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2 earthquakes recorded in Greece regional monitoring zone

Real-Time Earthquakes in Greece

Continuous seismic tracking along the Hellenic Subduction Zone, Aegean Sea Arc, and Ionian Fault System.

GREECE EVENTS

2

TECTONIC SETTING

Hellenic Subduction Zone & Aegean Microplate Arc

TELEMETRY WINDOW

Live Telemetry Feed

LARGEST EVENT

M 2.7 211 km E of Mytilene, Greece

Recent Earthquakes in Greece

LIVE

Live telemetry feed and seismic report for earthquakes in Greece.

Active Fault Systems & Tectonic Setting

Geodynamic boundaries, subduction dynamics, and crustal deformation zones.

Subduction / Zone:HELLENIC-ARC
Slip Rate:35–40 mm/year convergence
Stress Regime:Megathrust Subduction, Continental Rifting & Strike-Slip

Greece is located in the most seismically active region of Europe, where the African Plate subducts beneath the Aegean Sea Microplate along the Hellenic Trench. This active subduction zone produces frequent moderate to severe earthquake activity monitored in real time by the Institute of Geodynamics at NOA.

Hellenic Subduction Arc

Subduction Megathrust

Sweeping convergent arc stretching from the Ionian Islands past southern Crete to Rhodes.

Gulf of Corinth Rift Faults

Normal Extensional Rift

One of the fastest-opening continental rifts on Earth (up to 15 mm/yr extension).

Cephalonia Transform Fault (CTF)

Right-Lateral Strike-Slip

High-slip transform boundary connecting the Hellenic subduction zone with Adriatic thrust systems.

Landmark & Historical Earthquakes

Significant seismic benchmarks, cataloged magnitudes, and geological impacts.

1953M 7.2

Cephalonia / Zakynthos, Ionian Sea

August 12, 1953

Devastating sequence that destroyed almost every structure across the southern Ionian islands.

1999M 6.0

Mount Parnitha / Athens

September 7, 1999

Shallow normal fault rupture 18 km north of central Athens causing heavy factory and apartment collapses.

2020M 7.0

North of Samos Island, Aegean Sea

October 30, 2020

Normal fault rupture triggering localized tsunami inundation on Samos and heavy damage in nearby İzmir, Turkey.

Frequently Asked Questions

Common questions about seismic activity, safety, and monitoring in Greece.

Why is Greece the most seismically active country in Europe?▾

Greece accounts for over half of Europe's total seismic energy release because it sits over the rapid 35 mm/yr subduction of the African plate under the Aegean microplate, combined with the rapid opening of the Corinth Rift.

What is the Gulf of Corinth rift?▾

The Gulf of Corinth is a geological rift separating the Peloponnese from mainland Greece, spreading apart at up to 15 mm per year—making it one of the world's most rapidly expanding and active continental rift basins.

How does the Greek 112 emergency alert work?▾

Greece's Ministry of Climate Crisis and Civil Protection uses Cell Broadcast 112 to send instant localized emergency alerts in Greek and English to all smartphones in regions affected by earthquakes, tsunamis, or wildfires.