Earthquake · Tuesday, September 15, 2026
Magnitude 3.3 earthquake 17 km WSW of Petrolia, CA
A magnitude 3.3 (minor) earthquake struck 17 km WSW of Petrolia, CA on Tuesday, September 15, 2026 at , at a depth of 9 km (shallow).
- Magnitude
- 3.3Minor
- Depth
- 9km · shallow
- Time
- Epicenter
- 40.29° N
124.48° W - Aftershocks so far
- 0within 250 km
- Largest aftershock
- —
55 days ago · USGS id nc75435962 · 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 3.3 means
Minor earthquakes are often felt by people nearby but almost never cause damage.
A magnitude 3.3 releases about 30 times the seismic energy of a magnitude 2.3, roughly the energy of 1 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 3.7 struck 74 km away on Sep 7, 21:44 UTC, so this is most likely one of its aftershocks.
| Time (UTC) | Magnitude | Depth | Distance | Location |
|---|---|---|---|---|
| before | 1.8 | 3 km | 228 km | 3 km SE of The Geysers, CA |
| before | 1.1 | 3 km | 216 km | 9 km WNW of The Geysers, CA |
| before | 1.1 | 0 km | 221 km | 4 km WNW of The Geysers, CA |
| before | 1.1 | 5 km | 215 km | 8 km ESE of Cloverdale, CA |
| before | 1.1 | 2 km | 220 km | 5 km WNW of The Geysers, CA |
| before | 1.0 | 2 km | 217 km | 8 km NW of The Geysers, CA |
| before | 3.7 | 24 km | 74 km | 35 km E of Hydesville, CA |
| before | 1.2 | 6 km | 154 km | 5 km NNW of Redwood Valley, CA |
| before | 1.2 | -1 km | 227 km | 2 km SE of The Geysers, CA |
| before | 1.5 | 2 km | 213 km | 11 km WNW of Cobb, CA |
| before | 2.3 | 15 km | 8 km | 11 km WSW of Petrolia, CA |
| before | 1.3 | 6 km | 214 km | 7 km ESE of Cloverdale, CA |
| before | 1.1 | 3 km | 218 km | 6 km WNW of The Geysers, CA |
| before | 1.4 | 1 km | 228 km | 3 km SSE of The Geysers, CA |
| before | 1.0 | 1 km | 214 km | 11 km NW of The Geysers, CA |
| before | 1.4 | 6 km | 214 km | 7 km ESE of Cloverdale, CA |
| before | 2.0 | 12 km | 32 km | 19 km SE of Petrolia, CA |
| before | 1.1 | 2 km | 218 km | 5 km WNW of Cobb, CA |
| before | 1.1 | 3 km | 215 km | 10 km WNW of The Geysers, CA |
| before | 1.1 | 2 km | 216 km | 9 km WNW of The Geysers, CA |
| before | 1.1 | 1 km | 223 km | 2 km N of The Geysers, CA |
| before | 2.0 | 2 km | 218 km | 5 km WNW of Cobb, CA |
| before | 2.0 | 7 km | 144 km | 8 km E of Willits, CA |
| before | 2.3 | 2 km | 224 km | 3 km SSW of Cobb, CA |
| before | 1.1 | 3 km | 218 km | 6 km NW of The Geysers, CA |
| before | 1.9 | 1 km | 226 km | 2 km E of The Geysers, CA |
| before | 1.0 | 1 km | 223 km | 2 km NNW of The Geysers, CA |
| before | 0.9 | 1 km | 218 km | 7 km NW of The Geysers, CA |
| before | 1.1 | 1 km | 219 km | 6 km W of Cobb, CA |
| before | 1.6 | 4 km | 239 km | 8 km E of Hidden Valley 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.