Lisbon faces a moderate but genuinely serious earthquake risk, lower in day-to-day frequency than cities on major plate boundaries but capable of rare, catastrophic events. Portugal's capital lies near the boundary between the African and Eurasian plates, which runs through the Atlantic offshore to the southwest. Large earthquakes here are infrequent, so the region can go long periods with little activity, but the faults offshore in the Gulf of Cadiz and along the Azores-Gibraltar zone can produce very powerful quakes and ocean-crossing tsunamis. Much of central Lisbon is also built on soft riverside sediments that amplify shaking.
Earthquakes in Lisbon: The 1755 Great Quake & Tsunami



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The city's defining catastrophe was the Great Lisbon earthquake of 1 November 1755, an offshore event estimated at magnitude 8.5 to 9.0. It struck on All Saints' Day, and the shaking, the fires that followed, and a massive tsunami that swept up the Tagus killed tens of thousands of people and destroyed most of the city, an event so vast it influenced European philosophy and helped give birth to modern seismology. Lisbon was famously rebuilt with early anti-seismic "gaiola" timber-frame construction. While a repeat of 1755 is rare on human timescales, the historical record and modern hazard studies mean the risk is real, and newer buildings follow seismic design standards.
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