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Earthquake · Thursday, October 29, 2026

Magnitude 4.9 earthquake 111 km SW of Port-Vila, Vanuatu

A magnitude 4.9 (light) earthquake struck 111 km SW of Port-Vila, Vanuatu on Thursday, October 29, 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
4.9Light
Depth
10km · shallow
Time
Epicenter
18.50° S
167.63° E
Aftershocks so far
3within 250 km
Largest aftershock
4.6M

11 days ago · USGS id us7000ttyd · 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 4.9 means

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

A magnitude 4.9 releases about 32 times the seismic energy of a magnitude 3.9, roughly the energy of 338 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

3 aftershocks and 2 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 3.7.

Time (UTC)MagnitudeDepthDistanceLocation
4.5 247 km 175 km 87 km N of Isangel, Vanuatu
4.6 83 km 153 km 58 km WNW of Isangel, Vanuatu
4.6 10 km 52 km 59 km SW of Port-Vila, Vanuatu
before 4.9 22 km 209 km 73 km SW of Isangel, Vanuatu
before 4.8 10 km 31 km 98 km SW of Port-Vila, Vanuatu

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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