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Earthquake · Monday, October 19, 2026

Magnitude 4.6 earthquake 4 km ENE of San José El Ídolo, Guatemala

A magnitude 4.6 (light) earthquake struck 4 km ENE of San José El Ídolo, Guatemala on Monday, October 19, 2026 at , at a depth of 99 km (intermediate).

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Magnitude
4.6Light
Depth
99km · intermediate
Time
Epicenter
14.46° N
91.38° W
Aftershocks so far
11within 250 km
Largest aftershock
5.6M

22 days ago · USGS id us6000u3cu · 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 4.6 means

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

A magnitude 4.6 releases about 32 times the seismic energy of a magnitude 3.6, roughly the energy of 120 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.

Intermediate-depth earthquakes (70 to 300 km) occur inside subducting slabs. The extra distance to the surface spreads the shaking over a wider area at lower intensity.

Nearby earthquakes and aftershocks

This event is part of a sequence: a larger magnitude 5.6 struck 116 km away on Nov 10, 14:54 UTC, so this is most likely one of its foreshocks.

Time (UTC)MagnitudeDepthDistanceLocation
4.8 59 km 112 km 34 km S of Puerto San José, Guatemala
5.6 35 km 116 km 43 km S of Puerto San José, Guatemala
4.5 34 km 106 km 77 km SW of La Gomera, Guatemala
4.2 58 km 141 km 30 km WSW of Puerto Madero, Mexico
4.1 35 km 187 km 86 km WSW of Puerto Madero, Mexico
4.3 10 km 186 km 99 km SW of Puerto Madero, Mexico
4.0 72 km 204 km 39 km S of La Esperanza (El Zapotal), Mexico
4.4 35 km 157 km 74 km SSW of Puerto Madero, Mexico
4.1 39 km 222 km 69 km SSW of La Esperanza (El Zapotal), Mexico
4.2 182 km 57 km 4 km WSW of Patzité, Guatemala
4.2 10 km 204 km 136 km SW of Brisas Barra de Suchiate, Mexico
before 4.0 111 km 244 km 13 km NNE of Pijijiapan, Mexico
before 4.3 10 km 187 km 113 km SW of Brisas Barra de Suchiate, Mexico
before 4.2 30 km 100 km 64 km SSW of La Gomera, Guatemala
before 5.2 10 km 166 km 86 km SW of Brisas Barra de Suchiate, Mexico
before 4.8 10 km 222 km 129 km SW of Puerto Madero, Mexico
before 4.8 117 km 173 km 2 km NW of Acacoyagua, Mexico
before 4.6 10 km 176 km 99 km SW of Brisas Barra de Suchiate, Mexico
before 4.4 26 km 105 km 63 km S of Champerico, Guatemala
before 4.5 35 km 88 km 43 km S of Champerico, Guatemala
before 4.1 10 km 171 km 85 km SW of Puerto Madero, Mexico
before 4.9 62 km 196 km 80 km SW of El Arenal, Mexico
before 4.5 10 km 216 km 121 km SW of Puerto Madero, Mexico
before 4.2 115 km 43 km 9 km SSW of Yepocapa, Guatemala
before 4.1 71 km 145 km 28 km SW of Buenos Aires, Mexico
before 4.2 10 km 221 km 120 km WSW of Puerto Madero, Mexico
before 4.7 89 km 48 km 7 km WNW of La Gomera, Guatemala
before 4.2 143 km 229 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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