Earthquake · Saturday, September 26, 2026
Magnitude 1.6 earthquake 9 km WSW of Grapevine, CA
A magnitude 1.6 (micro) earthquake struck 9 km WSW of Grapevine, CA on Saturday, September 26, 2026 at , at a depth of 9 km (shallow).
- Magnitude
- 1.6Micro
- Depth
- 9km · shallow
- Time
- Epicenter
- 34.92° N
119.03° W - Aftershocks so far
- 0within 250 km
- Largest aftershock
- —
47 days ago · USGS id ci41339615 · 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 1.6 means
Micro earthquakes are generally not felt and are recorded only by seismographs.
A magnitude 1.6 releases about 33 times the seismic energy of a magnitude 0.6, 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
This event is part of a sequence: a larger magnitude 3.4 struck 165 km away on Sep 2, 12:37 UTC, so this is most likely one of its aftershocks.
| Time (UTC) | Magnitude | Depth | Distance | Location |
|---|---|---|---|---|
| before | 2.0 | 7 km | 220 km | 22 km NE of San Lucas, CA |
| before | 1.1 | 6 km | 120 km | 16 km WSW of Johannesburg, CA |
| before | 2.8 | 7 km | 120 km | 16 km WSW of Johannesburg, CA |
| before | 1.2 | 4 km | 225 km | 16 km NNW of San Simeon, CA |
| before | 1.3 | 14 km | 188 km | 2 km NNE of Loma Linda, CA |
| before | 1.1 | 1 km | 167 km | 9 km ENE of Coso Junction, CA |
| before | 1.1 | 10 km | 209 km | 10 km N of Big Bear City, CA |
| before | 1.0 | 4 km | 214 km | 5 km NNW of Beaumont, CA |
| before | 1.0 | 4 km | 214 km | 5 km NNW of Beaumont, CA |
| before | 1.2 | 18 km | 230 km | 11 km N of Cabazon, CA |
| before | 1.5 | 7 km | 120 km | 16 km WSW of Johannesburg, CA |
| before | 1.6 | 16 km | 249 km | 5 km SW of Idyllwild, CA |
| before | 0.9 | 7 km | 158 km | 12 km ENE of Ridgecrest, CA |
| before | 1.0 | 4 km | 175 km | 11 km ENE of North Tustin, CA |
| before | 1.7 | 3 km | 175 km | 11 km ENE of North Tustin, CA |
| before | 1.5 | -1 km | 123 km | 5 km NW of Boron, CA |
| before | 1.6 | 18 km | 139 km | 3 km WSW of Paramount, CA |
| before | 1.6 | 7 km | 85 km | 3 km WSW of Sylmar, CA |
| before | 1.3 | 3 km | 214 km | 5 km NNW of Beaumont, CA |
| before | 1.1 | 16 km | 11 km | 7 km NNW of Grapevine, CA |
| before | 1.0 | 4 km | 215 km | 5 km N of Beaumont, CA |
| before | 1.1 | 3 km | 214 km | 5 km NNW of Beaumont, CA |
| before | 1.3 | 30 km | 185 km | 4 km W of Highland, CA |
| before | 1.1 | 15 km | 128 km | 20 km NE of Kernville, CA |
| before | 1.1 | 7 km | 119 km | 17 km WSW of Johannesburg, CA |
| before | 1.0 | 16 km | 236 km | 7 km NE of Cabazon, CA |
| before | 1.4 | 3 km | 168 km | 3 km SSE of Villa Park, CA |
| before | 1.1 | 17 km | 228 km | 6 km NNW of Cabazon, CA |
| before | 1.8 | 17 km | 228 km | 6 km NNW of Cabazon, CA |
| before | 1.9 | 10 km | 250 km | 13 km SE of Pinnacles, 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.