Earthquake · Sunday, November 1, 2026
Magnitude 1.4 earthquake 15 km WSW of Johannesburg, CA
A magnitude 1.4 (micro) earthquake struck 15 km WSW of Johannesburg, CA on Sunday, November 1, 2026 at , at a depth of 7 km (shallow).
- Magnitude
- 1.4Micro
- Depth
- 7km · shallow
- Time
- Epicenter
- 35.34° N
117.80° W - Aftershocks so far
- 0within 250 km
- Largest aftershock
- —
12 days ago · USGS id ci41570728 · 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 1.4 means
Micro earthquakes are generally not felt and are recorded only by seismographs.
A magnitude 1.4 releases about 35 times the seismic energy of a magnitude 0.4, 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 2.7 struck 185 km away on Oct 4, 21:07 UTC, so this is most likely one of its aftershocks.
| Time (UTC) | Magnitude | Depth | Distance | Location |
|---|---|---|---|---|
| before | 1.7 | 11 km | 205 km | 11 km N of Goleta, CA |
| before | 1.2 | 16 km | 204 km | 10 km WSW of Idyllwild, CA |
| before | 1.3 | 19 km | 204 km | 10 km WSW of Idyllwild, CA |
| before | 1.2 | 3 km | 234 km | 11 km S of Anza, CA |
| before | 1.3 | 4 km | 157 km | 4 km SSW of Redlands, CA |
| before | 1.4 | 4 km | 157 km | 5 km SSW of Redlands, CA |
| before | 1.2 | 4 km | 157 km | 5 km SSW of Redlands, CA |
| before | 1.1 | 4 km | 156 km | 4 km SSW of Redlands, CA |
| before | 1.4 | 4 km | 157 km | 5 km SSW of Redlands, CA |
| before | 1.4 | 16 km | 205 km | 5 km SW of Idyllwild, CA |
| before | 1.0 | 10 km | 166 km | 4 km NNE of Villa Park, CA |
| before | 1.2 | 21 km | 153 km | 1 km WSW of Pico Rivera, CA |
| before | 1.0 | 9 km | 239 km | 18 km ESE of Anza, CA |
| before | 1.0 | 17 km | 156 km | 5 km SE of Loma Linda, CA |
| before | 1.5 | 1 km | 90 km | 13 km NNE of Coso Junction, CA |
| before | 1.6 | 17 km | 151 km | 1 km NW of Loma Linda, CA |
| before | 1.8 | 9 km | 246 km | 5 km WNW of Round Valley, California |
| before | 1.1 | 4 km | 241 km | 22 km ESE of Anza, CA |
| before | 1.1 | 15 km | 209 km | 9 km SSW of Idyllwild, CA |
| before | 1.3 | -1 km | 35 km | 5 km NNW of Boron, CA |
| before | 1.0 | 0 km | 130 km | 15 km NNW of Piru, CA |
| before | 1.0 | 7 km | 83 km | 27 km E of Coso Junction, CA |
| before | 1.0 | 15 km | 151 km | 1 km NNE of Loma Linda, CA |
| before | 1.1 | 14 km | 240 km | 20 km ESE of Anza, CA |
| before | 1.2 | 14 km | 213 km | 11 km NW of Anza, CA |
| before | 1.8 | 1 km | 118 km | 21 km E of Porterville, CA |
| before | 2.7 | 22 km | 185 km | 8 km WSW of Corcoran, CA |
| before | 1.2 | 3 km | 157 km | 5 km SSW of Redlands, CA |
| before | 1.1 | 15 km | 209 km | 8 km SSW of Idyllwild, CA |
| before | 1.6 | 3 km | 85 km | 10 km NE of Coso Junction, 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.