426:, jolting many people from their sleep, including the Europeans settling in the area. Almost all the Europeans residing in an establishment ran out of their residences for fear that they would crumble. Tremors were still felt even 20 minutes later. The mainshock struck at just before midnight, described as more violent than earlier events, and as if being "seized by several hands and shaken violently backward and forwards". All the local residents in the city dashed out of their homes. The earthquake was so intense that standing was nearly impossible.
42:
466:
1385:
415:, the mainshock was still strong enough to be felt even from Nepal. It shook houses and woke many residents from their sleep. Many people rushed out of their houses even as more strong shock rocked the city. Huge chunks of cornice and plasters fell from walls during the quake. Several native dwellings were reportedly destroyed, and at least three people died from house collapses. A massive fissure also tore through the ground some two miles from the city.
49:
58:
532:, felt four distinct shocks with the last two causing homes to creak, and lamps to swing about. The shaking caused animals including birds, elephants, and snakes to behave unusually. Residents of the city ran out of their homes, fearing it would collapse on them, and began to pray. The same effects were observed in other parts of India, where many people and animals became frightened.
481:, rockfalls and avalanches in the mountainous region destroyed over 4,600 homes and temples. The two foreshocks occurring a few hours to minutes before the larger quake may have greatly reduced the death toll. Residents were driven out of their homes and dwellings due to panic caused by the two shocks. Had the two foreshocks not happened, many residents would have been killed.
376:
for 40 seconds, it was significant but not strong enough to cause any fatalities. Plants and trees were seen swaying from the crowns to their roots. The next foreshock occurred at 10:45 pm, which had similar effects like the one five hours earlier. These foreshocks would have a large influence on the
380:
Fifteen minutes later, another earthquake rocked the city. It was described in the beginning as gentle rocking, followed by some rumbling sounds. Shaking then escalated to a more violent characteristic; trees were seen bending, and houses ripped from their foundations. Horses and cattle escaped from
500:
collapsed completely and was never rebuilt. The other tower suffered minor damage and was repaired shortly after. The new tower stood over the city until 1934 when the magnitude 8.0 earthquake would knock it down again. The other was partially damaged and quickly restored, only to be destroyed once
381:
their stalls, frightened by the earthquake. The earthquake was so strong that people found it difficult to walk, like those seen in footages of the 2015 earthquake. It lasted an approximate three minutes. Many terrified residents got to the ground and began to pray during the earthquake.
523:
In India, the earthquake caused some serious damage to towns and destroyed a small number of buildings. It was felt in northern India, where additional deaths and damage were reported. Damage there was generally less widespread, with fewer deaths recorded. The capital of
520:(then Bhatgaon), east of the Kathmandu Valley, at least 200 individuals were killed, making it the worst affected area outside the valley. One quarter (25%) to 70% of the town suffered major destruction, including at least 2,000 homes and six to eight temples.
579:
313:
prepared after the quake, researchers believe the earthquake was caused by an 80–120 km × 40 km section of the megathrust rupturing. The same fault patch that ruptured in 1833 would re-rupture again during the
438:
sequence immediately followed after the mainshock, but it gradually decayed after persisting for several weeks. Strong aftershocks were felt on
October 4, October 18, and November 26 of 1833.
305:
The décollement rupture area of the 1833 event is likely the same as in 2015, but closer to
Kathmandu. Both earthquakes occurred along the MHT but did not rupture to the surface, thus, were
302:
was a repeat of the 1833 event. All of which failed to release all the strain that had been building over the past centuries thus was an incomplete rupture of the Main
Himalayan Thrust.
894:
792:
Stacey S. Martin; Susan E. Hough; Charleen Hung (2015). "Ground
Motions from the 2015 Mw 7.8 Gorkha, Nepal, Earthquake Constrained by a Detailed Assessment of Macroseismic Data".
1257:
449: 6.8 and 7.4, too small to cause any surface ruptures. Its epicenter location remains uncertain although some geologists suggest it was in the same location as the
298:. This thrust fault is the source of most of Nepal's earthquakes. The earthquake of 1833 has been suggested by geologists to be a repeat of the 1344 earthquake, and the
1345:
364:. Another epicenter area located roughly 130 km west of the 1934 earthquake epicenter, at the eastern edge of a seismic gap has been favoured by many authors.
266:. Despite the extent of the damage, the number of fatalities resulting from the earthquake was surprisingly low, at approximately 500. This was because the
741:
513:
became unfit for occupancy. In all, a total of 18,000 buildings were totally wiped out, with over 4,000 having collapsed in the
Kathmandu Valley region.
764:
1058:
1421:
1290:
1232:
445: 6.5 or greater. Thirty-three years later, another large earthquake struck on May 23, 1866. Estimates of this magnitude range between M
258:. The earthquake caused major destruction in numerous towns and villages in Nepal, northern India, and Tibet. The earthquake was also felt in
404:
on
September 12 the same year, the earthquake was perceived as wave-like with long rolls and peaks, in a northeast and southwest direction.
850:"Location and Magnitude of the 1833 Nepal Earthquake and its Relation to the Rupture zones of Contiguous Great Himalayan earthquakes"
336:
116:
1611:
41:
17:
925:
198:
1753:
1748:
1051:
1015:
1641:
1414:
1283:
1560:
1144:
441:
In 1835, a major aftershock struck the same region. The estimated magnitude of this aftershock is on the order of M
1768:
1621:
1530:
1520:
1510:
1474:
1320:
1134:
1124:
502:
319:
1656:
1044:
733:
551:
492:, 400 buildings crumpled to the ground, burying many occupants residing in them. One of the two towers of the
477:
The earthquake was felt over an area roughly 1 million km in Nepal, northern India, and southern Tibet. Large
1738:
1733:
1728:
1651:
1459:
1407:
1389:
1276:
950:
1430:
1299:
546:
541:
1666:
1631:
1340:
1184:
299:
1681:
1585:
1570:
1540:
1444:
1310:
1154:
1084:
246:
99:
1743:
1702:
1636:
1352:
1189:
450:
1580:
1252:
1217:
389:
1707:
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1606:
1590:
1545:
1479:
1454:
1449:
1169:
1164:
1159:
1109:
1099:
1089:
992:
306:
165:
687:"Himalayan earthquakes: a review of historical seismicity and early 21st century slip potential"
1763:
1758:
1646:
1626:
1555:
1515:
1505:
1500:
1469:
1357:
1335:
1179:
1174:
1119:
1094:
1686:
1676:
1671:
1575:
1565:
1550:
1535:
1525:
1484:
1372:
1367:
1330:
1325:
1242:
1199:
1194:
1149:
1139:
1129:
1114:
454:
283:
151:
598:
1362:
801:
698:
594:
329:
location of the earthquake due to the poor constrains in data. Researcher and seismologist
8:
1247:
1237:
506:
242:
88:
805:
702:
973:
861:
649:
633:
612:
330:
977:
951:"Revealing What is Dear: the post-earthquake iconisation of the Dharahara, Kathmandu"
401:
322:, as the 1833 event did little to release the elastic tension along the décollement.
616:
965:
817:
809:
706:
686:
602:
489:
255:
1209:
470:
161:
577:
1227:
895:"Historiography and Commentary on the Nepal–India Earthquake of 26 August 1833"
310:
295:
969:
607:
287:
1722:
580:"Slip deficit in central Nepal: omen for a repeat of the 1344 AD earthquake?"
525:
510:
497:
423:
351:
338:
274:
earlier that day, causing many residents to take refuge outside their homes.
131:
118:
1222:
791:
291:
465:
1036:
865:
822:
653:
637:
1399:
1268:
1070:
849:
813:
478:
435:
263:
259:
711:
517:
493:
484:
At least 30% or more of all homes in northern Nepal and the southern
419:
385:
373:
326:
271:
267:
1067:
734:"Significant Earthquake Information NEPAL: KATHMANDU; INDIA: BIHAR"
254:) of 7.6–7.9 and struck with an epicenter somewhere in or near the
529:
408:
892:
578:
L. Bollinger; P. Tapponnier; S. N. Sapkota; Y. Klinger (2016).
509:, was completely destroyed, and the garden houses belonging to
485:
412:
184:
180:
176:
923:
924:
Asiatic
Society of Bengal (1833). Prinsep, James (ed.).
843:
841:
839:
837:
835:
833:
765:"Study: Nepal Could Be Due for Another Major Earthquake"
1016:"Nepal's Historic Architecture Destroyed By Earthquake"
680:
678:
676:
674:
672:
670:
927:
The
Journal of the Asiatic Society of Bengal, Volume 2
830:
245:. This earthquake had an estimated moment magnitude (
667:
48:
632:
372:At about 6:00 pm, the first foreshock was felt in
453:, or it might be a deeper event like that of the
1720:
888:
886:
884:
882:
787:
785:
691:Geological Society, London, Special Publications
290:structure that defines the boundary between the
638:"Three little known early earthquakes in India"
377:number of casualties caused by the mainshock.
1415:
1284:
1052:
879:
782:
418:The foreshocks were also distinctly felt in
893:Sujit Dasgupta; Basab Mukhopadhyay (2015).
860:(2). Current Science Association: 101–128.
648:(4). Current Science Association: 506–508.
628:
626:
619:– via Earth Observatory of Singapore.
1422:
1408:
1291:
1277:
1059:
1045:
1066:
821:
710:
606:
388:, the earthquake was assigned a modified
333:determined the epicenter coordinates was
247:
100:
1429:
1298:
762:
623:
464:
270:was preceded by two smaller but intense
14:
1721:
847:
684:
488:region were totally destroyed. In the
1403:
1272:
1040:
1013:
990:
948:
899:Indian Journal of History of Science
573:
571:
569:
567:
24:
25:
1780:
917:
564:
57:
1384:
1383:
991:Karki, Shristi (22 April 2021).
56:
47:
40:
1007:
984:
942:
763:Metcalfe, John (14 June 2016).
744:from the original on 2022-03-22
325:Very little is known about the
241:occurred on August 26 at 22:58
191:
794:Seismological Research Letters
756:
726:
552:List of historical earthquakes
429:
400:). In an article published by
13:
1:
993:"Had a great fall, and lived"
557:
367:
27:Earthquake in Nepal and India
1258:North Himalayan Normal Fault
547:List of earthquakes in India
542:List of earthquakes in Nepal
7:
535:
239:1833 Nepal–India earthquake
31:1833 Bihar–Nepal earthquake
10:
1785:
1754:Buried rupture earthquakes
1749:Natural disasters in Bihar
277:
1703:Earthquake zones of India
1695:
1599:
1493:
1437:
1381:
1306:
1208:
1077:
970:10.1017/S0021911819000172
608:10.1186/s40623-016-0389-1
460:
451:May 2015 Nepal earthquake
227:
219:
211:
190:
172:
157:
147:
110:
94:
83:
75:
35:
1253:South Tibetan Detachment
1218:Geology of the Himalayas
1078:Notable Himalayan quakes
958:Journal of Asian Studies
587:Earth, Planets and Space
455:Bihar earthquake in 1988
390:Mercalli intensity scale
307:blind thrust earthquakes
1708:Geology of the Himalaya
1642:October 2015 Hindu Kush
599:2016EP&S...68...12B
1769:1833 disasters in Asia
949:Hutt, Michael (2019).
848:Bilham, Roger (1995).
685:Bilham, Roger (2019).
474:
300:2015 Gorkha earthquake
1243:Main Himalayan Thrust
503:1934 Bihar earthquake
468:
320:1934 Bihar earthquake
284:Main Himalayan Thrust
152:Main Himalayan Thrust
18:1833 Nepal earthquake
1739:Earthquakes in Tibet
1734:Earthquakes in India
1729:Earthquakes in Nepal
1622:2009 Andaman Islands
1521:1941 Andaman Islands
1475:1881 Nicobar Islands
1465:1833 Kathmandu–Bihar
1431:Earthquakes in India
1300:Earthquakes in Nepal
1105:1833 Kathmandu–Bihar
1014:Stott, Rory (2015).
1248:Main Central Thrust
1238:Main Frontal Thrust
806:2015SeiRL..86.1524M
703:2019GSLSP.483..423B
469:The newly restored
348: /
128: /
32:
1561:1988 Myanmar–India
1460:1819 Rann of Kutch
1145:1988 Myanmar-India
930:. pp. 564–567
814:10.1785/0220150138
634:Nicholas Ambraseys
475:
331:Nicholas Ambraseys
30:
1716:
1715:
1612:2004 Indian Ocean
1397:
1396:
1266:
1265:
507:Matabarsing Thapa
501:again during the
402:The India Gazette
309:. Inferring from
235:
234:
16:(Redirected from
1776:
1744:1833 earthquakes
1667:2017 Uttarakhand
1632:April 2015 Nepal
1551:1980 Pithoragarh
1531:1950 Assam–Tibet
1511:1934 Nepal–India
1424:
1417:
1410:
1401:
1400:
1387:
1386:
1321:1934 Nepal–India
1316:1833 Bihar–Nepal
1293:
1286:
1279:
1270:
1269:
1185:April 2015 Nepal
1135:1950 Assam–Tibet
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1038:
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825:
800:(6): 1524–1532.
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490:Kathmandu Valley
392:rating of VIII (
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256:Kathmandu Valley
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243:local time (NPT)
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1682:2023 Badakhshan
1595:
1586:1997 Chittagong
1571:1991 Uttarkashi
1541:1967 Koynanagar
1489:
1445:1505 Lo Mustang
1433:
1428:
1398:
1393:
1377:
1311:1505 Lo Mustang
1302:
1297:
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1210:Plate tectonics
1204:
1155:1991 Uttarkashi
1085:1505 Lo Mustang
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854:Current Science
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668:
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642:Current Science
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516:In the town of
471:Dharahara Tower
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84:Local time
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1696:Related topics
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995:. Nepali Times
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505:. The home of
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1662:2017 Tripura
1652:2016 Sagaing
1617:2005 Kashmir
1607:2001 Gujarat
1600:21st century
1591:1999 Chamoli
1546:1975 Kinnaur
1494:20th century
1480:1885 Kashmir
1464:
1455:1803 Garhwal
1450:1555 Kashmir
1388:
1315:
1233:Oldham Fault
1223:Indian Plate
1170:2008 Damxung
1165:2005 Kashmir
1160:1999 Chamoli
1110:1885 Kashmir
1104:
1100:1803 Garhwal
1090:1555 Kashmir
1023:. Retrieved
1019:
1009:
997:. Retrieved
986:
961:
957:
944:
932:. Retrieved
926:
919:
907:. Retrieved
905:(3): 491–513
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869:. Retrieved
857:
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823:10356/104422
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292:Indian Plate
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238:
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201:
1657:2016 Magway
1647:2016 Imphal
1627:2011 Sikkim
1556:1984 Cachar
1516:1935 Quetta
1506:1930 Dhubri
1501:1905 Kangra
1470:1869 Cachar
1358:2016 Imphal
1346:aftershocks
1336:2011 Sikkim
1180:2011 Sikkim
1175:2009 Bhutan
1120:1905 Kangra
1095:1714 Bhutan
1071:earthquakes
748:12 December
496:, built by
430:Aftershocks
355: /
288:décollement
220:Aftershocks
135: /
1723:Categories
1687:2023 Nepal
1677:2022 Nepal
1672:2021 Assam
1576:1993 Latur
1566:1988 Nepal
1536:1956 Anjar
1526:1947 Assam
1485:1897 Assam
1438:Historical
1341:April 2015
1331:1988 Nepal
1326:1980 Nepal
1200:2023 Nepal
1195:2021 Assam
1150:1988 Nepal
1140:1980 Nepal
1130:1947 Assam
1125:1934 Bihar
1115:1897 Assam
558:References
479:landslides
436:aftershock
368:Earthquake
357:27.7; 85.7
272:foreshocks
264:Bangladesh
260:Chittagong
228:Casualties
212:Foreshocks
137:27.7; 85.7
1363:2016 Kani
1068:Himalayan
1020:ArchDaily
978:165687047
769:Bloomberg
518:Bhaktapur
494:Dharahara
420:Gorakhpur
386:Kathmandu
374:Kathmandu
327:epicenter
268:mainshock
231:~500 dead
194:intensity
111:Epicenter
95:Magnitude
64:Kathmandu
1390:Category
1353:May 2015
1025:23 April
999:23 April
934:24 April
909:22 April
871:23 April
866:24097233
742:Archived
718:23 April
654:24107899
636:(2004).
617:32078899
536:See also
473:in 1920.
396:) to X (
98:7.6–7.9
802:Bibcode
699:Bibcode
659:25 July
595:Bibcode
530:Lucknow
409:Chhapra
398:Extreme
343:85°42′E
340:27°42′N
278:Geology
202:Extreme
200:MMI X (
123:85°42′E
120:27°42′N
976:
864:
774:12 Dec
652:
615:
593:: 12.
461:Impact
394:Severe
183:&
162:Thrust
87:22:58
974:S2CID
954:(PDF)
862:JSTOR
650:JSTOR
613:S2CID
583:(PDF)
486:Tibet
413:Bihar
286:is a
185:Tibet
181:India
177:Nepal
166:Blind
148:Fault
1027:2021
1001:2021
936:2021
911:2021
873:2021
776:2020
750:2020
738:NGDC
720:2021
661:2021
294:and
282:The
237:The
223:Yes
192:Max.
158:Type
966:doi
818:hdl
810:doi
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89:NPT
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