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Earthquake · Monday, October 12, 2026

Magnitude 4.1 earthquake 85 km SW of Puerto Madero, Mexico

A magnitude 4.1 (light) earthquake struck 85 km SW of Puerto Madero, Mexico on Monday, October 12, 2026 at , at a depth of 10 km (shallow).

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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
4.1Light
Depth
10km · shallow
Time
Epicenter
14.12° N
92.93° W
Aftershocks so far
23within 250 km
Largest aftershock
5.6M

30 days ago · USGS id us6000u3v3 · 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 4.1 means

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

A magnitude 4.1 releases about 32 times the seismic energy of a magnitude 3.1, roughly the energy of 21 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 5.6 struck 230 km away on Nov 10, 14:54 UTC, so this is most likely one of its foreshocks.

Time (UTC)MagnitudeDepthDistanceLocation
4.8 59 km 235 km 34 km S of Puerto San José, Guatemala
5.6 35 km 230 km 43 km S of Puerto San José, Guatemala
4.5 34 km 173 km 77 km SW of La Gomera, Guatemala
4.2 58 km 59 km 30 km WSW of Puerto Madero, Mexico
4.1 35 km 28 km 86 km WSW of Puerto Madero, Mexico
4.3 10 km 15 km 99 km SW of Puerto Madero, Mexico
4.0 72 km 110 km 39 km S of La Esperanza (El Zapotal), Mexico
4.4 35 km 14 km 74 km SSW of Puerto Madero, Mexico
4.1 10 km 116 km 115 km SW of La Esperanza (El Zapotal), Mexico
4.1 39 km 96 km 69 km SSW of La Esperanza (El Zapotal), Mexico
4.2 182 km 203 km 4 km WSW of Patzité, Guatemala
4.6 49 km 128 km 97 km SW of El Palmarcito, Mexico
4.2 10 km 59 km 136 km SW of Brisas Barra de Suchiate, Mexico
4.6 99 km 171 km 4 km ENE of San José El Ídolo, Guatemala
4.0 111 km 189 km 13 km NNE of Pijijiapan, Mexico
4.3 10 km 34 km 113 km SW of Brisas Barra de Suchiate, Mexico
4.2 30 km 184 km 64 km SSW of La Gomera, Guatemala
5.2 10 km 11 km 86 km SW of Brisas Barra de Suchiate, Mexico
4.8 10 km 50 km 129 km SW of Puerto Madero, Mexico
4.8 117 km 139 km 2 km NW of Acacoyagua, Mexico
4.6 10 km 18 km 99 km SW of Brisas Barra de Suchiate, Mexico
4.4 26 km 111 km 63 km S of Champerico, Guatemala
4.5 35 km 108 km 43 km S of Champerico, Guatemala
before 4.9 62 km 62 km 80 km SW of El Arenal, Mexico
before 4.5 10 km 46 km 121 km SW of Puerto Madero, Mexico
before 4.2 115 km 212 km 9 km SSW of Yepocapa, Guatemala
before 4.1 71 km 73 km 28 km SW of Buenos Aires, Mexico
before 4.2 10 km 53 km 120 km WSW of Puerto Madero, Mexico
before 4.7 89 km 195 km 7 km WNW of La Gomera, Guatemala
before 4.2 143 km 182 km 15 km SW of El Ramal (Porvenir), Mexico

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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