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1169 Sicily earthquake

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29: 220: 36: 282:, with fill of up to 700 metres (2,297 ft) and 800 metres (2,625 ft) respectively. Onshore, two ages of faulting have been recognised, an earlier phase trending NW-SE and a later phase trending SSW-NNE that clearly offsets the first group, including the Avola fault and the Rosolini-Ispica fault system. 389:, with no significant eruption. As with the 1693 earthquake the 1169 event seems to have followed after a major period of eruptive activity. Calculations have shown that a major eruption may significantly increase the stress on the normal faults to the south-east of the volcano. 500:
Barbano, Maria Serafina; De Martini, P.M.; Pantosti, D.; Smedile, A.; Del Carlo, P.; Gerardi, F.; Guarnieri, P.; Pirrotta, C. (2010). "In search of tsunami deposits along the eastern coast of Sicily (Italy): state of the art". In Guarnieri, Pierpaolo (ed.).
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at the time of the earthquake, blaming most of the deaths in Catania and the tsunami on the eruption. However, most later workers believe the tsunami was triggered by the earthquake and that the only effect on Etna was the collapse of part of the cone above
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zone, a zone of extensional faulting which runs for about 370 kilometres (230 mi), forming three main segments through Calabria, along the east coast of Sicily and immediately offshore, and finally forming the southeastern margin of the
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correlated with this earthquake have been found both onshore and offshore. The tsunami is also thought to be responsible for moving several large boulders from the middle of the sublittoral zone onto the coast between Augusta and Syracuse.
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Smedile, A.; De Martini P.M.; Pantosti D.; Bellucci L.; Del Carlo P.; Gasperini L.; Pirrotta C.; Polonia A. & Boschi E. (2011). "Possible tsunami signatures from an integrated study in the Augusta Bay offshore (Eastern Sicily—Italy)".
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Estimates of the death toll in the earthquake vary, with 15,000 being often quoted, sometimes for the overall total and sometimes just for Catania. A few sources give the higher estimate of 25,000.
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would take part in a Byzantine invasion of the island. However, these disaffected exiles were soon allowed to return and there was no invasion, nor the rebellion that it might have triggered.
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collapsed, killing the Bishop John of Ajello, 44 of the Benedictine monks, and many others who were crowded into the building for the feast of St. Agatha. Lentini, Modica,
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Catalano, S.; De Guidi G.; Monaco C.; Tortorici G. & Tortorici L. (2008). "Active faulting and seismicity along the Siculo–Calabrian Rift Zone (Southern Italy)".
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the flow of another spring, known as Tais, stopped after the earthquake. Two hours later it returned with much greater force than before and had the colour of blood.
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Hirn, A.; Nicolich R.; Gallart J.; Laigle M.; Cernobori L. & ETNASEIS Scientific Group (1997). "Roots of Etna volcano in faults of great earthquakes".
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Scicchitano, G.; Monaco C. & Tortorici L. (2007). "Large boulder deposits by tsunami waves along the Ionian coast of south-eastern Sicily (Italy)".
417: 260: 1141: 1877: 1551: 298:. The damaged area is similar to that for the 1693 earthquake, suggesting that both the location and magnitude were similar. Intensities of X ( 294:
is quite uncertain, with different seismologists giving locations offshore and onshore; there is similar uncertainty regarding the
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The tsunami affected most of the Ionian coast of Sicily and caused inundation from Messina in the north to the mouth of the
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Barbano, M.S.; De Martini P.M.; Pantosti D.; Smedile A.; Del Carlo P.; Gerardi F.; Guarnieri P. & Pirrotta C. (2011).
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Azzaro, R.; Barbano M.S. (2000). "Analysis of the seismicity of Southeastern Sicily: a proposed tectonic interpretation".
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described the effects on the Arethusa spring in Syracuse, which increased its rate of flow greatly and became salty. Near
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The magnitude of the earthquake has been estimated from intensity information and these estimates vary from 6.4 on the M
1544: 1112: 1036: 679: 1867: 1790: 680:"A unique 4000 yrs long geological record of multiple tsunami inundations in the Augusta Bay (eastern Sicily, Italy)" 637: 515: 327: 1498: 914: 1816: 1508: 1604: 1418: 1367: 1164: 475: 1862: 1537: 1483: 1341: 1244: 1178: 274:, dipping to the east. Most of these lie offshore, and some control basins that contain large thicknesses of 1463: 678:
De Martini, P.M.; Barbano M.S.; Smedile A.; Gerardi F.; Pantosti D.; Del Carlo P. & Pirrotta C. (2010).
1694: 1560: 1473: 1382: 633:"Quaternary normal faulting in southeastern Sicily (Italy): a seismic source for the 1693 large earthquake" 470: 187:). It had an estimated magnitude of between 6.4 and 7.3 and an estimated maximum perceived intensity of X ( 1811: 1518: 1438: 1377: 480: 263:, a carbonate platform in southeastern Sicily. Faults in the Calabrian segment were responsible for the 1887: 1785: 1750: 1740: 1684: 1674: 1624: 1413: 929: 646: 270:
In the southern part of the eastern coast of Sicily, investigations have identified a series of active
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Advances in Natural and Technological Hazards Research. Vol. 13. Springer. p. 36.
1009: 967:. The Mediaeval academy of America. Vol. 31. Mediaeval Academy of America. p. 115. 891: 211:. Overall, the earthquake is estimated to have caused the deaths of at least 15,000 people. 1372: 1229: 1133: 1037:"In search of Tsunami deposits along the eastern coast of Sicily (Italy): state of the art" 933: 887: 821: 782: 698: 650: 605: 278:
sediments. The two largest faults, known as the western and eastern master faults, border
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Guidoboni, E.; Ferrari G.; Mariotti D.; Comastri A.; Tarabusi G. & Valensise G.
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Scicchitano, G.; Costa B.; Di Stefano A.; Longhitano S. & Monaco C. (2008).
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In the chaos that followed the earthquake, there was concern that exiles like
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occurred on 4 February 1169 at 08:00 local time on the eve of the feast of
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saw the earthquake as God's punishment on the Sicilians for the exile of
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The History of the Tyrants of Sicily by "Hugo Falcandus," 1154–69
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Some accounts of this earthquake refer to a major eruption from
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Bianca, M.; Monaco C.; Tortorici L. & Cernobori L. (1999).
362: 307: 247:. This subduction zone is responsible for the formation of the 204: 180: 126: 184: 1163: 913:
Feuillet, N.; Cocco M.; Musumeci C. & Nostro C. (2006).
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were severely damaged, and the earthquake also triggered a
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Falcando, Ugo (1998). Loud G.A.; Wiedmann T.E.J. (eds.).
1111:. Translated by Loud G.A. pp. 4–6. Archived from 1011:
Tsunamis in the Mediterranean Sea, 2000 B.C.-2000 A.D.
746:. SocietĂ  Geologica Italiana: 159–162. Archived from 1106:"Some Letters of Peter of Blois concerning Sicily" 575: 987:. Manchester University Press. pp. 216–217. 1854: 254:. Most of the damaging earthquakes occur on the 801: 35: 1545: 1149: 1007: 1001: 1080:. Edinburgh University Press. p. 205. 976: 974: 1552: 1538: 1156: 1142: 1100: 724: 541: 539: 537: 535: 493: 945: 671: 662: 409:and Syracuse were also severely damaged. 397:Catania was almost completely destroyed. 1559: 1165:Historical earthquakes (1000 AD–1500 AD) 1073: 1067: 980: 971: 906: 571: 569: 567: 565: 218: 1028: 589: 532: 349:(Energy magnitude scale) to 7.3 on the 1855: 765: 1878:12th century in the Kingdom of Sicily 1533: 1137: 1044:Recent Progress on Earthquake Geology 960: 954: 846: 840: 624: 562: 510:. New York: Nova Science Publishers. 504:Recent progress on earthquake geology 1094: 867: 876:Earth and Planetary Science Letters 375: 302:) have been estimated for Catania, 231:Sicily lies on part of the complex 214: 13: 964:Latin Monasticism in Norman Sicily 457:of Catania, replacing his brother 14: 1904: 922:Geophysical Journal International 638:Geophysical Journal International 290:The location of the earthquake's 947:10.1111/j.1365-246X.2005.02824.x 664:10.1046/j.1365-246X.1999.00942.x 34: 27: 133: 476:List of historical earthquakes 449:and the appointment of Bishop 1: 1077:The Muslims of Medieval Italy 900:10.1016/S0012-821X(97)00023-X 486: 285: 834:10.1016/j.margeo.2006.12.005 795:10.1016/j.margeo.2011.01.002 711:10.1016/j.margeo.2010.07.005 471:List of earthquakes in Italy 426: 7: 740:Rend. Online SGI Note Brevi 618:10.1016/j.tecto.2007.05.008 481:List of historical tsunamis 464: 412:In a contemporary account, 10: 1909: 1832:January 2017 Central Italy 1827:October 2016 Central Italy 1046:. Nova. pp. 109–146. 930:Royal Astronomical Society 647:Royal Astronomical Society 604:(1–4). Elsevier: 177–192. 453:, through bribery, to the 356: 265:1783 Calabrian earthquakes 1822:August 2016 Central Italy 1799: 1708: 1567: 1406: 1350: 1299: 1253: 1202: 1171: 1042:. In Guarnieri P. (ed.). 392: 161: 153: 132: 121: 84: 70: 62: 51:4 February 1169 47: 23: 1868:12th-century earthquakes 193:Mercalli intensity scale 1650:1694 Irpinia–Basilicata 1008:Solov'ev, S.L. (2000). 892:1997E&PSL.148..171H 781:(1–4). Elsevier: 1–13. 1791:1997 Umbria and Marche 351:surface wave magnitude 296:1693 Sicily earthquake 272:normal dip-slip faults 228: 173:1169 Sicily earthquake 19:1169 Sicily earthquake 1499:1585 Aleutian Islands 1074:Metcalfe, A. (2009). 850:Tsunamis in the World 256:Siculo-Calabrian rift 225:Siculo-Calabrian rift 222: 1863:Earthquakes in Italy 1561:Earthquakes in Italy 961:White, L.T. (1938). 586:Viewed 25 June 2012. 365:River in the south. 328:Santi Pietro e Paolo 165:15,000–25,000 deaths 1817:2012 Northern Italy 1514:1596 Keichō–Fushimi 1419:1509 Constantinople 1118:on 10 December 2013 938:2006GeoJI.164..697F 826:2007MGeol.238...75S 787:2011MGeol.281....1S 753:on 25 February 2012 703:2010MGeol.276...42D 655:1999GeoJI.139..370B 610:2008Tectp.453..177C 578:Annali di Geofisica 437:Robert of Loritello 233:convergent boundary 223:Main faults of the 102: /  20: 1605:1456 Central Italy 1484:1580 Dover Straits 1368:1456 Central Italy 1342:1382 Dover Straits 1245:1185 East Midlands 1179:1033 Jordan Valley 847:Tinti, S. (1993). 229: 18: 1888:Medieval tsunamis 1850: 1849: 1695:1883 Casamicciola 1527: 1526: 1474:1575 San Salvador 1383:1475 Tenochtitlan 1087:978-0-7486-2008-1 1053:978-1-60876-147-0 1021:978-0-7923-6548-8 994:978-0-7190-5435-8 860:978-0-7923-2316-7 447:Stephen du Perche 399:Catania Cathedral 169: 168: 1900: 1554: 1547: 1540: 1531: 1530: 1519:1590 Neulengbach 1509:1586 Lima–Callao 1439:1522 Vila Franca 1158: 1151: 1144: 1135: 1134: 1128: 1127: 1125: 1123: 1117: 1110: 1098: 1092: 1091: 1071: 1065: 1064: 1062: 1060: 1041: 1032: 1026: 1025: 1005: 999: 998: 978: 969: 968: 958: 952: 951: 949: 919: 910: 904: 903: 871: 865: 864: 844: 838: 837: 805: 799: 798: 769: 763: 762: 760: 758: 752: 737: 728: 722: 721: 719: 717: 684: 675: 669: 668: 666: 628: 622: 621: 593: 587: 585: 573: 560: 559: 557: 555: 543: 530: 529: 509: 497: 459:William of Blois 433:Tancred of Lecce 376:Eruption of Etna 369:Tsunami deposits 215:Tectonic setting 195:. The cities of 149: 147: 135: 117: 116: 114: 113: 112: 107: 106:37.217°N 14.95°E 103: 100: 99: 98: 95: 58: 56: 38: 37: 31: 21: 17: 1908: 1907: 1903: 1902: 1901: 1899: 1898: 1897: 1853: 1852: 1851: 1846: 1795: 1786:1990 Carlentini 1751:1930 Senigallia 1741:1920 Garfagnana 1704: 1685:1857 Basilicata 1563: 1558: 1528: 1523: 1464:1570 ConcepciĂłn 1414:1505 Lo Mustang 1402: 1346: 1295: 1249: 1198: 1167: 1162: 1132: 1131: 1121: 1119: 1115: 1108: 1099: 1095: 1088: 1072: 1068: 1058: 1056: 1054: 1039: 1033: 1029: 1022: 1006: 1002: 995: 979: 972: 959: 955: 917: 911: 907: 872: 868: 861: 845: 841: 806: 802: 770: 766: 756: 754: 750: 735: 729: 725: 715: 713: 682: 676: 672: 629: 625: 594: 590: 574: 563: 553: 551: 544: 533: 518: 507: 498: 494: 489: 467: 429: 418:Casale Saraceno 395: 378: 359: 348: 340:Reggio Calabria 320:Piazza Armerina 288: 261:Hyblean Plateau 217: 141: 139: 110: 108: 104: 101: 96: 93: 91: 89: 88: 79: 63:Local time 54: 52: 48:Local date 43: 42: 41: 40: 39: 12: 11: 5: 1906: 1896: 1895: 1890: 1885: 1880: 1875: 1873:1169 in Europe 1870: 1865: 1848: 1847: 1845: 1844: 1839: 1834: 1829: 1824: 1819: 1814: 1809: 1803: 1801: 1797: 1796: 1794: 1793: 1788: 1783: 1778: 1773: 1768: 1763: 1758: 1756:1936 Cansiglio 1753: 1748: 1743: 1738: 1733: 1728: 1723: 1718: 1712: 1710: 1706: 1705: 1703: 1702: 1697: 1692: 1687: 1682: 1677: 1675:1783 Calabrian 1672: 1667: 1662: 1657: 1652: 1647: 1642: 1637: 1632: 1627: 1625:1638 Calabrian 1622: 1617: 1615:1626 Girifalco 1612: 1607: 1602: 1597: 1592: 1587: 1582: 1577: 1571: 1569: 1565: 1564: 1557: 1556: 1549: 1542: 1534: 1525: 1524: 1522: 1521: 1516: 1511: 1506: 1501: 1496: 1491: 1486: 1481: 1476: 1471: 1466: 1461: 1456: 1451: 1446: 1441: 1436: 1431: 1426: 1421: 1416: 1410: 1408: 1404: 1403: 1401: 1400: 1395: 1390: 1385: 1380: 1375: 1370: 1365: 1363:1428 Catalonia 1360: 1354: 1352: 1348: 1347: 1345: 1344: 1339: 1334: 1329: 1324: 1319: 1314: 1309: 1303: 1301: 1297: 1296: 1294: 1293: 1288: 1283: 1278: 1273: 1268: 1263: 1257: 1255: 1251: 1250: 1248: 1247: 1242: 1237: 1232: 1227: 1222: 1217: 1212: 1206: 1204: 1200: 1199: 1197: 1196: 1191: 1189:1068 Near East 1186: 1184:1038 Dingxiang 1181: 1175: 1173: 1169: 1168: 1161: 1160: 1153: 1146: 1138: 1130: 1129: 1102:Peter of Blois 1093: 1086: 1066: 1052: 1027: 1020: 1000: 993: 970: 953: 905: 866: 859: 839: 810:Marine Geology 800: 775:Marine Geology 764: 723: 687:Marine Geology 670: 623: 598:Tectonophysics 588: 561: 531: 516: 491: 490: 488: 485: 484: 483: 478: 473: 466: 463: 451:John of Ajello 443:Peter of Blois 428: 425: 414:Hugo Falcandus 394: 391: 377: 374: 358: 355: 346: 287: 284: 245:Eurasian Plate 216: 213: 167: 166: 163: 159: 158: 155: 151: 150: 137: 130: 129: 123: 122:Areas affected 119: 118: 86: 82: 81: 77: 72: 68: 67: 64: 60: 59: 49: 45: 44: 33: 32: 26: 25: 24: 9: 6: 4: 3: 2: 1905: 1894: 1891: 1889: 1886: 1884: 1881: 1879: 1876: 1874: 1871: 1869: 1866: 1864: 1861: 1860: 1858: 1843: 1840: 1838: 1835: 1833: 1830: 1828: 1825: 1823: 1820: 1818: 1815: 1813: 1812:2009 L'Aquila 1810: 1808: 1805: 1804: 1802: 1798: 1792: 1789: 1787: 1784: 1782: 1779: 1777: 1774: 1772: 1771:1971 Tuscania 1769: 1767: 1764: 1762: 1759: 1757: 1754: 1752: 1749: 1747: 1744: 1742: 1739: 1737: 1734: 1732: 1731:1915 Avezzano 1729: 1727: 1724: 1722: 1721:1907 Calabria 1719: 1717: 1716:1905 Calabria 1714: 1713: 1711: 1707: 1701: 1698: 1696: 1693: 1691: 1688: 1686: 1683: 1681: 1678: 1676: 1673: 1671: 1668: 1666: 1663: 1661: 1658: 1656: 1655:1703 Apennine 1653: 1651: 1648: 1646: 1643: 1641: 1638: 1636: 1635:1659 Calabria 1633: 1631: 1630:1639 Amatrice 1628: 1626: 1623: 1621: 1618: 1616: 1613: 1611: 1608: 1606: 1603: 1601: 1598: 1596: 1593: 1591: 1588: 1586: 1583: 1581: 1578: 1576: 1573: 1572: 1570: 1566: 1562: 1555: 1550: 1548: 1543: 1541: 1536: 1535: 1532: 1520: 1517: 1515: 1512: 1510: 1507: 1505: 1502: 1500: 1497: 1495: 1492: 1490: 1489:1582 Ancuancu 1487: 1485: 1482: 1480: 1479:1575 Valdivia 1477: 1475: 1472: 1470: 1467: 1465: 1462: 1460: 1457: 1455: 1452: 1450: 1447: 1445: 1442: 1440: 1437: 1435: 1432: 1430: 1427: 1425: 1422: 1420: 1417: 1415: 1412: 1411: 1409: 1405: 1399: 1396: 1394: 1391: 1389: 1386: 1384: 1381: 1379: 1378:1461 L'Aquila 1376: 1374: 1371: 1369: 1366: 1364: 1361: 1359: 1356: 1355: 1353: 1349: 1343: 1340: 1338: 1335: 1333: 1330: 1328: 1327:1349 Apennine 1325: 1323: 1320: 1318: 1315: 1313: 1312:1303 Hongdong 1310: 1308: 1305: 1304: 1302: 1298: 1292: 1291:1293 Kamakura 1289: 1287: 1284: 1282: 1279: 1277: 1274: 1272: 1269: 1267: 1264: 1262: 1259: 1258: 1256: 1252: 1246: 1243: 1241: 1238: 1236: 1233: 1231: 1228: 1226: 1223: 1221: 1218: 1216: 1213: 1211: 1208: 1207: 1205: 1201: 1195: 1192: 1190: 1187: 1185: 1182: 1180: 1177: 1176: 1174: 1170: 1166: 1159: 1154: 1152: 1147: 1145: 1140: 1139: 1136: 1114: 1107: 1103: 1097: 1089: 1083: 1079: 1078: 1070: 1055: 1049: 1045: 1038: 1031: 1023: 1017: 1013: 1012: 1004: 996: 990: 986: 985: 977: 975: 966: 965: 957: 948: 943: 939: 935: 931: 928:(3). London: 927: 923: 916: 909: 901: 897: 893: 889: 885: 881: 877: 870: 862: 856: 852: 851: 843: 835: 831: 827: 823: 819: 815: 811: 804: 796: 792: 788: 784: 780: 776: 768: 749: 745: 741: 734: 727: 712: 708: 704: 700: 696: 692: 688: 681: 674: 665: 660: 656: 652: 648: 645:(2). London: 644: 640: 639: 634: 627: 619: 615: 611: 607: 603: 599: 592: 584:(1): 171–188. 583: 579: 572: 570: 568: 566: 549: 542: 540: 538: 536: 527: 523: 519: 517:9781608761470 513: 506: 505: 496: 492: 482: 479: 477: 474: 472: 469: 468: 462: 461:in the post. 460: 456: 452: 448: 444: 440: 438: 434: 424: 421: 419: 415: 410: 408: 404: 400: 390: 388: 383: 373: 370: 366: 364: 354: 352: 343: 341: 337: 333: 329: 325: 321: 317: 313: 309: 305: 301: 297: 293: 283: 281: 277: 273: 268: 266: 262: 257: 253: 250: 249:stratovolcano 246: 242: 238: 237:African Plate 234: 226: 221: 212: 210: 206: 202: 198: 194: 190: 186: 183:(in southern 182: 178: 174: 164: 160: 156: 152: 148: 145: 138: 131: 128: 124: 120: 115: 111:37.217; 14.95 87: 83: 80: 73: 69: 65: 61: 50: 46: 30: 22: 16: 1800:21st century 1781:1980 Irpinia 1761:1962 Irpinia 1746:1930 Irpinia 1726:1908 Messina 1709:20th century 1700:1887 Liguria 1670:1743 Salento 1665:1732 Irpinia 1660:1706 Abruzzo 1620:1627 Gargano 1610:1570 Ferrara 1590:1222 Brescia 1584: 1469:1570 Ferrara 1459:1556 Shaanxi 1454:1555 Kashmir 1444:1536 Xichang 1434:1522 AlmerĂ­a 1407:16th-century 1358:1420 Caldera 1351:15th-century 1300:14th-century 1281:1275 British 1276:1269 Cilicia 1266:1222 Brescia 1254:13th-century 1234: 1203:12th-century 1172:11th-century 1120:. 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INGV-SGA 487:References 322:and VIII ( 286:Earthquake 276:Quaternary 267:sequence. 252:Mount Etna 241:subducting 235:where the 177:St. Agatha 162:Casualties 97:14°57′00″E 94:37°13′01″N 55:1169-02-04 1398:1498 MeiĹŤ 1373:Haowhenua 1230:1157 Hama 820:: 75–91. 697:: 42–57. 526:429026456 427:Aftermath 292:epicentre 191:) on the 136:intensity 85:Epicenter 71:Magnitude 884:Elsevier 818:Elsevier 695:Elsevier 465:See also 387:Taormina 316:Syracuse 125:Eastern 1883:Catania 1122:25 June 1059:25 June 934:Bibcode 888:Bibcode 882:(1–2). 822:Bibcode 816:(1–4). 783:Bibcode 757:24 June 716:24 June 699:Bibcode 693:(1–4). 651:Bibcode 606:Bibcode 554:24 June 407:Sortino 357:Tsunami 353:scale. 332:Messina 312:Violent 304:Lentini 300:Extreme 201:Lentini 197:Catania 189:Extreme 154:Tsunami 144:Extreme 142:MMI X ( 53: ( 1084:  1050:  1018:  991:  857:  524:  514:  393:Damage 363:Simeto 336:Strong 324:Severe 310:, IX ( 308:Modica 205:Modica 181:Sicily 127:Sicily 1116:(PDF) 1109:(PDF) 1040:(PDF) 918:(PDF) 751:(PDF) 736:(PDF) 683:(PDF) 508:(PDF) 338:) in 326:) at 314:) at 185:Italy 66:08:00 1124:2012 1082:ISBN 1061:2012 1048:ISBN 1016:ISBN 989:ISBN 855:ISBN 759:2012 718:2012 556:2012 522:OCLC 512:ISBN 435:and 382:Etna 330:and 318:and 306:and 227:zone 203:and 171:The 134:Max. 74:7.3 942:doi 926:164 896:doi 880:148 830:doi 814:238 791:doi 779:281 707:doi 691:276 659:doi 643:139 614:doi 602:453 455:see 239:is 179:of 157:Yes 1859:: 1104:. 973:^ 940:. 924:. 920:. 894:. 878:. 828:. 812:. 789:. 777:. 742:. 738:. 705:. 689:. 685:. 657:. 641:. 635:. 612:. 600:. 582:43 580:. 564:^ 534:^ 520:. 405:, 342:. 199:, 1553:e 1546:t 1539:v 1157:e 1150:t 1143:v 1126:. 1090:. 1063:. 1024:. 997:. 950:. 944:: 936:: 902:. 898:: 890:: 863:. 836:. 832:: 824:: 797:. 793:: 785:: 761:. 744:1 720:. 709:: 701:: 667:. 661:: 653:: 620:. 616:: 608:: 558:. 528:. 347:e 146:) 78:s 76:M 57:)

Index

1169 Sicily earthquake is located in Sicily
Ms
37°13′01″N 14°57′00″E / 37.217°N 14.95°E / 37.217; 14.95
Sicily
MMI X (Extreme)
St. Agatha
Sicily
Italy
Mercalli intensity scale
Catania
Lentini
Modica
paleotsunami

Siculo-Calabrian rift
convergent boundary
African Plate
subducting
Eurasian Plate
stratovolcano
Mount Etna
Siculo-Calabrian rift
Hyblean Plateau
1783 Calabrian earthquakes
normal dip-slip faults
Quaternary
half-grabens
epicentre
1693 Sicily earthquake
Lentini

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