EarthBrowser Open EarthBrowser

Earthquake · Saturday, October 10, 2026

Magnitude 1.9 earthquake 5 km ESE of Yucaipa, CA

A magnitude 1.9 (micro) earthquake struck 5 km ESE of Yucaipa, CA on Saturday, October 10, 2026 at , at a depth of 18 km (shallow).

Loading the live globe…
The epicenter (largest marker, center) on EarthBrowser’s globe with the other recent earthquakes in the region. Tap a marker to open its 3D cross-section; drag to look around.
Magnitude
1.9Micro
Depth
18km · shallow
Time
Epicenter
34.02° N
116.99° W
Aftershocks so far
0within 250 km
Largest aftershock
—

30 days ago · USGS id ci41345927 · last revised

Open in EarthBrowser Download on theApp Store

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 2.6 struck 135 km away on Sep 11, 10:19 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.5 20 km 124 km 3 km ESE of Lennox, CA
before 1.2 15 km 120 km 5 km NW of Willowbrook, CA
before 1.4 20 km 123 km 4 km E of Lennox, CA
before 1.9 12 km 150 km 20 km SW of Rancho Palos Verdes, CA
before 1.5 17 km 122 km 4 km N of Gardena, CA
before 2.0 11 km 77 km 12 km NNW of Warner Springs, CA
before 2.5 5 km 213 km 6 km SSW of Ojai, CA
before 1.5 21 km 123 km 3 km ESE of Lennox, CA
before 1.3 19 km 122 km 3 km ESE of Inglewood, CA
before 1.4 18 km 123 km 3 km ESE of Inglewood, CA
before 1.0 16 km 11 km 4 km NNW of Banning, CA
before 1.2 4 km 108 km 3 km W of Alhambra, CA
before 1.1 6 km 75 km 14 km N of Warner Springs, CA
before 1.3 16 km 122 km 4 km E of Lennox, CA
before 1.4 17 km 122 km 4 km ESE of Inglewood, CA
before 1.6 18 km 122 km 4 km E of Lennox, CA
before 1.6 4 km 12 km 2 km NW of Banning, CA
before 1.0 4 km 13 km 2 km NW of Banning, CA
before 1.1 2 km 121 km 4 km NW of Willowbrook, CA
before 1.6 19 km 121 km 4 km WNW of Willowbrook, CA
before 1.4 19 km 123 km 3 km ESE of Inglewood, CA
before 1.9 20 km 123 km 4 km ESE of Lennox, CA
before 1.3 4 km 213 km 7 km SSW of Ojai, CA
before 1.2 5 km 244 km 6 km NE of Coso Junction, CA
before 1.3 17 km 122 km 4 km ESE of Inglewood, CA
before 1.7 15 km 81 km 10 km NNE of Lake Henshaw, CA
before 1.1 8 km 111 km 5 km NNW of East Los Angeles, CA
before 1.7 5 km 213 km 8 km SSW of Ojai, CA
before 1.1 20 km 124 km 3 km E of Lennox, CA
before 2.1 6 km 213 km 8 km SSW of Ojai, 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.

More live views