EarthBrowser Open EarthBrowser

Earthquake · Thursday, September 3, 2026

Magnitude 3.3 earthquake 48 km NE of Chase, Alaska

A magnitude 3.3 (minor) earthquake struck 48 km NE of Chase, Alaska on Thursday, September 3, 2026 at , at a depth of 72 km (intermediate).

Loading the live globe…
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
3.3Minor
Depth
72km · intermediate
Time
Epicenter
62.77° N
149.48° W
Aftershocks so far
80within 250 km
Largest aftershock
3.0M

67 days ago · USGS id aka2026rlkqil · last revised

Open in EarthBrowser Download on theApp Store

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 3.3 means

Minor earthquakes are often felt by people nearby but almost never cause damage.

A magnitude 3.3 releases about 32 times the seismic energy of a magnitude 2.3, roughly the energy of 1 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

80 aftershocks and 20 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 2.1.

Time (UTC)MagnitudeDepthDistanceLocation
2.1 5 km 33 km 69 km S of Cantwell, Alaska
1.4 4 km 115 km 55 km ENE of Cantwell, Alaska
1.2 5 km 223 km 36 km WNW of Four Mile Road, Alaska
2.3 81 km 102 km 31 km SW of Petersville, Alaska
1.6 13 km 229 km 37 km NE of Paxson, Alaska
2.3 1 km 110 km 20 km NW of Willow, Alaska
2.0 79 km 28 km 53 km SW of Cantwell, Alaska
1.3 4 km 227 km 78 km WNW of Tyonek, Alaska
2.8 123 km 67 km 61 km N of Petersville, Alaska
1.2 10 km 223 km 36 km WNW of Four Mile Road, Alaska
1.2 2 km 138 km 35 km W of Ferry, Alaska
2.4 93 km 96 km 25 km SW of Petersville, Alaska
1.3 5 km 210 km 44 km S of Manley Hot Springs, Alaska
2.8 18 km 207 km 46 km N of Valdez, Alaska
2.3 15 km 119 km 8 km N of Meadow Lakes, Alaska
2.6 14 km 207 km 48 km SSE of Nelchina, Alaska
1.1 5 km 231 km 27 km N of Four Mile Road, Alaska
1.8 119 km 70 km 70 km WSW of Cantwell, Alaska
2.0 91 km 111 km 31 km N of Skwentna, Alaska
1.3 47 km 203 km 48 km SSE of Nelchina, Alaska
1.0 5 km 222 km 35 km WNW of Four Mile Road, Alaska
1.1 8 km 224 km 38 km WNW of Four Mile Road, Alaska
1.2 6 km 223 km 37 km WNW of Four Mile Road, Alaska
1.5 30 km 138 km 3 km NE of Big Lake, Alaska
1.8 5 km 228 km 77 km WNW of Tyonek, Alaska
1.1 11 km 225 km 38 km WNW of Four Mile Road, Alaska
1.3 46 km 94 km 41 km NNE of Chickaloon, Alaska
1.8 129 km 79 km 64 km SE of Denali National Park, Alaska
1.6 75 km 212 km 4 km S of Tyonek, Alaska
1.3 7 km 210 km 44 km S of Manley Hot Springs, Alaska

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.

More live views