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Earthquake · Sunday, October 18, 2026

Magnitude 4.4 earthquake 68 km ENE of Petropavlovsk-Kamchatsky, Russia

A magnitude 4.4 (light) earthquake struck 68 km ENE of Petropavlovsk-Kamchatsky, Russia on Sunday, October 18, 2026 at , at a depth of 73 km (intermediate).

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Magnitude
4.4Light
Depth
73km · intermediate
Time
Epicenter
53.20° N
159.63° E
Aftershocks so far
11within 250 km
Largest aftershock
5.3M

26 days ago · USGS id us6000u347 · 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.

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 6.9 struck 214 km away on Oct 16, 03:35 UTC, so this is most likely one of its aftershocks.

Time (UTC)MagnitudeDepthDistanceLocation
4.2 92 km 25 km 51 km ENE of Petropavlovsk-Kamchatsky, Russia
4.5 101 km 160 km 91 km SSW of Vilyuchinsk, Russia
4.7 76 km 19 km 74 km E of Petropavlovsk-Kamchatsky, Russia
4.4 97 km 83 km 35 km SE of Vilyuchinsk, Russia
5.0 10 km 219 km 205 km SSE of Vilyuchinsk, Russia
4.0 131 km 201 km 73 km SSE of Atlasovo, Russia
4.2 68 km 105 km 103 km SE of Vilyuchinsk, Russia
5.3 70 km 119 km 101 km SSE of Vilyuchinsk, Russia
4.2 29 km 188 km 178 km SSE of Vilyuchinsk, Russia
4.5 70 km 68 km 129 km ENE of Petropavlovsk-Kamchatsky, Russia
4.5 72 km 74 km 53 km SE of Vilyuchinsk, Russia
before 4.6 10 km 216 km 193 km E of Ozernovskiy, Russia
before 6.9 135 km 214 km 72 km NE of Ozernovskiy, Russia
before 4.9 10 km 199 km 190 km SSE of Vilyuchinsk, Russia
before 4.6 189 km 127 km 85 km N of Yelizovo, Russia
before 4.3 10 km 215 km 213 km SSE of Vilyuchinsk, Russia
before 4.4 10 km 194 km 197 km SE of Vilyuchinsk, Russia
before 4.9 10 km 185 km 184 km SSE of Vilyuchinsk, Russia
before 4.6 69 km 20 km 82 km E of Petropavlovsk-Kamchatsky, Russia
before 4.6 78 km 189 km 96 km NE of Ozernovskiy, Russia
before 4.8 10 km 162 km 191 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.7 34 km 114 km 138 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.4 84 km 14 km 58 km ENE of Petropavlovsk-Kamchatsky, Russia
before 4.8 10 km 239 km 194 km S of Ust’-Kamchatsk Staryy, Russia
before 5.1 10 km 184 km 182 km SSE of Vilyuchinsk, Russia
before 4.4 10 km 201 km 201 km SSE of Vilyuchinsk, Russia
before 4.2 10 km 159 km 189 km SE of Petropavlovsk-Kamchatsky, Russia
before 5.0 10 km 135 km 163 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.7 35 km 165 km 153 km SSE of Vilyuchinsk, Russia
before 4.4 93 km 146 km 52 km WSW of Paratunka, Russia

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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