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1839 Ava earthquake

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468: 560: 484: 544: 524: 496: 39: 572: 512: 27: 379:  7.9 and rupture length to be 285–325 km (177–202 mi). The 1839 earthquake ruptured two segments; the Meiktila segment in the south and Sagaing segment in the north. They estimated 5.5 m (18 ft) of displacement on the Sagaing segment while slip on the Meiktila segment was around 3.8 m (12 ft). The felt area based on the Modified Mercalli intensity was larger than the 360:
believed to have ruptured during the earthquake. This segment runs from Nay Pyi Taw to Mandalay, a length of about 260 km (160 mi). Remote sensing and field observation revealed a maximum displacement of 5–7 m (16–23 ft) along the trace of the 1839 rupture just outside Mandalay. This would place the magnitude at 7.4–8.0+ and generate a ~300 km (190 mi)
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recorded catastrophic damage and liquefaction in Mandalay and the surrounding area. Many pagodas collapsed during the event. Chasms and fissures more than 10 ft (3.0 m) wide were seen in Amarapura and nearly every brick building was reduced to rubble. Some villages were swallowed up as a
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segment of the fault ruptured during this earthquake for a length of 400 km (250 mi), corresponding to a magnitude 8.1–8.3 earthquake, although little research has been conducted to provide further constrains. On the basis for its overall lack of seismic activity, the Meiktila segment is
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as they slide past each other at a rate of 18 to 49 mm/yr. The fault runs the entire length of the country for over 1,200 km and continues its trace into the Andaman Sea. The Sagaing Fault is Burma's largest and most active source of seismic threat, running through or close to major cities like
339:, a magnitude 7.1 earthquake struck close to the city of Mandalay, re-rupturing the 1839 rupture zone for about 60 km (37 mi). Meanwhile, the 260 km (160 mi) long Meiktila segment has not experienced any major earthquake since 1839 and is considered a 523: 467: 495: 284:. This large fault marks the boundary between the Indian and Burma plates. The megathrust emerges from the seafloor in Bangladesh, where it runs parallel and east of the 483: 1046: 648:
National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information
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the 180 km (110 mi) long Sagaing segment produced two major earthquakes but there are no records of its impact. Ten years later, in
1039: 1149: 109: 679: 511: 1154: 1144: 444:, where the currents became violent and overflowed its banks. It was felt for thousands of miles away from the epicenter, as far as 233: 169: 1342: 1124: 897: 1337: 1332: 1307: 1185: 1032: 440:
result of liquefaction. By a contemporary British estimate, about 300–400 people died. The shock also reversed the flow of the
1322: 1317: 1055: 593: 588: 571: 550: 1312: 1175: 220:, was a disastrous seismic event that struck present-day central Myanmar on March 23. This earthquake with an estimated 932:
Re-estimating the magnitude of 1839 Ava earthquake through geomorphic mapping and macroseismic records, central Myanmar
420: 1159: 368: 61: 1327: 1114: 38: 1139: 1119: 953: 643: 332: 92: 1129: 336: 1205: 1200: 1195: 1190: 1099: 1073: 388: 380: 225: 860:"Morphotectonics of the Central Sagaing fault West of Mandalay: Trace of the 1839 Ava Earthquake Rupture" 858:
Wang, Y.; Tapponnier, P.; Aung, T.; Tun, S. T.; Khaing, S. N.; Aung, L. T.; Sieh, K. (16 December 2014).
836: 1261: 1210: 1134: 1083: 436: 1215: 1104: 871: 763: 934:] (Masters thesis). Department of Geosciences, College of Sciences, National Taiwan University. 702: 1266: 1241: 1109: 311: 277: 1246: 1059: 722: 474: 428: 361: 307: 802: 1024: 859: 331:. Several large and damaging earthquakes have occurred on this fault in historical times. In 1256: 935: 781: 771: 714: 683: 651: 530: 281: 221: 154: 1236: 441: 300: 269: 26: 875: 767: 1286: 257: 1301: 1231: 901: 751: 726: 296: 144: 1281: 253: 1276: 1271: 1251: 618:"A Catalogue of Indian Earthquakes from the earliest time to the end of AD 1869" 502: 340: 324: 319: 315: 304: 265: 261: 534: 505:
resting on the ground after losing its supports to the quake, pictured in 1873
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Yóu dìbiǎo pòliè yǔ zhèndù jìlù chóngjiàn 1839 miǎndiàn ā wǎ dìzhèn zhī guīmó
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and macroseismic data from historic accounts to estimate its magnitude at ~M
289: 272:. Along the west coast of the Coco Islands, off the Rahkine coast, and into 673: 939: 776: 352: 328: 288:. This boundary continues to north of Burma where it ends at the eastern 898:"Myanmar setting up global positioning system for earthquake monitoring" 786: 453: 449: 395:  7.9). The maximum assigned Modified Mercalli intensity was XI ( 356: 687: 415:
in 1838, which also damaged the capital. Great damage was reported in
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Nan Myint Tower slightly tilted due to ground effects from the tremor
237: 718: 445: 432: 372: 244:. Damage was enormous in Ava, resulting in the death of hundreds. 241: 954:"Significant Earthquake Information MYANMAR (BURMA): AVA (INNWA)" 752:"Active Tectonics and Earthquake Potential of the Myanmar region" 416: 1028: 900:. People's Daily Online. People's Daily Online. Archived from 224:
as high as 8.3, was one of the largest in the country, since
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Soe Thura Tun; Ian M. Watkinson (15 November 2017).
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Myanmar is wedged between four tectonic plates; the
1224: 1168: 1092: 1066: 198: 190: 182: 161: 150: 140: 103: 87: 79: 71: 60: 801:Tapponnier, Paul; Kerry, Kerry (21 January 2010). 435:sustained serious damage as a result of shaking. 314:in the north. It accommodates motion between the 835:. Myanmar Times. Myanmar Times. Archived from 1040: 8: 756:Journal of Geophysical Research: Solid Earth 667: 665: 19: 533:in 2014. Extensive restoration was done by 517:A plaque that stands beside the Mingun Bell 45: 1047: 1033: 1025: 25: 18: 785: 775: 642:National Geophysical Data Center (1972). 622:Memoirs of the Geological Survey of India 303:that runs through Burma and connects the 93: 637: 635: 611: 609: 565:Preserved ruins from the ancient capital 387:  7.7) and similar in area to the 605: 463: 833:"Govt unveils quake preparedness plan" 1001: 999: 976: 974: 7: 745: 743: 644:"Significant Earthquake Information" 53:1839 Ava earthquake (Southeast Asia) 707:Geological Society, London, Memoirs 228:. It was assigned a maximum of XI ( 812:. Nanyang Technological University 680:California Institute of Technology 14: 234:Modified Mercalli intensity scale 570: 558: 542: 522: 510: 494: 482: 466: 44: 37: 1225:Fault zones and tectonic plates 986:SOAS Bulletin of Burma Research 473:Large cracks in the incomplete 162: 594:List of historical earthquakes 589:List of earthquakes in Myanmar 268:, that interact due to active 1: 831:Thant, Htoo (7 August 2019). 675:Earthquake Geology of Myanmar 551:Maha Aungmye Bonzan Monastery 537:in 1874 after the earthquake. 703:"The Sagaing Fault, Myanmar" 437:British officials in Myanmar 896:Xinhua (25 November 2009). 16:Earthquake in British India 1359: 1060:plate tectonics in Myanmar 864:AGU Fall Meeting Abstracts 577:Overgrown ruins of a stupa 369:National Taiwan University 928:由地表破裂與震度紀錄重建1839緬甸阿瓦地震之規模 33: 24: 927: 477:caused by the earthquake 411:was preceded by a large 299:is a mostly continental 1343:Strike-slip earthquakes 1338:1839 disasters in Asia 1333:1839 natural disasters 1308:Earthquakes in Myanmar 923:Wu, Sheng-Han (2022). 389:2002 Denali earthquake 381:1912 Maymyo earthquake 276:, is a highly oblique 1323:British rule in Burma 1318:19th century in Burma 1262:Main Himalayan Thrust 419:, so severe that the 157:(present–day Myanmar) 940:10.6342/ntu202203906 777:10.1002/2013JB010762 423:was moved to nearby 270:geological processes 214:Amarapura earthquake 212:, also known as the 1313:Earthquakes in Asia 1267:Main Frontal Thrust 1242:Three Pagodas Fault 1150:1988 Lancang–Gengma 1011:The Asiatic Journal 876:2014AGUFM.T24B..04W 768:2014JGRB..119.3767W 278:convergent boundary 210:1839 Ava earthquake 121: /  21: 20:1839 Ava earthquake 1247:West Andaman Fault 1145:1988 Myanmar–India 553:after repair works 475:Mingun Pahtodawgyi 403:Damage and effects 236:, and was felt in 1295: 1294: 1186:2009 Coco Islands 1181:2004 Indian Ocean 1176:2003 Taungdwingyi 810:RSIS Commentaries 750:Yu, Wang (2014). 688:10.7907/XWW2-9P26 672:Wang, Yu (2013). 206: 205: 1350: 1328:1839 earthquakes 1257:Sunda megathrust 1201:2012 Thabeikkyin 1125:1950 Assam–Tibet 1067:Pre-20th century 1049: 1042: 1035: 1026: 1019: 1018: 1003: 994: 993: 978: 969: 968: 966: 964: 950: 944: 943: 920: 914: 913: 911: 909: 904:on 22 March 2016 893: 887: 886: 884: 882: 855: 849: 848: 846: 844: 828: 822: 821: 819: 817: 807: 798: 792: 791: 789: 779: 747: 738: 737: 735: 733: 698: 692: 691: 669: 660: 659: 656:10.7289/V5TD9V7K 639: 630: 629: 616:Oldham, Thomas. 613: 574: 562: 546: 531:Hsinbyume Pagoda 526: 514: 498: 486: 470: 308:spreading center 282:Sunda megathrust 248:Tectonic setting 222:moment magnitude 178: 176: 164: 155:Konbaung dynasty 136: 135: 133: 132: 131: 126: 122: 119: 118: 117: 114: 98: 67:1839-03-23 24:30 48: 47: 41: 29: 22: 1358: 1357: 1353: 1352: 1351: 1349: 1348: 1347: 1298: 1297: 1296: 1291: 1237:Kyaukkyan Fault 1220: 1164: 1160:1997 Chittagong 1088: 1062: 1053: 1023: 1022: 1005: 1004: 997: 980: 979: 972: 962: 960: 952: 951: 947: 929: 922: 921: 917: 907: 905: 895: 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1197: 1194: 1192: 1189: 1187: 1184: 1182: 1179: 1177: 1174: 1173: 1171: 1167: 1161: 1158: 1156: 1155:1995 Menglian 1153: 1151: 1148: 1146: 1143: 1141: 1138: 1136: 1133: 1131: 1128: 1126: 1123: 1121: 1118: 1116: 1113: 1111: 1108: 1106: 1103: 1101: 1100:1912 Taunggyi 1098: 1097: 1095: 1091: 1085: 1082: 1080: 1077: 1075: 1072: 1071: 1069: 1065: 1061: 1057: 1050: 1045: 1043: 1038: 1036: 1031: 1030: 1027: 1016: 1012: 1008: 1002: 1000: 996: 991: 987: 983: 977: 975: 971: 959: 955: 949: 946: 941: 937: 933: 926: 919: 916: 903: 899: 892: 889: 877: 873: 869: 865: 861: 854: 851: 838: 834: 827: 824: 811: 804: 797: 794: 788: 783: 778: 773: 769: 765: 761: 757: 753: 746: 744: 740: 728: 724: 720: 716: 712: 708: 704: 697: 694: 689: 685: 681: 677: 676: 668: 666: 662: 657: 653: 649: 645: 638: 636: 632: 627: 623: 619: 612: 610: 606: 599: 595: 592: 590: 587: 586: 582: 573: 568: 561: 556: 552: 545: 540: 536: 532: 525: 520: 513: 508: 504: 497: 492: 485: 480: 476: 469: 464: 459: 457: 455: 451: 447: 443: 438: 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Retrieved 957: 948: 931: 924: 918: 906:. Retrieved 902:the original 891: 879:. Retrieved 867: 863: 853: 841:. Retrieved 837:the original 826: 814:. Retrieved 809: 796: 759: 755: 730:. Retrieved 710: 706: 696: 674: 647: 625: 621: 406: 396: 366: 350: 320:Sunda Plates 294: 266:Burma plates 251: 229: 217: 213: 209: 207: 202:300–400 dead 172: 1277:Sunda Plate 1272:Burma Plate 1252:Kabaw Fault 1206:2016 Imphal 1196:2011 Tarlay 1140:1976 Yunnan 1056:Earthquakes 787:10220/19774 762:(4): 3767. 713:: 413–441. 503:Mingun Bell 341:seismic gap 325:Nay Pyi Daw 191:Aftershocks 128: / 1302:Categories 1211:2016 Chauk 1135:1975 Bagan 1084:1858 Prome 1079:1839 Innwa 600:References 535:Mindon Min 347:Earthquake 286:Chin Hills 274:Bangladesh 199:Casualties 183:Foreshocks 130:21.9; 96.0 64: time 1216:2016 Kani 1105:1930 Bago 958:NGDC NCEI 727:134291037 678:(Ph.D.). 425:Amarapura 413:foreshock 409:mainshock 371:combined 290:Himalayas 232:) on the 165:intensity 104:Epicenter 88:Magnitude 1110:1930 Pyu 1007:"Burmah" 963:23 March 908:23 March 881:23 March 843:23 March 816:23 March 732:23 March 583:See also 353:Meiktila 329:Mandalay 323:Yangon, 258:Eurasian 171:MMI XI ( 91:7.9–8.3 1017:. 1839. 992:. 2003. 872:Bibcode 764:Bibcode 460:Gallery 454:Bangkok 450:Kolkata 397:Extreme 362:rupture 357:Sagaing 310:to the 305:Andaman 238:Rangoon 230:Extreme 173:Extreme 116:96°00′E 113:21°54′N 725:  452:, and 429:Mingun 264:, and 254:Indian 930:[ 806:(PDF) 723:S2CID 446:Dhaka 433:stupa 427:. 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Index


epicenter.
UTC
Mw
21°54′N 96°00′E / 21.9°N 96.0°E / 21.9; 96.0
Sagaing Fault
Konbaung dynasty
MMI XI (Extreme)
moment magnitude
1762
Modified Mercalli intensity scale
Rangoon
Bhamo
Indian
Eurasian
Sunda
Burma plates
geological processes
Bangladesh
convergent boundary
Sunda megathrust
Chin Hills
Himalayas
Sagaing Fault
transform fault
Andaman
spreading center
collision zone
Burma
Sunda Plates

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