4 km South-East of Santa Maria di Licodia
A moderate earthquake, felt by people in the area. At only a few km deep the shaking is felt more sharply at the surface.
Where
4 km South-East of Santa Maria di LicodiaEarthquakes in the province of CataniaEarthquakes in SiciliaVolcanic area: Mount Etna
Here the ground shakes mostly because of moving magma and underground fluids, not colliding plates: events are typically shallow, frequent and organised in swarms. This activity is constantly monitored by INGV.
How far away could it be felt?
An estimate of how far people may have felt this quake.
- up to ~15 km · clearly felt by almost everyone≈ 352,000 people live in this area
- up to ~39 km · felt by many people, especially on upper floors≈ 1.1m people live in this area
- up to ~84 km · felt only by some, at rest≈ 2.7m people live in this area
The coloured rings on the map below show these distances.
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
61 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 ~4× compared to reality.
- Catania17 km from the epicentrefirst tremor in ~3 smain shaking in ~5 s
- Acireale20 km from the epicentrefirst tremor in ~3 smain shaking in ~6 s
- Siracusa72 km from the epicentrefirst tremor in ~12 smain shaking in ~21 s
- Modica78 km from the epicentrefirst tremor in ~13 smain shaking in ~22 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.
shallower than the area average (~13 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?
It is part of a seismic swarm: many closely spaced quakes in the same area, with no dominant shock. A typical, well-known behaviour of some Italian areas.
How often does it happen here?
Within 50 km of this epicentre, a magnitude ≥ 4.5 earthquake has occurred on average this often: 2 events in the last 11 years of the INGV catalogue.
An average computed on the recent past: it tells how used this area is to shaking, not when the next quake will come — earthquakes cannot be predicted.
The great earthquakes in this area's history
Almost a thousand years of catalogues: the strongest documented events within ~50 km.
Source: Parametric Catalogue of Italian Earthquakes CPTI15 (INGV, CC BY 4.0).
The closest seismic structure
The epicentre lies about 4 km from Gela-Catania, 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).