Magnitude 4.9 Earthquake Depth 10 km Strikes Central Türkiye on 15th November 2024

Diagram of Anatolian faults, tectonic plates, and earthquake focus
A geological cross-section illustrates the Anatolian fault systems, tectonic plates, and earthquake focus near Maraş and Gaziantep.

Concise Takeaway

A magnitude 4.9 earthquake struck central Türkiye on 15th November 2024, occurring at a shallow depth of 10 km. The tremor was felt across several towns and districts, though early reports indicated no major damage or casualties.

Earthquake Overview

The quake occurred in one of Türkiye’s active tectonic regions, where the Anatolian Plate interacts with both the Arabian Plate and the Eurasian Plate. Because the earthquake was shallow, residents experienced noticeable shaking even though the magnitude was moderate.

People across the region reported:

  • Light to moderate shaking
  • Brief vibrations lasting a few seconds
  • Swaying of household items
  • No immediate structural damage

Emergency services monitored the situation closely following the event.

Related Guide
How Earthquake Magnitudes Are Calculated

Impact on Communities

Local authorities confirmed:

  • No significant damage
  • No injuries reported
  • No disruption to essential services
  • No tsunami threat

Some residents briefly evacuated buildings as a precaution, following standard earthquake‑safety behaviour common in Türkiye.

Response from Authorities

Türkiye’s disaster‑management agencies:

  • Logged the event and issued intensity assessments
  • Checked infrastructure in affected districts
  • Monitored communication networks
  • Assessed vulnerable buildings
  • Reassured the public that the event posed no ongoing threat

Officials also reminded residents of earthquake‑preparedness guidelines, especially in regions with a history of seismic activity.

Scientific Context

Central Türkiye lies near several major fault systems, including:

  • The North Anatolian Fault (NAF)
  • The East Anatolian Fault (EAF)
  • Secondary strike‑slip and thrust faults across the Anatolian interior

Earthquakes of magnitude 4.5–5.0 are common due to:

  • Crustal deformation
  • Strike‑slip fault movement
  • Stress accumulation along active fault zones

A shallow depth of 10 km often makes shaking more noticeable but typically limits widespread damage.

Related Guide
What Is a Subduction Zone? Understanding One of Earth’s Most Powerful Geological Features


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