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Earthquake · Friday, October 16, 2026

Magnitude 6.9 earthquake 76 km NE of Ozernovskiy, Russia

A magnitude 6.9 (strong) earthquake struck 76 km NE of Ozernovskiy, Russia on Friday, October 16, 2026 at , at a depth of 135 km (intermediate).

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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
6.9Strong
Depth
135km · intermediate
Time
Epicenter
51.98° N
157.27° E
Aftershocks so far
5within 250 km
Largest aftershock
5.3M

25 days ago · USGS id us6000u2mq · 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 6.9 means

Strong earthquakes can damage buildings near the epicenter, especially older or poorly built ones, and are felt over a wide area.

A magnitude 6.9 releases about 32 times the seismic energy of a magnitude 5.9, roughly the energy of 338 thousand 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

5 aftershocks and 21 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 5.7.

Time (UTC)MagnitudeDepthDistanceLocation
4.4 97 km 127 km 35 km SE of Vilyuchinsk, Russia
4.3 85 km 246 km 84 km S of Severo-Kuril’sk, Russia
5.0 10 km 178 km 205 km SSE of Vilyuchinsk, Russia
5.3 70 km 133 km 101 km SSE of Vilyuchinsk, Russia
4.3 78 km 206 km 67 km E of Petropavlovsk-Kamchatsky, Russia
before 4.9 10 km 190 km 198 km SSE of Vilyuchinsk, Russia
before 4.5 183 km 232 km 82 km SSW of Mil’kovo, Russia
before 4.9 10 km 189 km 180 km SE of Vilyuchinsk, Russia
before 4.6 69 km 213 km 82 km E of Petropavlovsk-Kamchatsky, Russia
before 4.6 78 km 22 km 96 km NE of Ozernovskiy, Russia
before 4.8 10 km 235 km 191 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.7 34 km 197 km 138 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.4 84 km 204 km 58 km ENE of Petropavlovsk-Kamchatsky, Russia
before 5.1 10 km 183 km 182 km SSE of Vilyuchinsk, Russia
before 4.4 10 km 198 km 201 km SSE of Vilyuchinsk, Russia
before 4.2 10 km 234 km 189 km SE of Petropavlovsk-Kamchatsky, Russia
before 5.0 10 km 216 km 163 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.7 35 km 154 km 153 km SSE of Vilyuchinsk, Russia
before 4.4 93 km 86 km 52 km WSW of Paratunka, Russia
before 5.0 31 km 183 km 171 km SE of Vilyuchinsk, Russia
before 4.9 39 km 146 km 136 km SSE of Vilyuchinsk, Russia
before 5.0 10 km 182 km 179 km SSE of Vilyuchinsk, Russia
before 5.8 29 km 173 km 165 km SSE of Vilyuchinsk, Russia
before 4.9 32 km 210 km 136 km SE of Petropavlovsk-Kamchatsky, Russia
before 5.0 35 km 212 km 142 km SE of Petropavlovsk-Kamchatsky, Russia
before 4.7 57 km 155 km 107 km SE of Vilyuchinsk, 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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