effects of bihar earthquake 1934

Surv., 68, 177-239; 1935). Seeber L and Armbruster J G 1981 Great detachment earthquakes along the Himalayan arc and long-term forecasting; In: Earthquake Prediction - an International Review (eds) Simpson D W and Richards P G, Maurice Ewing Series, Am. Singh D D and Gupta H K 1980 Source dynamics of two great earthquakes of the Indian subcontinent; the Bihar- Nepal earthquake of January 15, 1934 and the Quetta earthquake of May 30, 1935; Bull. The chowk hat of Monghyr town had a most gruesome spectacle and scarcely a building or wall was left standing. A brick arch bridge between the civil lines and the old town was also fractured. Portland cement subjected to rigid tests replaced mud mortar. Thus much of the damage in northern India was not due to high ground acceleration there but rather due to surface disruption of the earths surfacial layers. ), 2019. In Purnea the cast iron piles of a bridge between the civil lines and the railway station were broken. The great 1934 Himalayan earthquake of moment magnitude (Mw) 8.1 generated a large zone of ground failure and liquefaction in north Bihar, India, in addition to the earthquakes of 1833 (Mw ~7.7) and. The reason for this was partly due to its misleading early instrumental location, partly due to the sedimentary basin amplification of seismic waves south of the then assumed epicenter which resulted in massive damage near the Ganges, and partly due to the exclusion of foreigners from Nepal (1815 to 1950) which lead to much of the damage in Nepal not being recognized. The Earthquake had hit chiefly the wealthy and middle classes in the urban areas. Minimum rupture length had been estimated as 100 Km. The 1934 NepalIndia earthquake or 1934 BiharNepal earthquake was one of the worst earthquakes in India's history. Tectonophysics, 453, 6373. The worst damage in Terai was observed in Siraha and Saptari Districts. 1934-01-15 08:43:25 UTC at 08:43 January 15, 1934 UTC Location: Epicenter at 26.885, 86.589 19.2 km from Lahn (12.2 miles) Nepal India Border . Bettinelli P, Avouac J-P, Flouzat M, Jouanne F, Bollinger L, Willis P and Chitrakar G R 2006 Plate motion of India and interseismic strain in the Nepal Himalaya from GPS and DORIS measurements; J. Geod. About 3,000 persons in Muzaffarpur had met their death in the Earthquake. Seeber, L., & Armbruster, J. Shortly after the earthquake, Mahama Gandhi was said to have visited the area to observe the destruction and to bring comfort to the injured. Marcussen, E. (2017). alluvial plain of Bihar (India) and Nepal, and the hilly regions of eastern Himalayan ranges. New observations disagree with previous interpretations of surface rupture along the himalayan frontal thrust during the great 1934 Bihar-Nepal earthquake. Himalayan tectonics: A modern synthesis. Seismic moments of major earthquakes and the average rate of slip in central Asia. The shock of the Great Earthquake of Bihar from the preceding rumbling sound lasted for about 3 to 5 minutes and in that brief period about 10,000 persons were killed and extensive damages to buildings, roads, bridges, railway tracks and cultivation fields were caused. The magnitude of the earthquake was 8.1. According to a report on the Bihar Earthquake and measures taken in consequence thereof up to 31 December, 1934, brought out by the then provincial Bihar government in 1935, public and residential building were practically razed in Munger, Darbhanga and Muzaffarpur districts. De Graff-Hunter J 1934 The Indian earthquake (1934); Nature(London) 133 236-237. (Before Earthquake) &&&&&&&& &&& &&(During Earthquake), Fig-1 (Images of the then Dharahara, a nine-storeyed tower at Sundhara, Kathmandu; Before, During and After 1934 Earthquake. The largest instrumentally recorded earthquake within a radius of 300 km happened on 15. Sir E. Pascoe's lecture on Indian earthquakes and their causes is published by the Royal Society of Arts (Journal, 82, 577-594; 1934), and papers on the North Bihar earthquake by Dr. M. S . Damage there was generally less widespread, with fewer deaths recorded. Most of the Government buildings in Laheriasarai town had collapsed. 1934 Bihar Earthquake (click photos to enlarge): The last entry in GTG's service record states "Resigned commission in A.I.R.O. The Kesariya Stupa in the town of Bihar was reduced 6 m in height to 35 m by the 1934 earthquake. Bijih logam ditem terlebih dahulu dilakukan http://goo.gl/f0vB7K This indicates that adequate structural design is the key to reduce the earthquake risk in Nepal. He specializes in the quantification and simulation of A simple loss estimation study was conducted as a preparation for a possible repeat of an earthquake like the 1934 one. The epicenter was in the vicinity of the large Bihar-Nepal earthquakes of 1833 (magnitude 7.0-7.5) and 1934 (magnitude 8.4). The great Indian Earthquake of January 15, 1934. In Nepal, Damage was mainly destructive in central Nepal, including Kathmandu valley & Eastern part of the country. and Geology at UC Davis and Due to convergence of Indian and Tibetan plates seismicity in Himalaya region has been higher always. Inst., 13, 417-432; 1935), who spent seven weeks during the following summer in the central district. In Nepal, 8519 people lost their lives whereas in India 7188 people lost their lives. Auden) from the Geological Survey of India visited Kathmandu, which had been severely shaken. Depending on the locality, the earthquake was said to last for 2-5 minutes with peak shaking around 2.5 mins after the initiation of earthquake. A low-magnitude earthquake hit parts of Bihar on Monday night, though no damage was reported. Duvall, M., Waldron, J. W. F., Godin, L., & Najman, Y. A., Auden, J. The towns of Munger and Muzaffarpur were completely destroyed. Everest. Whereas areas like Dhankuta, Sindhupalchowk, Rasuwagadhi, Chainpur, Taplejung also suffered damage. Seismicity of the earth and associated phenomena. News from the most affected region arrived only two or three days later. Nature Geoscience, 6, 7176. 1988 A.D. / 2045 B.S. Current Science, 69, 101127. 1442-1444. As per the report, distribution of damage in northern India was very uneven. Likewise, damage was observed in Gorkha, Ilam, Nuwakot, Pokhara, Palpa, Bhimphedi too. Nepal Ko Maha Bhukampa (The Great Earthquake of Nepal) (pp. Thank you for visiting nature.com. An appraisal of damage by Pandey and Molnar (1988) based on a translation of a contemporary damage published in Nepali by Major Brahma Sumsher J. The ground around these sand fissures subsided, causing more damage. Hayes et al. Bilham, R. (2019). Bhaktapur also saw massive destruction but less than these five villages. Sukhija, B. S., Rao, M. N., Reddy, D. V., Nagabhushanam, P., Kumar, D., Lakshmi, B. V., & Sharma, P. (2002). The towns to the south of the river Ganges like Patna, Bhagalpur, and Gaya escaped with lighter damages. Burrard, S. (1934). More than 80,000 houses were damaged. This sea was gradually consumed through the subduction of the oceanic floor beneath Tibet. The agricultural field was covered in knee-deep mud following the 1934 Bihar earthquake. Thru~ t (MRT) and is about 50 Km east northeast of the location of great Bihar-Nepal earthquake of january 15, 1934. Its rupture length was estimated to be 1,200 miles. The BiharNepal Earthquake of 1934. [1] Wikipedia entry on the Bihar Earthquake: http://en.wikipedia.org/wiki/1934_Bihar_earthquake. This 8.0 magnitude earthquake occurred on 15 January 1934 at around 2:13pm IST (08:43 UTC) and caused widespread damage in northern Bihar and in Nepal. 1st English edition. Lack of a central zone in which the shaking was demonstrably stronger than elsewhere suggests that the waves did not originate within the plains of India. The buildings along the riverfront in Patna or Bhagalpur suffered very badly. [8] The town of Birgunj was destroyed, along with its telephone line to Kathmandu. 6 Celebs Who Lost Their Lives Under the Knife. (1981). Additionally, Devastatingdisasters.com participates in various other affiliate programs, and we sometimes get a commission through purchases made through our links. Publ. Major Their most famous difference and debate was in 1934 when Gandhi was reported in the press to have made a statement following the devastating Bihar earthquake of 1934: "I want you to be superstitious enough to believe with me that the earthquake is a divine chastisement for the great sin we have committed against those whom we describe as Harijans". The total casualties was about 10,000 people in the area and many thousands were injured by the falling debris. 110 1010-1027. It should be noted that peak shaking occurred only after few minutes of initiation of shaking allowing sufficient time for evacuation at the mid-day; hence less casualties. But after the extensive study on the damages in Nepal conducted by Nepali Officers too and based on the evidences compiled by Shree M. J Brahma Sumsher, later it was relocated within Nepal. India Memoir. 117, S2, 773-782. 1.Bihar Earthquake, 1934 This quake is considered to be one of the worst quakes in Indian history. Soc. The problem of the permanent drainage of the area was sought to be tackled by this Division and they had the rich material of the work of the Survey of India who had run flying levels over the areas. The epicentre for this A catalog of felt intensity data for 589 earthquakes in India, 16362008. (Following is a reproduction of the account written by P.C Roy Choudhury). It shook an area half a million square miles in extent in Nepal and Tibet. In: P. J. Treloar, & M. P. Searle (Eds. Journal of Asian Earth Sciences. Nepal is situated within this seismically active Himalayan mountain belt. Soc. Copyright 2023 Devastating Disasters.com | Powered by, Bihar Earthquake India January 15, 1934. CrossRef Get the most important science stories of the day, free in your inbox. 1934 AD: This is known as Great Nepal Bihar Earthquakes is the strongest earthquake of the 20 th century and this. Most of the damage was due to slumping, fissuring and tilting of the ground.The absence of any preferred orientation of the fissures and the prevalence of the sand and water issued from the fissures suggest that the destruction of the earth surface was limited to surfacial layers only not to faulting of the basement beneath that area. Most of the buildings are masonry structures which were heavily damaged during the earthquake. London:Special Publications. S. K. BANERJI . 5. 6 85-98. The results indicated that there had been no marked increase either in the transfer of land or in borrowing money accepting among the improvident aboriginals of Monghyr and Bhagalpur districts. Pandey, M. R., & Molnar, P. (1988). Around 4.300 people died and roughly 20% of all buildings were destroyed and another 40% got damaged. The quake was felt at far-off places such as Kanpur (440 km south-east from the The continuing northward motion of India at the rate of about four centimeters per year has created wide-spread deformation, giving rise to the worlds highest mountains. (1984). The area west of Kathmandu has not ruptured in the last three hundred years and stands out as a potential site for future great Himalayan earthquakes. The activity is a result of the slow northward movement of the Indian Subcontinent, colliding with the great Asian landmass of China. Majority of seismic events in the Kumaun-Garhwal Himalayas region is located close to the MCT or north and south of it. There is evidence that even larger events have occurred in the past, and geodetic and seismic monitoring show that stress is accumulating now. In the brief period thousands of buildings were reduced to debris, the surface of the land changed, fissures appeared, wells were sanded up, buildings that were survived developed huge cracks, water gushed details from wells, thousand and thousands of square miles of land were filled by enormous jagged fissures and pitted with small volcanic craters from which sand or grey mud spread over the field. Kumar, S., Wesnousky, S., Rockwell, T. K., Briggs, R. W., Thakur, V. C., & Jayangondaperumal, R. (2006). 125 people lost their lives, 248 were seriously injured. . The towns to the south of the river Ganges like Patna, Bhagalpur, and Gaya escaped with lighter damages. 1939) that described its effects in India in detail but which contains scant information on the effects above the rupture area north of the Nepal border. There is some dispute as to the epicenter of the event, with one report placing it about 10 km south of Mt. The new specifications promulgated by the Government laying stress on the use of horizontal reinforced concrete of R.B. Plates seismicity in Himalaya region has been higher always Najman, Y in northern India was very uneven Bhagalpur., including Kathmandu valley & eastern part of the buildings are masonry structures which were heavily during! Million square miles in extent in Nepal, and the hilly regions of Himalayan... Also suffered damage active Himalayan mountain belt a bridge between the civil and. 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effects of bihar earthquake 1934