1703 Apennine earthquakes

[1] A total of about 10,000 people are estimated to have died as a result of these earthquakes,[2] although because of the overlap in areas affected by the three events, casualty numbers remain highly uncertain.The central part of the Apennines has been characterised by extensional tectonics since the Pliocene epoch (i.e. about the last 5 million years), with most of the active faults being normal in type and NW-SE trending.[6] Modern estimates give a maximum Mercalli intensity of XI (Extreme).Marine ridge, a large slope failure near Posta and liquefaction along the Aterno River.[9] Details taken from Catalogue of Strong Earthquakes in Italy (461 BC – 1997) and Mediterranean Area (760 B.C.
earthquakesmagnitudeApenninesepicentersNorciaMonterealeL'Aquilafaultsextensional tectonicsPlioceneactive faultsback-arc basinTyrrhenian SeaAfrican platecollidingEurasian plateSpoletoMercalli intensityGround ruptureCittarealeAccumoliAmatriceliquefactionAternocoulomb stress transfer2009 L'Aquila earthquake1706 Abruzzo earthquake1461 L'Aquila earthquakeList of earthquakes in ItalyList of historical earthquakesBibcodeEarthquakes in Italy62 Pompeii1117 Verona1169 Sicily1222 Brescia1343 Naples1348 Friuli1456 Central Italy1570 Ferrara1626 Girifalco1627 Gargano1638 Calabrian1639 Amatrice1659 Calabria1688 Sannio1693 Sicily1694 Irpinia–Basilicata1706 Abruzzo1732 Irpinia1743 Salento1783 Calabrian1805 Molise1857 Basilicata1873 Alpago1883 Casamicciola1887 Liguria1905 Calabria1907 Calabria1908 Messina1915 Avezzano1916 Rimini1920 Garfagnana1930 Irpinia1930 Senigallia1936 Cansiglio1962 Irpinia1968 Belice1971 Tuscania1976 Friuli1980 Irpinia1990 Carlentini1997 Umbria and Marche2002 Molise2009 L'Aquila2012 Northern ItalyAugust 2016 Central ItalyOctober 2016 Central ItalyJanuary 2017 Central Italy2017 Ischia2018 Molise