
- 4km · shallow
- Time
- Epicenter
- 35.66° N
117.55° W - Aftershocks so far
- 0within 250 km
- Largest aftershock
- —
14 days ago · USGS id ci41352719 · last revised
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 1.1 means
Micro earthquakes are generally not felt and are recorded only by seismographs.
A magnitude 1.1 releases about 30 times the seismic energy of a magnitude 0.1, 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 3.8 struck 179 km away on Sep 30, 03:00 UTC, so this is most likely one of its aftershocks.
| Time (UTC) | Magnitude | Depth | Distance | Location |
|---|---|---|---|---|
| before | 1.1 | 28 km | 243 km | 12 km NNW of Aguanga, CA |
| before | 1.6 | 0 km | 184 km | 39 km SSE of Sandy Valley, Nevada |
| before | 1.2 | 1 km | 98 km | 14 km SE of Tehachapi, CA |
| before | 1.0 | 12 km | 195 km | 24 km SW of Pine Mountain Club, CA |
| before | 1.4 | 2 km | 63 km | 12 km NNE of Coso Junction, CA |
| before | 1.4 | 2 km | 200 km | 2 km SSE of Home Gardens, CA |
| before | 1.0 | 16 km | 248 km | 7 km ENE of Anza, CA |
| before | 1.0 | -1 km | 159 km | 9 km NNW of Big Bear City, CA |
| before | 1.2 | 11 km | 196 km | 25 km SW of Pine Mountain Club, CA |
| before | 1.2 | 0 km | 214 km | 59 km SW of Rachel, Nevada |
| before | 1.6 | 16 km | 184 km | 3 km SE of Loma Linda, CA |
| before | 1.1 | 6 km | 248 km | 4 km WSW of Anza, CA |
| before | 1.6 | 6 km | 180 km | 3 km SSE of Piru, CA |
| before | 1.0 | 30 km | 226 km | 3 km W of Idyllwild, CA |
| before | 1.2 | 1 km | 170 km | 15 km NNW of Piru, CA |
| before | 1.3 | 1 km | 170 km | 16 km NNW of Piru, CA |
| before | 1.0 | 13 km | 244 km | 4 km NW of Anza, CA |
| before | 1.1 | 5 km | 174 km | 3 km E of Fontana, CA |
| before | 1.0 | 4 km | 249 km | 7 km WSW of Anza, CA |
| before | 1.3 | 3 km | 236 km | 18 km SSE of Mammoth Lakes, CA |
| before | 3.8 | 11 km | 179 km | 4 km SE of Piru, CA |
| before | 1.5 | 9 km | 204 km | 25 km SW of Maricopa, CA |
| before | 1.2 | 4 km | 58 km | 8 km NNE of Coso Junction, CA |
| before | 1.3 | 3 km | 28 km | 20 km ESE of Little Lake, CA |
| before | 1.3 | 5 km | 240 km | 9 km NNW of Avenal, CA |
| before | 1.5 | 4 km | 237 km | 7 km N of Goldfield, Nevada |
| before | 1.1 | 16 km | 186 km | 7 km ENE of Yucaipa, CA |
| before | 1.0 | 16 km | 227 km | 7 km ESE of Valle Vista, CA |
| before | 1.4 | 4 km | 28 km | 20 km ESE of Little Lake, CA |
| before | 1.7 | 6 km | 45 km | 16 km WSW of Johannesburg, 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.