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Earthquake · Tuesday, November 3, 2026

Magnitude 4.7 earthquake 10 km N of Delta, B.C., MX

A magnitude 4.7 (light) earthquake struck 10 km N of Delta, B.C., MX on Tuesday, November 3, 2026 at , at a depth of 16 km (shallow).

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Magnitude
4.7Light
Depth
16km · shallow
Time
Epicenter
32.44° N
115.18° W
Aftershocks so far
0within 250 km
Largest aftershock
—

6 days ago · USGS id ci41572064 · last revised

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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 4.7 means

Light earthquakes are widely felt near the epicenter, rattling windows and shelves, but rarely cause damage.

A magnitude 4.7 releases about 31 times the seismic energy of a magnitude 3.7, roughly the energy of 168 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

0 aftershocks and 100 earlier earthquakes within 250 km in the 30 days around this event. Aftershock rates fall off quickly in the first days (Omori's law); the largest aftershock is typically about one magnitude unit smaller than the mainshock (Båth's law), here around magnitude 3.5.

Time (UTC)MagnitudeDepthDistanceLocation
before 1.7 15 km 193 km 8 km W of Palomar Observatory, CA
before 1.2 4 km 179 km 11 km S of Anza, CA
before 1.1 19 km 165 km 20 km SSW of La Quinta, CA
before 1.0 12 km 134 km 11 km SE of Borrego Springs, CA
before 0.9 10 km 132 km 20 km ESE of Julian, CA
before 1.9 18 km 243 km 5 km ESE of Yucaipa, CA
before 1.0 30 km 224 km 8 km NE of Cabazon, CA
before 1.0 10 km 138 km 16 km SW of Oasis, CA
before 2.5 12 km 195 km 9 km WNW of Anza, CA
before 1.8 13 km 197 km 11 km S of Idyllwild, CA
before 1.6 12 km 233 km 14 km WNW of Morongo Valley, CA
before 1.8 10 km 121 km 10 km NNE of Ocotillo Wells, CA
before 1.8 10 km 121 km 10 km NNE of Ocotillo Wells, CA
before 1.1 13 km 192 km 8 km N of Anza, CA
before 1.1 11 km 166 km 22 km ESE of Anza, CA
before 1.2 10 km 129 km 12 km WNW of Ocotillo Wells, CA
before 1.1 3 km 209 km 14 km ENE of Temecula, CA
before 1.3 4 km 94 km 6 km WSW of Niland, CA
before 1.7 12 km 194 km 9 km WNW of Anza, CA
before 1.3 8 km 172 km 16 km N of Warner Springs, CA
before 1.2 14 km 193 km 8 km N of Anza, CA
before 1.5 14 km 193 km 8 km NNW of Anza, CA
before 1.2 9 km 193 km 7 km NNW of Anza, CA
before 1.1 28 km 238 km 8 km NNE of Beaumont, CA
before 1.0 14 km 193 km 8 km N of Anza, CA
before 2.1 14 km 193 km 8 km NNW of Anza, CA
before 1.0 17 km 192 km 9 km N of Anza, CA
before 1.0 12 km 192 km 8 km N of Anza, CA
before 1.5 14 km 193 km 8 km NNW of Anza, CA
before 1.0 13 km 168 km 19 km ESE of Anza, 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.

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