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Earthquake · Saturday, September 26, 2026

Magnitude 4.9 earthquake 78 km ESE of Kokopo, Papua New Guinea

A magnitude 4.9 (light) earthquake struck 78 km ESE of Kokopo, Papua New Guinea on Saturday, September 26, 2026 at , at a depth of 64 km (shallow).

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Magnitude
4.9Light
Depth
64km · shallow
Time
Epicenter
4.64° S
152.91° E
Aftershocks so far
25within 250 km
Largest aftershock
6.0M

47 days ago · USGS id us6000txv7 · 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

This event is part of a sequence: a larger magnitude 6.0 struck 127 km away on Oct 13, 18:45 UTC, so this is most likely one of its foreshocks.

Time (UTC)MagnitudeDepthDistanceLocation
4.3 56 km 158 km 121 km SW of Kokopo, Papua New Guinea
5.0 10 km 150 km 158 km S of Kokopo, Papua New Guinea
4.8 45 km 87 km 89 km S of Kokopo, Papua New Guinea
4.5 52 km 124 km 99 km SSW of Kokopo, Papua New Guinea
4.9 91 km 69 km 29 km S of Kokopo, Papua New Guinea
4.2 74 km 167 km 129 km SW of Kokopo, Papua New Guinea
4.4 10 km 122 km 138 km S of Kokopo, Papua New Guinea
5.1 10 km 95 km 127 km SSE of Kokopo, Papua New Guinea
4.7 10 km 162 km 152 km SSW of Kokopo, Papua New Guinea
4.1 407 km 154 km 198 km NW of Arawa, Papua New Guinea
4.3 10 km 130 km 144 km S of Kokopo, Papua New Guinea
4.5 10 km 114 km 127 km S of Kokopo, Papua New Guinea
4.9 35 km 114 km 126 km S of Kokopo, Papua New Guinea
4.7 10 km 112 km 124 km S of Kokopo, Papua New Guinea
4.6 10 km 32 km 73 km E of Kokopo, Papua New Guinea
4.6 10 km 94 km 120 km SSE of Kokopo, Papua New Guinea
4.5 10 km 111 km 129 km S of Kokopo, Papua New Guinea
6.0 22 km 127 km 128 km S of Kokopo, Papua New Guinea
4.3 10 km 124 km 122 km S of Kokopo, Papua New Guinea
4.7 10 km 118 km 133 km S of Kokopo, Papua New Guinea
4.6 49 km 120 km 115 km S of Kokopo, Papua New Guinea
5.1 27 km 124 km 122 km S of Kokopo, Papua New Guinea
5.3 31 km 128 km 129 km S of Kokopo, Papua New Guinea
4.9 21 km 25 km 55 km ESE of Kokopo, Papua New Guinea
5.1 28 km 124 km 121 km S of Kokopo, Papua New Guinea
before 5.6 58 km 10 km 74 km ESE of Kokopo, Papua New Guinea
before 5.1 94 km 70 km 32 km S of Kokopo, Papua New Guinea
before 5.2 96 km 176 km 139 km SW of Kokopo, Papua New Guinea
before 4.9 10 km 206 km 191 km ESE of Kimbe, Papua New Guinea
before 4.3 367 km 151 km 90 km NNE of Rabaul, Papua New Guinea

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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