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Published byBaldwin Martin Modified over 9 years ago
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Lisbon Portugal November 1, 1755 at 9:40am Earthquakes from epicenter in Atlantic Ocean 200 km WSW of Cape St Vincent Estimated 8.5-9.0, 2-3 minutes, near 100,00 lost First scientifically studied earthquake For its effect over a large area Born : modern seismology Forty min after, water receded Tsunami 10 m (33 ft) high Carried debris 0.5 km inland Two other waves followed Fissures 5m (15 feet) opened Damaged 90% buildings Fires destroyed libraries, raged for five days Case: Great Lisbon Earthquake Google Images: Lisbon 1755 Earthquake
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Earthquake shocks felt throughout Europe Felt in Finland, N. Africa, Greenland, Caribbean Tsunamis 66 ft N. Africa, Martinique, Barbados 3 ft Cornwall, England, Ireland Boundary between African (Nubian) and Eurasian plates Complex, active tectonic movement Responsible for prior earthquakes: Eight in 14 th century, five in 16 th century Three in 17 th century Two others in 18 th century 1531 : destroyed 1500 homes 1597 : three streets vanished Distance and History
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Azores-Gibraltar Fault Zone Azores-Gibraltar fault zone Azores-Gibraltar Major geological fault associated with Lisbon quakeLisbon quake Runs east from eastern end of Terceira Rift in Azores Extends through Strait of Gibraltar to Mediterranean Forms part of tectonic boundary Between African (Nubian) and Eurasian plates Diffuse fault boundary; not quite understood
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