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Earthquake · Thursday, October 15, 2026

Magnitude 4.4 earthquake 63 km S of Champerico, Guatemala

A magnitude 4.4 (light) earthquake struck 63 km S of Champerico, Guatemala on Thursday, October 15, 2026 at , at a depth of 26 km (shallow).

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Magnitude
4.4Light
Depth
26km · shallow
Time
Epicenter
13.72° N
91.98° W
Aftershocks so far
20within 250 km
Largest aftershock
5.6M

26 days ago · USGS id us6000u2le · 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 4.4 means

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

A magnitude 4.4 releases about 32 times the seismic energy of a magnitude 3.4, roughly the energy of 60 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 121 km away on Nov 10, 14:54 UTC, so this is most likely one of its foreshocks.

Time (UTC)MagnitudeDepthDistanceLocation
4.8 59 km 126 km 34 km S of Puerto San José, Guatemala
5.6 35 km 121 km 43 km S of Puerto San José, Guatemala
4.5 34 km 61 km 77 km SW of La Gomera, Guatemala
4.2 58 km 122 km 30 km WSW of Puerto Madero, Mexico
4.1 35 km 137 km 86 km WSW of Puerto Madero, Mexico
4.3 10 km 121 km 99 km SW of Puerto Madero, Mexico
4.0 72 km 198 km 39 km S of La Esperanza (El Zapotal), Mexico
4.4 35 km 100 km 74 km SSW of Puerto Madero, Mexico
4.1 10 km 227 km 115 km SW of La Esperanza (El Zapotal), Mexico
4.1 39 km 198 km 69 km SSW of La Esperanza (El Zapotal), Mexico
4.2 182 km 158 km 4 km WSW of Patzité, Guatemala
4.6 49 km 237 km 97 km SW of El Palmarcito, Mexico
4.2 10 km 115 km 136 km SW of Brisas Barra de Suchiate, Mexico
4.6 99 km 105 km 4 km ENE of San José El Ídolo, Guatemala
4.3 10 km 109 km 113 km SW of Brisas Barra de Suchiate, Mexico
4.2 30 km 74 km 64 km SSW of La Gomera, Guatemala
5.2 10 km 101 km 86 km SW of Brisas Barra de Suchiate, Mexico
4.8 10 km 154 km 129 km SW of Puerto Madero, Mexico
4.8 117 km 197 km 2 km NW of Acacoyagua, Mexico
4.6 10 km 105 km 99 km SW of Brisas Barra de Suchiate, Mexico
before 4.5 35 km 20 km 43 km S of Champerico, Guatemala
before 4.1 10 km 111 km 85 km SW of Puerto Madero, Mexico
before 4.9 62 km 164 km 80 km SW of El Arenal, Mexico
before 4.5 10 km 154 km 121 km SW of Puerto Madero, Mexico
before 4.2 115 km 133 km 9 km SSW of Yepocapa, Guatemala
before 4.1 71 km 136 km 28 km SW of Buenos Aires, Mexico
before 4.2 10 km 164 km 120 km WSW of Puerto Madero, Mexico
before 4.7 89 km 103 km 7 km WNW of La Gomera, Guatemala
before 5.0 10 km 61 km 60 km SSW of Ocós, Guatemala

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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