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1349 Apennine earthquakes

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data gathered from scarping, fault length, and collapsed sections of Venafro's Roman aqueduct indicates the epicenter of the main shock was likely along the Aquae Iuliae fault. The fault suspected of causing this earthquake occurred on the Aqua Iuliae fault along the Molise-Campania border.
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Giudoboni, Emanuela (August 2012). "Ancient and Medieval Earthquakes in the Area of L'Aquila (Northwestern Abruzzo, Central Italy), A.D. 1–1500: A Critical Revision of the Historical and Archaeological Data".
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Galli, Paolo Antiono Costantino; Nasto, Jose Alfredo (2 May 2008). "Unmasking the 1349 earthquake source (southern Italy): paleoseismologicaland archaeoseismological indications from the Aquae Iuliae fault".
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Galli, Paul A. C.; Naso, José A. (15 September 2008). "Unmasking the 1349 earthquake source (southern Italy): paleoseismological and archaeoseismological indications from the Aquae Iuliae fault".
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Brick and Block Masonry: Proceedings of the 16th International Brick and Block Masonry Conference, Padova, Italy, 26-30 June 2016
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fault network, with the first and most destructive shock's epicenter originating from the north-west
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The first earthquake, with an estimated magnitude of 6.7, struck on 9 September in the north-west
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The town of L'Aquila has been described as being almost "completely destroyed." The abbey of
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southeast of the Molisano town of Venafro. The second quake struck on 10 of September near
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describes damage in Rome to the city's monuments. The side of the four-story
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collapsed towards the caelian hills, leaving a massive mound of
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Modena, Claudio; Porto, F. da; Valluzzi, M. R. (2016-11-03).
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rubble Rome later quarried for construction materials.
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Earthquake sequence in Italy's Apennine Mountain region
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On 9 September 1349, an earthquake sequence began in
382: 36: 408: 306:Bulletin of the Seismological Society of America 372:. Vol. 2. J. Murray. 1899. p. 424. 338: 302: 279: 265: 360: 296: 176:. These earthquakes originated from the 261: 259: 257: 255: 253: 409: 156:that severely affected the regions of 250: 13: 14: 453: 35: 28: 172:, with damage even reported in 126: 376: 332: 195: 1: 342:Journal of Structural Geology 268:Journal of Structural Geology 243: 231: 7: 389:. CRC Press. p. 2464. 10: 458: 354:10.1016/j.jsg.2008.09.007 290:10.1016/j.jsg.2008.09.007 125: 101: 64: 56: 48: 24: 20:1349 Apennine earthquakes 427:14th-century earthquakes 369:The Works of Lord Byron 86:41.454308°N 14.123227°E 212:and bridges. The poet 432:14th century in Italy 240:was also devastated. 437:Disasters in Abruzzo 422:Earthquakes in Italy 181:fold and thrust belt 91:41.454308; 14.123227 318:2012BuSSA.102.1600G 274:(2): 128–131, 145. 82: /  21: 356:– via JSTOR. 326:10.1785/0120110173 189:Paleoseismological 154:Apennine Mountains 19: 396:978-1-4987-9592-0 170:Italian Peninsula 146: 145: 449: 442:Medieval Abruzzo 401: 400: 380: 374: 373: 364: 358: 357: 336: 330: 329: 300: 294: 293: 283: 263: 142: 140: 128: 97: 96: 94: 93: 92: 87: 83: 80: 79: 78: 75: 52:9 September 1349 39: 38: 32: 22: 18: 457: 456: 452: 451: 450: 448: 447: 446: 407: 406: 405: 404: 397: 381: 377: 366: 365: 361: 337: 333: 301: 297: 281:10.1.1.1034.234 264: 251: 246: 234: 210:Roman aqueducts 198: 134: 132: 90: 88: 84: 81: 76: 73: 71: 69: 68: 49:Local date 44: 43: 42: 41: 40: 17: 12: 11: 5: 455: 445: 444: 439: 434: 429: 424: 419: 403: 402: 395: 375: 359: 348:(2): 128–149. 331: 295: 248: 247: 245: 242: 233: 230: 197: 194: 144: 143: 130: 123: 122: 103: 102:Areas affected 99: 98: 66: 62: 61: 58: 54: 53: 50: 46: 45: 34: 33: 27: 26: 25: 15: 9: 6: 4: 3: 2: 454: 443: 440: 438: 435: 433: 430: 428: 425: 423: 420: 418: 415: 414: 412: 398: 392: 388: 387: 379: 371: 370: 363: 355: 351: 347: 343: 335: 327: 323: 319: 315: 311: 307: 299: 291: 287: 282: 277: 273: 269: 262: 260: 258: 256: 254: 249: 241: 239: 229: 227: 223: 219: 215: 211: 207: 203: 193: 190: 186: 182: 179: 175: 171: 167: 163: 159: 155: 151: 141: 138: 131: 124: 120: 116: 112: 108: 104: 100: 95: 67: 63: 59: 55: 51: 47: 31: 23: 385: 378: 368: 362: 345: 341: 334: 309: 305: 298: 271: 267: 238:Montecassino 235: 199: 147: 136: 312:(4): 1606. 196:Earthquakes 89: / 411:Categories 244:References 222:travertine 77:14°07′24″E 74:41°27′16″N 276:CiteSeerX 232:Aftermath 218:Colosseum 129:intensity 65:Epicenter 57:Magnitude 214:Petrarch 206:L'Aquila 202:Campania 187:region. 185:Campania 178:Apennine 135:MMI XI ( 121:regions) 117:, & 115:Campania 314:Bibcode 166:Abruzzo 137:Extreme 119:Abruzzo 105:Italy ( 393:  278:  162:Latium 158:Molise 111:Molise 107:Latium 150:Italy 417:1349 391:ISBN 226:tufa 224:and 174:Rome 164:and 127:Max. 350:doi 322:doi 310:102 286:doi 152:'s 60:6.7 413:: 346:31 344:. 320:. 308:. 284:. 272:31 270:. 252:^ 160:, 113:, 109:, 399:. 352:: 328:. 324:: 316:: 292:. 288:: 139:)

Index

1349 Apennine earthquakes is located in Italy
41°27′16″N 14°07′24″E / 41.454308°N 14.123227°E / 41.454308; 14.123227
Latium
Molise
Campania
Abruzzo
MMI XI (Extreme)
Italy
Apennine Mountains
Molise
Latium
Abruzzo
Italian Peninsula
Rome
Apennine
fold and thrust belt
Campania
Paleoseismological
Campania
L'Aquila
Roman aqueducts
Petrarch
Colosseum
travertine
tufa
Montecassino



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