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4 earthquakes recorded in Turkey regional monitoring zone

Real-Time Earthquakes in Turkey

Continuous seismic tracking along the North Anatolian, East Anatolian, and Aegean plate boundaries.

TURKEY EVENTS

4

TECTONIC SETTING

Anatolian Microplate, Arabian & Eurasian Collision

TELEMETRY WINDOW

Live Telemetry Feed

LARGEST EVENT

M 2.7 17 km N of Simav, 43, Türkiye

Recent Earthquakes in Turkey

LIVE

Live telemetry feed and seismic report for earthquakes in Turkey.

Active Fault Systems & Tectonic Setting

Geodynamic boundaries, subduction dynamics, and crustal deformation zones.

Subduction / Zone:ANATOLIAN-FAULT-SYSTEM
Slip Rate:20–25 mm/year (NAF), 10–15 mm/year (EAF)
Stress Regime:Continental Strike-Slip & Extensional Graben Faulting

Turkey is traversed by the strike-slip North Anatolian Fault and East Anatolian Fault, driven by the collision of the Arabian, African, and Eurasian plates. This high-stress tectonic setting produces devastating crustal earthquakes monitored in real time by AFAD.

North Anatolian Fault Zone (NAFZ)

Right-Lateral Strike-Slip

1,500 km transform fault cutting east-west across northern Turkey; passes just south of Istanbul.

East Anatolian Fault Zone (EAFZ)

Left-Lateral Strike-Slip

Major plate boundary absorbing collision between Arabian Plate and Anatolian Block.

Aegean Extensional Province

Normal Graben Faulting

North-south crustal extension generating frequent shallow tremors along the Aegean coast.

Landmark & Historical Earthquakes

Significant seismic benchmarks, cataloged magnitudes, and geological impacts.

2023M 7.8

Pazarcık, Kahramanmaraş

February 6, 2023

Catastrophic strike-slip rupture followed 9 hours later by an M7.7 event on the Çardak fault; devastated 11 provinces.

1999M 7.6

İzmit / Kocaeli, Marmara

August 17, 1999

Ruptured 120 km of the western North Anatolian Fault, catalyzing nationwide building code overhauls.

1939M 7.8

Erzincan, Eastern Anatolia

December 27, 1939

Initiated a famous westward-migrating earthquake sequence across the North Anatolian Fault.

Frequently Asked Questions

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

Why is Turkey so prone to major earthquakes?▾

Turkey sits atop the Anatolian tectonic block, which is compressed like a wedge between the northward-moving Arabian plate and the rigid Eurasian plate, forcing the crust to rupture along active strike-slip faults.

What is the expected Marmara / Istanbul earthquake hazard?▾

Seismologists track a locked seismic gap along the North Anatolian Fault under the Sea of Marmara south of Istanbul, calculating a significant probability of an M7.0+ event over the coming decades.

Where can citizens check their official AFAD meeting area?▾

Citizens in Turkey can look up their designated local post-earthquake evacuation assembly zone (Afet Toplanma Alanı) through the government e-Devlet portal or AFAD mobile app.