Earthquake · Wednesday, October 21, 2026
Magnitude 4.0 earthquake near Fiji region
A magnitude 4.0 (light) earthquake struck Fiji region on Wednesday, October 21, 2026 at , at a depth of 567 km (deep).
- Magnitude
- 4.0Light
- Depth
- 567km · deep
- Time
- Epicenter
- 19.49° S
177.59° W - Aftershocks so far
- 18within 250 km
- Largest aftershock
- 6.1M
20 days ago · USGS id us6000u3u9 · last revised
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 4.0 means
Light earthquakes are widely felt near the epicenter, rattling windows and shelves, but rarely cause damage.
A magnitude 4.0 releases about 32 times the seismic energy of a magnitude 3.0, roughly the energy of 15 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.
Deep earthquakes (below 300 km) happen far down in a sinking slab of oceanic plate. They are felt over very large distances but rarely cause damage, and they do not generate tsunamis.
Nearby earthquakes and aftershocks
This event is part of a sequence: a larger magnitude 6.1 struck 223 km away on Nov 5, 17:21 UTC, so this is most likely one of its foreshocks.
| Time (UTC) | Magnitude | Depth | Distance | Location |
|---|---|---|---|---|
| 4.3 | 596 km | 180 km | 226 km E of Levuka, Fiji | |
| 4.5 | 572 km | 190 km | Fiji region | |
| 4.3 | 567 km | 169 km | 263 km E of Levuka, Fiji | |
| 6.1 | 535 km | 223 km | Fiji region | |
| 4.3 | 559 km | 231 km | 218 km ENE of Levuka, Fiji | |
| 4.6 | 556 km | 26 km | Fiji region | |
| 4.4 | 542 km | 233 km | 252 km ENE of Levuka, Fiji | |
| 4.3 | 581 km | 169 km | 240 km E of Levuka, Fiji | |
| 4.4 | 576 km | 31 km | Fiji region | |
| 4.3 | 618 km | 172 km | 287 km E of Levuka, Fiji | |
| 4.8 | 372 km | 157 km | Fiji region | |
| 4.3 | 602 km | 200 km | 236 km E of Levuka, Fiji | |
| 4.2 | 640 km | 128 km | 291 km E of Levuka, Fiji | |
| 4.3 | 637 km | 136 km | 287 km E of Levuka, Fiji | |
| 5.5 | 642 km | 141 km | 283 km E of Levuka, Fiji | |
| 4.4 | 571 km | 242 km | 198 km ENE of Levuka, Fiji | |
| 4.3 | 463 km | 164 km | 289 km W of Houma, Tonga | |
| 4.2 | 625 km | 247 km | Fiji region | |
| before | 4.4 | 141 km | 177 km | 164 km W of Pangai, Tonga |
| before | 4.1 | 535 km | 74 km | 268 km WNW of Houma, Tonga |
| before | 4.3 | 592 km | 86 km | Fiji region |
| before | 4.2 | 591 km | 163 km | 240 km E of Levuka, Fiji |
| before | 4.4 | 559 km | 201 km | Fiji region |
| before | 4.3 | 279 km | 239 km | 236 km WSW of Houma, Tonga |
| before | 4.3 | 566 km | 229 km | 188 km E of Levuka, Fiji |
| before | 5.9 | 585 km | 216 km | Fiji region |
| before | 4.4 | 541 km | 243 km | 168 km E of Levuka, Fiji |
| before | 4.6 | 513 km | 100 km | 260 km WNW of Houma, Tonga |
| before | 4.6 | 560 km | 51 km | 268 km WNW of Houma, Tonga |
| before | 4.5 | 560 km | 212 km | 249 km E of Levuka, Fiji |
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.