Earthquake · Friday, September 11, 2026
Magnitude 1.9 earthquake 6 km SW of Santa Paula, CA
A magnitude 1.9 (micro) earthquake struck 6 km SW of Santa Paula, CA on Friday, September 11, 2026 at , at a depth of 10 km (shallow).
- Magnitude
- 1.9Micro
- Depth
- 10km · shallow
- Time
- Epicenter
- 34.31° N
119.10° W - Aftershocks so far
- 0within 250 km
- Largest aftershock
- —
59 days ago · USGS id ci41544928 · 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 1.9 means
Micro earthquakes are generally not felt and are recorded only by seismographs.
A magnitude 1.9 releases about 30 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 3.4 struck 143 km away on Sep 2, 12:37 UTC, so this is most likely one of its aftershocks.
| Time (UTC) | Magnitude | Depth | Distance | Location |
|---|---|---|---|---|
| before | 1.1 | 10 km | 207 km | 10 km N of Big Bear City, CA |
| before | 1.0 | 4 km | 198 km | 5 km NNW of Beaumont, CA |
| before | 1.0 | 4 km | 198 km | 5 km NNW of Beaumont, CA |
| before | 1.2 | 18 km | 217 km | 11 km N of Cabazon, CA |
| before | 1.5 | 7 km | 163 km | 16 km WSW of Johannesburg, CA |
| before | 1.6 | 16 km | 227 km | 5 km SW of Idyllwild, CA |
| before | 0.9 | 7 km | 207 km | 12 km ENE of Ridgecrest, CA |
| before | 1.0 | 4 km | 142 km | 11 km ENE of North Tustin, CA |
| before | 1.7 | 3 km | 142 km | 11 km ENE of North Tustin, CA |
| before | 1.5 | -1 km | 152 km | 5 km NW of Boron, CA |
| before | 1.6 | 18 km | 97 km | 3 km WSW of Paramount, CA |
| before | 1.6 | 7 km | 57 km | 3 km WSW of Sylmar, CA |
| before | 1.3 | 3 km | 198 km | 5 km NNW of Beaumont, CA |
| before | 1.1 | 16 km | 78 km | 7 km NNW of Grapevine, CA |
| before | 1.0 | 4 km | 199 km | 5 km N of Beaumont, CA |
| before | 1.1 | 3 km | 198 km | 5 km NNW of Beaumont, CA |
| before | 1.3 | 30 km | 172 km | 4 km W of Highland, CA |
| before | 1.1 | 15 km | 191 km | 20 km NE of Kernville, CA |
| before | 1.1 | 7 km | 163 km | 17 km WSW of Johannesburg, CA |
| before | 1.0 | 16 km | 221 km | 7 km NE of Cabazon, CA |
| before | 1.4 | 3 km | 133 km | 3 km SSE of Villa Park, CA |
| before | 1.1 | 17 km | 213 km | 6 km NNW of Cabazon, CA |
| before | 1.8 | 17 km | 213 km | 6 km NNW of Cabazon, CA |
| before | 1.4 | 3 km | 227 km | 11 km ENE of Coso Junction, CA |
| before | 3.1 | 3 km | 227 km | 10 km ENE of Coso Junction, CA |
| before | 1.5 | 13 km | 173 km | 5 km S of Loma Linda, CA |
| before | 1.7 | 6 km | 164 km | 16 km WSW of Johannesburg, CA |
| before | 1.6 | 5 km | 208 km | 8 km W of Templeton, CA |
| before | 1.0 | 8 km | 151 km | 8 km N of Fontana, CA |
| before | 1.1 | 6 km | 200 km | 10 km N of Big Bear Lake, 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.