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Earthquake · Saturday, September 5, 2026

Magnitude 4.7 earthquake 95 km ESE of Isangel, Vanuatu

A magnitude 4.7 (light) earthquake struck 95 km ESE of Isangel, Vanuatu on Saturday, September 5, 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
4.7Light
Depth
10km · shallow
Time
Epicenter
19.91° S
170.10° E
Aftershocks so far
39within 250 km
Largest aftershock
6.6M

65 days ago · USGS id us7000tel1 · 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 32 times the seismic energy of a magnitude 3.7, roughly the energy of 169 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 6.6 struck 219 km away on Sep 25, 21:23 UTC, so this is most likely one of its foreshocks.

Time (UTC)MagnitudeDepthDistanceLocation
5.0 10 km 212 km 83 km NE of Tadine, New Caledonia
4.8 10 km 221 km 75 km NE of Tadine, New Caledonia
5.0 10 km 224 km 77 km ENE of Tadine, New Caledonia
5.3 10 km 218 km 76 km NE of Tadine, New Caledonia
5.2 10 km 227 km 67 km ENE of Tadine, New Caledonia
4.6 10 km 231 km 63 km ENE of Tadine, New Caledonia
5.1 10 km 217 km 78 km ENE of Tadine, New Caledonia
5.3 10 km 224 km 69 km NE of Tadine, New Caledonia
5.1 10 km 211 km 90 km ENE of Tadine, New Caledonia
5.0 10 km 240 km 61 km ENE of Tadine, New Caledonia
4.8 10 km 227 km 74 km ENE of Tadine, New Caledonia
5.1 10 km 228 km 74 km ENE of Tadine, New Caledonia
4.8 14 km 208 km 86 km NE of Tadine, New Caledonia
5.2 10 km 235 km 58 km NE of Tadine, New Caledonia
5.0 10 km 217 km 76 km NE of Tadine, New Caledonia
4.7 10 km 223 km 73 km ENE of Tadine, New Caledonia
4.9 10 km 221 km 73 km ENE of Tadine, New Caledonia
4.8 10 km 216 km 78 km ENE of Tadine, New Caledonia
4.8 10 km 196 km 97 km NE of Tadine, New Caledonia
4.7 10 km 224 km 71 km ENE of Tadine, New Caledonia
4.7 10 km 196 km 97 km NE of Tadine, New Caledonia
5.0 10 km 217 km 78 km ENE of Tadine, New Caledonia
5.0 10 km 213 km 84 km ENE of Tadine, New Caledonia
5.1 10 km 226 km 68 km NE of Tadine, New Caledonia
5.1 10 km 229 km 64 km ENE of Tadine, New Caledonia
5.3 10 km 236 km 58 km ENE of Tadine, New Caledonia
5.4 10 km 225 km 69 km ENE of Tadine, New Caledonia
5.5 10 km 237 km 61 km ENE of Tadine, New Caledonia
4.9 10 km 216 km 78 km NE of Tadine, New Caledonia
5.1 10 km 219 km 78 km ENE of Tadine, New Caledonia

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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