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Rome Seismic Zone • 200 km Monitoring Radius

Real-Time Earthquakes in Rome, Italy

Live seismic telemetry, active fault rupture tracking, and ground motion hazard monitoring for the Rome metropolitan area.

TECTONIC SETTING:Central Apennines Extensional Fault System & Colli Albani Volcanic Zone
METRO POPULATION:2.8 Million (4.3M Metro)
OBSERVATORY:INGV →

ROME EVENTS (200 KM)

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NEAREST ACTIVE FAULT

Central Apennines Normal Fault System (Fucino / L’Aquila / Amatrice) (85 km)

TELEMETRY WINDOW

Live Telemetry Feed

SEISMIC INTENSITY

LOW SEISMICITY (24H)

Landmark Historical Earthquakes in Rome

Significant seismic benchmarks, cataloged damage, and engineering lessons shaping modern safety standards.

1915M 6.7

Avezzano / Fucino Basin

1915-01-13•80 km from Rome•MMI VII in Rome

Killed over 30,000 people in Avezzano; severely shook Rome, cracking the Colosseum, the Pantheon portico, and multiple historic basilicas.

2016M 6.6

Norcia / Central Apennines

2016-10-30•120 km from Rome•MMI V–VI in Rome

Strongest earthquake in Italy in 36 years; felt violently in Rome, leading to temporary closures of the Colosseum and St. Paul Outside the Walls for safety inspections.

Seismic Geology & Soil Amplification in Rome

Plate boundaries, tectonic kinematics, and local geotechnical ground response characteristics.

PLATE BOUNDARY:African Plate & Eurasian Plate Collision Belt (Adria Microplate)
SLIP RATE:2–4 mm/year Apennine crustal extension
STRESS REGIME:Northeast-Southwest Crustal Extension (Normal Faulting)

Rome is situated on the Tiber River plain 80 km southwest of the highly seismic Central Apennine fault belt (Abruzzo, Umbria, Rieti). While major fault ruptures rarely occur directly inside the city, Apennine M6.5+ earthquakes propagate severe long-period ground motions into Rome’s alluvial floodplains.

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Local Soil Profile & Ground Motion Resonance

The Tiber River alluvium (loose gravel, sand, and silt) creates pronounced 2-to-3-fold seismic amplification, whereas the classic Seven Hills of Rome (volcanic tuff of the Roman Magmatic Province) provide stable bedrock.

Major Active Fault Systems Near Rome

Seismogenic fault lines, maximum credible magnitudes (MCE), and proximity to the metropolitan center.

85 KM FROM CITYM 6.8–7.0

Central Apennines Normal Fault System (Fucino / L’Aquila / Amatrice)

Active Normal Faults1–3 mm/year

A continuous chain of seismogenic normal faults capable of producing repeated severe M6+ shocks.

Seismic Safety, Observatory & Building Codes

Official seismological monitoring, building construction standards, early warnings, and emergency response.

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OFFICIAL SEISMIC OBSERVATORY

Istituto Nazionale di Geofisica e Vulcanologia (INGV) (INGV)

INGV Real-Time Seismic Telemetry & IT-alert System
BUILDING CODE STANDARD:Norme Tecniche per le Costruzioni (NTC 2018 / Eurocode 8)
Visit Official Observatory (INGV) →
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EMERGENCY HOTLINE
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Drop, Cover, and Hold On. Avoid standing near ancient Roman brick monuments and unreinforced masonry parapets during shaking.

Frequently Asked Questions About Earthquakes in Rome

Authoritative answers to common questions regarding seismic risks, building safety, and preparedness in Rome.

Is Rome at direct risk of earthquake destruction?▾

Rome is classified in Italian Seismic Zone 3 (low-to-moderate hazard). The primary hazard is not surface rupture under the city, but resonant amplification of distant M 6.5+ Apennine quakes in the soft Tiber Valley alluvium affecting historic monuments.