EarthBrowserEarthquake · Friday, October 30, 2026
Magnitude 4.2 earthquake 269 km NNE of Lospalos, Timor Leste
A magnitude 4.2 (light) earthquake struck 269 km NNE of Lospalos, Timor Leste on Friday, October 30, 2026 at , at a depth of 361 km (deep).
- Magnitude
- 4.2Light
- Depth
- 361km · deep
- Time
- Epicenter
- 6.49° S
128.35° E - Aftershocks so far
- 4within 250 km
- Largest aftershock
- 5.1M
11 days ago · USGS id us7000tu97 · 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 4.2 means
Light earthquakes are widely felt near the epicenter, rattling windows and shelves, but rarely cause damage.
A magnitude 4.2 releases about 32 times the seismic energy of a magnitude 3.2, roughly the energy of 30 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 5.7 struck 229 km away on Oct 28, 22:06 UTC, so this is most likely one of its aftershocks.
| Time (UTC) | Magnitude | Depth | Distance | Location |
|---|---|---|---|---|
| 4.4 | 135 km | 211 km | Banda Sea | |
| 5.1 | 94 km | 183 km | Banda Sea | |
| 4.4 | 378 km | 89 km | 253 km S of Ambon, Indonesia | |
| 4.3 | 255 km | 65 km | Banda Sea | |
| before | 4.6 | 10 km | 218 km | Pulau Pulau Tanimbar, Indonesia |
| before | 5.7 | 142 km | 229 km | 271 km WSW of Tual, Indonesia |
| before | 4.3 | 141 km | 133 km | Banda Sea |
| before | 4.2 | 159 km | 141 km | 129 km NE of Lospalos, Timor Leste |
| before | 4.4 | 127 km | 229 km | 267 km WSW of Tual, Indonesia |
| before | 4.1 | 110 km | 109 km | 257 km ENE of Lospalos, Timor Leste |
| before | 4.5 | 128 km | 97 km | 207 km NE of Lospalos, Timor Leste |
| before | 4.0 | 134 km | 178 km | Banda Sea |
| before | 4.3 | 340 km | 213 km | 115 km NNE of Baukau, Timor Leste |
| before | 4.4 | 143 km | 150 km | Banda Sea |
| before | 5.1 | 123 km | 121 km | 164 km NE of Lospalos, Timor Leste |
| before | 4.3 | 49 km | 149 km | 188 km ENE of Lospalos, Timor Leste |
| before | 4.2 | 157 km | 100 km | 203 km NE of Lospalos, Timor Leste |
| before | 4.5 | 158 km | 176 km | Banda Sea |
| before | 4.4 | 133 km | 102 km | 235 km NE of Lospalos, Timor Leste |
| before | 4.4 | 173 km | 125 km | 286 km ENE of Lospalos, Timor Leste |
| before | 4.1 | 141 km | 170 km | Banda Sea |
| before | 4.1 | 111 km | 218 km | 278 km WSW of Tual, Indonesia |
| before | 4.7 | 10 km | 195 km | 214 km E of Lospalos, Timor Leste |
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.