The capital sits on the Anatolian plateau away from the main plate boundary, but the North Anatolian Fault passes roughly 120 km to the north, where the 1944 Bolu-Gerede rupture extended the westward cascade of twentieth-century breaks.
72-hour composite hazard forecast
Recorded in the selected 14d period
Largest earthquake in the selected 14d period
Seismotectonic hazard assessment, structural exposure & historical context
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Living within 200 km of the city centre
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Mixed construction stock with regional engineering standards
Transform / Strike-Slip
Moderate deformation or intraplate seismic zone
No significant earthquakes recorded in the selected 14d period.
Every recorded earthquake in this area — filter by time range and sort by time or severity.
Verified scientific, operational, and emergency protocols