Dense population basin in Central Asia intersected by active compressional thrusts. The shallow 1966 Tashkent earthquake (M5.2) devastated the city center due to poor building resistance and amplified alluvial shaking.
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 seismically active radius (~300 km)
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Mixed construction stock with regional engineering standards
Convergent Margin
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.