Live Data

Earthquake Monitoring — Italy and Southern Italy

All seismic events in real time from the INGV network, with a dedicated section for Southern Italy: Calabria, Sicily, Tyrrhenian Sea and Ionian Sea.

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🔴 Recent significant events (M ≥ 3.0)
Automatically detected by INGV monitoring and archived on this site.
📄 Latest event report

On August 1, 2026 at 01:20 (Italian time, 23:20 UTC) an earthquake of magnitude 3.1 (Md) was recorded by INGV in the Campi Flegrei area, at a depth of 0.6 km. Location reviewed by seismologists, based on 20 seismic stations. Source: INGV — Istituto Nazionale di Geofisica e Vulcanologia (Italy's National Institute of Geophysics and Volcanology).

Official INGV report for this earthquake →
📰 Related INGV in-depth analysis
Evento sismico, Md 4.7, ai Campi Flegrei e comunicato di sciame: 31 luglio 2026
«Alle ore 19:46 italiane (17:46 UTC) del 31 luglio 2026, nell’area dei Campi Flegrei, è avvenuto un terremoto di magnitudo Md 4.7, ad una profondità pari a circa 3 km,»
Read the full report on INGVterremoti →
How to cite this data

ISIDe Working Group (2007), Italian Seismological Instrumental and Parametric Database (ISIDe), Istituto Nazionale di Geofisica e Vulcanologia (INGV). https://doi.org/10.13127/ISIDE — event no. 46730692 (magnitude Md 3.1), accessed on August 1, 2026.

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Detected earthquakes — event cards
Each card shows magnitude and location with a color tag based on the earthquake's hazard level. Tap a card to open the detailed event report.
Filter by magnitude M 0.0 – 8.0
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Seismic data © INGV — ISIDe database (DOI 10.13127/ISIDE), distributed under CC-BY 4.0 license. Card descriptions are generated automatically by SinoCloud from INGV parametric data; each card links to the official event page on terremoti.ingv.it.

Seismic Dashboard
Statistics calculated in real time from the INGV data shown on the map.
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Total events
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Max magnitude
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Average depth (km)
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Average magnitude
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M ≥ 3.0
Energy released (≈ TNT)
Magnitude Distribution
Number of events by magnitude range
Depth Distribution
Number of events by depth range (km)
Timeline
Number of events per day in the selected period
Top 10 — Strongest Events
The highest-magnitude events in the period
MLocationDepthDate
Distribution by Area
Areas with the highest number of recorded events
Science

Understanding earthquakes: magnitude, energy and depth

Magnitude measures the energy released by an earthquake on a logarithmic scale: each extra point corresponds to roughly 32 times more energy. The table below shows typical effects and worldwide annual frequency for each range.

MagnitudeClassTypical effectsFrequency (worldwide)
< 2.0MicroImperceptible, detected only by instrumentsmillions / year
2.0 – 2.9Very minorRarely felt by people> 1,000,000 / year
3.0 – 3.9MinorFelt near the epicenter, damage rare~ 100,000 / year
4.0 – 4.9ModerateObjects sway, possible minor damage~ 10,000 – 15,000 / year
5.0 – 5.9StrongDamage to vulnerable buildings~ 1,500 / year
6.0 – 6.9Very strongSevere damage in populated areas~ 120 / year
≥ 7.0MajorWidespread destruction~ 15 / year

Depth matters: shallow, intermediate and deep

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Shallow (0 – 70 km)

Most Italian earthquakes. At equal magnitude they're the most damaging, because the energy reaches the surface with little attenuation.

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Intermediate (70 – 300 km)

Typical of the southern Tyrrhenian Sea, where the Ionian plate sinks (subduction of the Calabrian Arc). Often barely felt at the surface despite high magnitudes — like the M 4.5 event at 245 km depth on July 24, 2026.

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Deep (> 300 km)

Rare in Italy; linked to deep subduction, which under the Tyrrhenian Sea reaches about 500 km.

Territory

Seismicity of Southern Italy: zones, faults and history

Southern Italy is among the areas of highest seismic hazard in Europe, due to the convergence between the African and Eurasian plates and subduction beneath the Ionian Sea.

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Calabrian Arc and Strait of Messina

Subduction of the Ionian Sea, with both crustal and deep seismicity. Site of the catastrophic 1783 and 1908 earthquakes.

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Southern Apennines

Active extensional faults between Irpinia, Basilicata and Pollino, responsible for the 1980 Irpinia earthquake.

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Mount Etna and the Aeolian Islands

Volcano-tectonic seismicity linked to active magmatism, with frequent but generally shallow, localized events.

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Tyrrhenian Sea and Marsili volcano

Marsili is Europe's largest submarine volcano: monitored by INGV for potential tsunami risk.

Significant historical earthquakes

YearEventMagnitudeCasualties (est.)Notes
1693Val di Noto (eastern Sicily)~ 7.4~ 60,000Tsunami; Baroque reconstruction of the Val di Noto
1783Calabria (sequence)~ 6.9 – 7.0tens of thousandsFive strong shocks over about two months
1908Messina – Reggio Calabria~ 7.1~ 80,000Tsunami in the Strait; among the worst in Europe
1980Irpinia – Basilicata~ 6.9~ 2,900Southern Apennines
Safety

What to do during an earthquake

Essential guidelines based on Civil Protection recommendations. Knowing them in advance reduces the risk of injury.

🎒 Before
  • Prepare an emergency kit: water, flashlight, radio, medication, documents.
  • Secure tall furniture, shelves and heavy objects to the wall.
  • Identify the safe spots in your home and escape routes.
  • Agree on a meeting point with your family.
🛑 During
  • Indoors: take cover under a sturdy table (drop, cover, hold on), away from windows and furniture that could fall.
  • Don't run down stairs or use the elevator.
  • Outdoors: move to an open space, away from buildings, trees and power lines.
  • In a car: stop away from bridges and overpasses.
✅ After
  • Check for injuries and provide first aid.
  • Shut off gas, water and electricity if you suspect damage.
  • Watch out for aftershocks.
  • Use the phone only for emergencies and follow Civil Protection updates.
Information

FAQ: Earthquakes, INGV and Safety

What is Magnitude and how does it differ from Intensity?
Magnitude measures the energy released by the earthquake at the epicenter (usually calculated with the Richter or Moment Magnitude scale). Intensity (Mercalli scale) instead measures the effects and damage produced by the earthquake at a given location: an earthquake can have a single Magnitude but different Intensities depending on where you are relative to the epicenter.
What's the difference between P Waves and S Waves?
P Waves (Primary) are compression waves and are the fastest; they're the first to be recorded by seismographs. S Waves (Secondary) are shear waves and travel more slowly. It's the S Waves, and even more so the subsequent surface waves, that cause most of the structural damage during an earthquake.
What is a Tsunami?
A tsunami is a series of anomalous waves generated by a sudden displacement of a large mass of water. The most common causes are strong undersea or coastal earthquakes, but they can also be triggered by volcanic eruptions (as in the case of the Marsili submarine volcano in the Tyrrhenian Sea) or large underwater landslides.
What is INGV and why does it matter?
INGV (Istituto Nazionale di Geofisica e Vulcanologia — Italy's National Institute of Geophysics and Volcanology) is the Italian public research body responsible for seismic and volcanic monitoring across the country. It monitors Italian seismic activity 24 hours a day and is responsible for alerting Civil Protection authorities in the event of disasters, including the Tsunami Alert System (CAT-INGV).
Is Southern Italy at high seismic risk?
Yes, Calabria and eastern Sicily, together with the southern Apennine arc, are among the areas of highest seismic hazard in Italy and Europe, due to the convergence between the Eurasian and African tectonic plates.
Can earthquakes be predicted?
No. Science today cannot predict the exact location, date and magnitude of an earthquake. What is possible is estimating an area's seismic hazard on a statistical and historical basis, and reducing risk through earthquake-resistant construction and prevention. Be wary of anyone claiming precise predictions: they have no scientific basis.
What's the difference between hypocenter and epicenter?
The hypocenter (or focus) is the point at depth where the rock rupture originates; the depth given for each event is precisely that of the hypocenter. The epicenter is its vertical projection onto the Earth's surface, i.e. the point on the map closest to the earthquake's source.
Why are there very deep earthquakes in the Tyrrhenian Sea?
Beneath the southern Tyrrhenian Sea, the Ionian Sea plate sinks into the mantle (subduction of the Calabrian Arc): this generates earthquakes down to about 500 km deep. These events are often barely felt at the surface even at high magnitudes, such as the magnitude 4.5 event recorded at 245 km depth on July 24, 2026.
Where does the data come from and how often is it updated?
The data comes from INGV's FDSN web service (ISIDe catalog) and is distributed under a Creative Commons BY 4.0 license. The map updates automatically every 15 minutes; events of magnitude 3.0 or higher are also archived and described on this page.
Is the seismic data shown reliable?
Yes: it comes directly from INGV, the only official public body in Italy for seismic monitoring. It should be noted, however, that the first magnitude, depth and location values are automatic and preliminary and may be revised by seismologists in the following hours: this is why the magnitude of the same event can change slightly over time. This page shows ISIDe catalog data exactly as published by INGV, with no modifications. For official emergency communications always refer to INGV and Civil Protection channels.