3 km South of Orani
A very light earthquake, probably not felt by people. At only a few km deep the shaking is felt more sharply at the surface.
Where
3 km South of OraniEarthquakes in the province of NuoroEarthquakes in SardegnaHow far away could it be felt?
A quake this small is usually not felt by people: only seismographs record it.
Statistical estimate from the Italian intensity attenuation model (INGV): actual perception depends on geology, buildings and depth. Very shallow events can be felt locally even below the threshold.
Earthquake map
2 eventsThe energy released
How much energy this quake unleashed, translated into everyday comparisons.
Each extra magnitude unit releases about 32 times more energy: an M5 is not "a bit stronger" than an M4 — it is a different league.
Energy estimated with the standard Gutenberg–Richter relation; an average lightning bolt ≈ 1 billion joules. Indicative values.
The race of the seismic waves
Two waves set off from the hypocentre: the faster P wave arrives first with a sharp jolt; the S wave carries the actual shaking.
Animation sped up ~6× compared to reality.
- Olbia83 km from the epicentrefirst tremor in ~14 smain shaking in ~24 s
- Sassari85 km from the epicentrefirst tremor in ~14 smain shaking in ~24 s
- Cagliari114 km from the epicentrefirst tremor in ~19 smain shaking in ~33 s
- Quartu Sant'Elena116 km from the epicentrefirst tremor in ~19 smain shaking in ~33 s
Theoretical times with average crustal speeds: real values vary with geology. The gap between P and S waves is what earthquake early-warning systems rely on.
How deep it was born
At only a few km deep the shaking is felt more sharply at the surface.
in line with the area average (~2 km)
For the same magnitude, a shallow earthquake is felt much more than a deep one: the energy starts closer to the surface.
What kind of quake is this?
In the 30 days around this event no other quakes were recorded within 30 km: a one-off episode, very common in Italy.
The closest seismic structure
The epicentre lies about 205 km from Northern Africa offshore - East, one of the seismic structures mapped by INGV geologists.
Faults are mapped to build better and understand the territory: knowing them says nothing about when an earthquake will occur, which remains unpredictable. Source: DISS 3.3 (INGV, CC BY 4.0).
Other quakes in the area
Data: INGV — National Institute of Geophysics and Volcanology (CC-BY 4.0)
Estimates computed by Meteare on INGV data (Gutenberg–Richter relation; Italian macroseismic intensity attenuation model).