Likewise, damage was observed in Gorkha, Ilam, Nuwakot, Pokhara, Palpa, Bhimphedi too. With a magnitude of about 8.1 to 8.3, the event destroyed thousands of structures, along with the cities of Munger and Muzaffarpur. Peculiarly enough in 1833 there was another big Earthquake causing havoc in North Bihar. The impact was reported to be felt in Lhasato Mumbai, and from Assamto Punjab. Molnar, P., & Deng, Q. Active strike-slip faults and an outer frontal thrust in the Himalayan foreland basin. Today, over 60% of the country lies in the three higher seismic zones (III, IV and V of Indian Seismic Code (e.g. Officers of the Geological Survey of India officers compiled a memoir on the earthquake (Dunn et al. Liquefaction studies using trench excavations at locations known to have suffered liquefaction in 1934 (Sukhija et al., 2002) . 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. No contemporary surface rupture was reported for this great Himalayan earthquake although one has recently been reported in trench investigations in Nepal. 82 2945-2969. Disasters 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. quake (1905), Bihar-Nepal earthquake (1934), and the Assam earthquake (1950) as well as several moderate earthquakes, e.g. Yeats R S, Nakata T, Faraj A, Fort M, Mirza M A, Pandey M R and Stein R S 1992 The Himalayan frontal fault system; Ann. News from the most affected region arrived only two or three days later. Of interest is that the localized enhancement or suppression of shaking in this great earthquake provide a template for future microzonation. 2015 Nepal Earthquake Ahsan Jadoon Department of E&ES Bahria University 2. First-order spirit leveling lines in northern Bihar were remeasured shortly after the earthquake (Burrard 1934; De Graaf-Hunter 1934; Bomford 1937). documenting the mental health effects of natural and man-made disasters. In the meantime, to ensure continued support, we are displaying the site without styles Nepal Ko Maha Bhukampa (The Great Earthquake of Nepal) (pp. The size of the area affected by earthquake-induced landslides depends on the magnitude of the earthquake, its focal depth, the topography and geologic conditions near the causative fault, and the amplitude, frequency composition, and duration of ground shaking. The agricultural field was covered in knee-deep mud following the 1934 Bihar earthquake. Nature (London), 582583. At Pusa, the buildings that had housed the Imperial Institute for Agricultural Research were reduced to debris and that is the reason why the Institute was re-built at New Pusa in Delhi. [9], The number of deaths was 10,70012,000[4][2] with 7,253 recorded in Bihar. Floods were there in the rivers carrying dirty waters. 1. 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. The 1934 NepalIndia earthquake or 1934 BiharNepal earthquake was one of the worst earthquakes in India's history. Anyone you share the following link with will be able to read this content: Sorry, a shareable link is not currently available for this article. Journal of Geophysical Research Solid Earth, 119(9), 71237163. It was the worst that ever occurred in that country. News from the country was available only next morning, showing that Patna, Monghyr and Jamalpur had suffered severely. Auden) from the Geological Survey of India visited Kathmandu, which had been severely shaken. The clock in the tower of the Secretariat stopped at 2.16 p.m. [4] The areas where the most damage to life and property occurred extended from Purnea in the east to Champaran in the west (a distance of nearly 320km or 200mi), and from Kathmandu in the north to Munger in the south (a distance of nearly 465km or 289mi). Journal of Geophysical Research, 89(B7), 62036227. Magnitude calibration of north Indian earthquakes. Geodetic Branch Survey of India (p. 97). The 2023 quake may end his rule. To the effects of shaking were added those of flood; the rivers rose high after the earthquake, bringing down sand, mud, trees, and all kinds of debris. Revolutions happen, The two atomic bombings from Hiroshima and Nagasaki in August, America is no stranger to the devastating impact a political, Timeline: 1 May 1960: An American U-2 spy plane being, During World War I prices in Germany had doubled, but, The fiasco of the Afghan presidential election of 2009 is, On February 20th, President Vladimir Putin released a warning to the West over Ukraine, by, Do you know how to protect yourself in case of an earthquake? Bihar earthquake 1934 6,000 . Theres never any convenient time for any. Seismological Research Letters, XX, 19. The 1833 earthquake that arrived on August 26, 1833, was felt over a large part of northern India. Soc. In D. W. Simpson & P. G. Richards (Eds. Pandey, M. R., & Molnar, P. (1988). Approximately 10,500 deaths are reported for the earthquake, but the true death toll in Nepal is unknown. Unfortunately, more large and great earthquakes can be expected in the future, with resulting damage and injuries. Almost half of the bridges in the valley would be impassible, and 10 percent of all paved roads would have moderate damage, such as deep cracks or subsidence. Damage there was generally less widespread, with fewer deaths recorded. 6 Celebs Who Lost Their Lives Under the Knife. Tect. 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. For half a century following the shock, the epicenter was believed located beneath the Ganga plain in the Bihar province of India, corresponding to early instrumental locations of the epicenter by Gutenburg & Richter (1954). The ground around these sand fissures subsided, causing more damage. Surv. Kumar, S., Wesnousky, S. G., Rockwell, T. K., Ragona, D., Thakur, V. C., & Seitz, G. G. (2001). Bashyal, R. P. (1998). Science, 294, 23282331. Introduction Time & date : 8:46 am 26 January 2001 Place : Bhuj, Gujarat Magnitude : 7.9 Intensity : X Epicenter : 23.419N 70.232E Focal length : 23 kms Season : Winter Damages : Over 18,600 persons are dead and over 167,000 injured. Minimum rupture length had been estimated as 100 Km. The Historic Nepal - Bihar earthquake measuring M 8.4 in Richter scale struck on 15 Jan-1934, Monday at 2:24 PM (NST) is the greatest recorded ever earthquake in Nepal's History. Geol. Journal of Geophysical Research, 82, 29452969. In Bhagalpur district many buildings collapsed. : , . Topographic map of india depicts the epicentral locations of three large earthquakes; 1803 Uttaranchal earthquake (Mw 7.5); 1934 Bihar-Nepal earthquake (Mw 8.1) and 2001 Bhuj earthquake (Mw 7.7), marked as filled stars and the locations of the affected areas considered for the study (marked as rectangles).Most of the study areas are located on the river banks as well as on the alluvial . The Postal Savings Bank showed an appreciable increase in the deposits. Based on these evidences, it was concluded that the rupture zone; hypocenter and thereby the epicenter laid beneath the lesser Himalayas and not beneath the plains of northern India. However buildings built on Bedrock survived well than those built on unconsolidated sedimentary deposit available at most part of the valley. bands at different levels in the structure interconnected with R.C. https://doi.org/10.1038/136485b0. Internet Explorer). Location and magnitude of the 1833 Nepal earthquake and its relation to the rupture zones of contiguous great Himalayan earthquakes. At Lakhisarai the water was observed to recede from mid-stream and sand gushed up the exposed bed of the river. The High Court and the Government House were damaged severely. Impact Summary; 85 1-14. B. Rana (1935) indicates that severe shaking occurred in eastern Nepal. Bihar Earthquake, 1934. The devastating quake of 8.3-magnitude on Richter scale that fateful day . 3.3 BIHAR - NEPAL EARTHQUAKE OF 1934 This 8.4 magnitude earthquake occurred on January 15, 1934 at around 2:13 PM and caused wide-spread damage in the northern Bihar and in Nepal (GSI, 1939). Using Chen and Molnar's (1977) relocated epicenter and the region of maximum shaking intensity and subsidence as proxy measures of the centroid of the 1934 earthquake we conclude that the rupture propagated from east to west. 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. 1442-1444. Current Science, 69, 101127. 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 epicenter of the earthquake was in Nepal six miles south of Mt. These effects are discussed in detail by Hough and Bilham (2008). Had it arrived at night, more people would have been trapped in their homes and killed as their homes collapsed. excessive rain during the earthquakes cause damage to the bridges. Anyone you share the following link with will be able to read this content: Sorry, a shareable link is not currently available for this article. R, Brahmaamera Jagabahdra, and Kesar Lall. document.getElementById( "ak_js_1" ).setAttribute( "value", ( new Date() ).getTime() ); At this moment, there are still a few COVID-19 variants, Have you ever considered that there were even more dangerous, Are Covid Vaccinations really THAT Safe? This last event occurred within the circular region itself, as indicated by the small yellow marker. The post earthquake reconstruction of roads, buildings, bridges, etc. Nepal Science, 307, 13021305. Seismicity of the earth and associated phenomena. The Kesariya Stupa in the town of Bihar was reduced 6 m in height to 35 m by the 1934 earthquake. M8.7 Assam earthquake, 1905 M8.6 Kangra earthquake, 1934 M8.4 Bihar-Nepal earthquake and the 1950 M8.6 Assam-Tibet earthquake. Portland cement subjected to rigid tests replaced mud mortar. Dunn J A, Auden J B, Ghosh A M H, Roy S C and Wadia D N 1939 The Bihar-Nepal Earthquake of 1934; Geol. Its rupture length was estimated to be 1,200 miles. (1981). Primary surface ruptures of the great himalayan earthquakes in 1934 and 1255. Saquib Salim is a well known historian under whose supervision various museums (Red Fort, National Library, IFFI, Jallianwala Bagh etc.) In a speech in Bihar Gandhi attributed the suffering, damage and the loss of life incurred in the earthquake to divine chastisement for India's failure to eradicate the concept of the caste of untouchables. [1] Wikipedia entry on the Bihar Earthquake: http://en.wikipedia.org/wiki/1934_Bihar_earthquake. New observations disagree with previous interpretations of surface rupture along the himalayan frontal thrust during the great 1934 Bihar-Nepal earthquake. Ratna Pustak Bhandar, Kathmandu, Nepal (136 p). Sapkota, S.; Tapponnier, P.; Bollinger, L.; Klinger, Y.; Gaudemer, Y.; Tiwari, D. R.; Siwakoti, I.; Rizza, M.Surface Rupture of the Mw 8.1, 1934, Bihar Nepal Earthquake AGU abstract 2011. Tilting and slumping of the houses were entirely absent. In: Earthquakes of the Indian Subcontinent. 4, pp. [9][10], Mahatma Gandhi visited the Bihar state. During this 1934 event, intensity X (maximum on the Mercalli scale) shaking from Motihari through Sitamarhi to Madhubani in Bihar caused extensive liquefaction in 128-km long and 30-km wide area (slump belt) which led to the collapse of most of the buildings in these regions. Mitigation Measures for Earthquakes in India Following the major quake, twenty-eight numbers of after-shocks were recorded; where few of them were greater shocks too. Hayes et al. Image Courtesy : Nepal Ko Mahabhukampa by Shree M. J Brahma Sumsher. Bulletin of the Seismological Society of America, 70, 757773. The reaction of the earthquake on rivers was remarkable. The earthquake shocks of magnitude 5 to 6 have been recorded in the Garhwal region in 1803, 1809, 1816, 1966, 34 L08304, doi:10.1029/2006GL029192. Ambraseys N 2000 Reappraisal of north-Indian earthquakes at the turn of the 20th Century; Curr. This mountainous region is one of the most seismically active continental areas on earth. The number of deaths was In G. J. Schenk (Ed. Cur Sci, 83, 10191025. The earthquake took place on January 15 around two o'clock in the afternoon and cause widespread damage. It is officially estimated that the flood-affected area of Bihar has increased from 2.5 million hectares in 1954 to 7.3 million hectares in 2016. A magnitude M W 7.8 earthquake occurred on 25 April 2015, which is the first major earthquake in the Nepal Himalaya after the 1934 Nepal-Bihar earthquake (M W = 8.1) [7]. In: Survey of India Geodetic Report 1936, (eds). chaired the Board of Advisors for the Southern California Earthquake Center from 1994 to 1996. ; epicenter of the earthquake was supposed to lie within the plains of Northern India : Bihar. In the light of the increased population today, compared with 1934, the death toll would likely be 22,000 and the number of injured 25,000. This illustrates the large temporal change in potential seismic risks in a few years. [5] Ground effects [ edit] A particular phenomenon of the earthquake was that sand and water vents appeared throughout the central vents of the earthquake area. Wesnousky, S. G., Kumahara, Y., Nakata, T., Chamlagain, D., & Neupane, P. (2018). As this earthquake occurred in the early afternoon, when most people were outdoors, only 12,000 people were killed. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. Gutenberg, B., & Richter, C. F. (1954). Along the Terai belt, destruction was observed from the eastern border of Nepal The northern edge of the rupture probably follows the line of microseismicity identified as the transition between the shallow-locked and downdip-creeping Indian plate at 15-19 km depth (Bettinelli et al 2006; Bollinger et al 2007), i.e. Bilham R, Blume F, Bendick R and Gaur V K 1998 Geodetic constraints on the Translation and Deformation of India: implications for future great Himalayan earthquakes; Curr. Kathmandu valley was severely damaged in that earthquake. https://doi.org/10.1029/2004JB003309. It shook an area half a million square miles in extent in Nepal and Tibet. Bilham, R., Gaur, V. K. and Molnar, P., Science, 2001, 293, 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. In Purnea the cast iron piles of a bridge between the civil lines and the railway station were broken. Large cracks appeared in the ground and several roads were damaged in Kathmandu; however, the temple of Pashupatinath, the guardian deity of Nepal, escaped any damage. Everest. 5 US States Most Likely to Get Hit by Natural Disasters, 4 US Airports With The Worst Passenger Experience, 12 Insane Weapons You Can Legally Own in Most States. 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 . The great Indian Earthquake of January 15, 1934. Shortly after the Bihar Earthquake of 1934, the social workers under a mistaken idea started constructing a bandh across an innumerable waterways blocking the roads and railways, culverts and drainage channels. Paleoseismological evidence of surface faulting along the northeastern himalayan front, India: Timing, size, and spatial extent of great earthquakes. Ambraseys N and Douglas J 2004 Magnitude calibration of north Indian earthquakes; Geophys. IS 1893 Part 1 [1]) and only about 3 % of . Hill districts of the epicentral zone of the 1934 earthquake tend to lose population, while Nepalese population dramatically increases in the foothills near the Indian border. the Institute of Geophysics and Planetary Physics, UC Santa Cruz. Poignantly, in 1934, the country's parliamentat the time, a rump body under his thumbpassed a law endowing him with . The High Court and the Government House were damaged severely. ISSN 0028-0836 (print). Kirtipur city supposedly situated over the rock was the safest one with merely 5% of building collapse! Also, the strong emphasis on the destruction in India left the impression that epicenter of 1934 Bihar-Nepal earthquake laid not within the Himalaya but south of the range, in the plains of India. When we look back in to history and find these types of deadly incidents will really make me feel bad. 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. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. Read John's blog. India 31, 104 pp.79. The first was its basic . The clock in the tower of the Secretariat stopped at 2.16 p.m. It resulted in a huge death toll and caused extensive destruction to buildings and infrastructure both in the central-eastern Nepal and the adjacent parts of India. 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. Liquefaction record of the great 1934 earthquake predecessors from the north Bihar alluvial plains of India. Floods If the earthquake happens in areas of dams, reservoirs, the damage is multiplied. Journal of Geophysical Research: Solid Earth, 124, 91829207. No precise geodetic measurements were in place across the 1934 rupture area due to Nepal's political isolation in 1850 when the Trigonometrical Survey of India was in progress. 483, pp. To obtain The impact was reported to be felt in Lhasa to Mumbai, and from Assam to Punjab. generally referred to as the Chamoli earthquake. First published on Sat 25 Apr 2015 16.53 EDT. Extensive damage was caused to life and property. Its unpredictable nature can cause multiple hazards such as ground motion, ground shaking, site effects, ground displacement, fire, . Explaining the 1934 Bihar-Nepal Earthquake: The Role of Science, Astrology, and Rumours. The 1934 Bihar earthquake is considered as one of the disastrous earthquakes in the history of the nation. http://goo.gl/TLJKhQ http://bit.ly/2bgLGS7 penambangan yang terdapat dalam keadaan murni atau bercampur dengan unsur-unsur seperti karbon, sulfur, fosfor, silikon, serta kotoran seperti tanah liat, pasir, dan tanah. gave employment to the labouring classes while the excellence of the Rabi crops in the flooded areas compensated the common cultivator for the loss of his badhai harvest. Mem. 110 1010-1027. The Historic Nepal - Bihar earthquake measuring M 8.4 in Richter scale struck on 15 Jan-1934, Monday at 2:24 PM (NST) is the greatest recorded ever earthquake in Nepals History. L. Fermor. Lave, J., Yule, D., Sapkota, S. N., Basant, K., Madden, C., Attal, M., & Pandey, R. (2005). It is certain that the loss of life would have been far more severe had not the main shock been preceded by two large foreshocks five hours before the main shock so that people went outdoors in alarm. Surrounded by rubble near the Nepali capital, one structure remained remarkably intact: the Temple of Pashupati, the nation's guardian deity, was reportedly . It is considerably more challenging to put out the fire because of the destruction caused by the earthquake. London:Special Publications. Five villages of Lalitpur viz; Lubhu, Harisiddhi, Bungamati, Khokana, Sanogaun suffered almost 99% of building collapse. (1939) and by Major General Brahma (Before Earthquake) &&&&&&&& &&& &&(During Earthquake), Fig-1 (Images of the then Dharahara, a nine-storeyed tower at Sundhara, Kathmandu; Before, During and After 1934 Earthquake. Large himalayan frontal thrust paleoearthquake at Khayarmara in Eastern Nepal. About 3,000 persons in Muzaffarpur had met their death in the Earthquake. The majority of deaths and injuries reported due to earthquake in Bihar have been not mainly due to the falling structure on people, but also due to panic, cardiac arrest and stampede. This is a preview of subscription content, access via your institution. Sun 26 Apr 2015 04.56 EDT. were researched. 8.0 magnitude earthquake. Am. Am. 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. In addition, possible death and injury figures were estimated by looking at statistics from previous comparable earthquakes in other parts of the world. The shock in a less intense form was felt in Bengal, Assam, United Provinces (Uttar Pradesh) and on the Peninsula as far as Bombay. Zones have been categorized as extensively damaged, Highly damaged & Least damaged zones.) Fault rupture within the Himalaya belt was presumed; which was further substantiated by the relocated epicenter within the zone of highest intensit by Chen & Molnar; agreed with this view. The earthquake that occurred in the afternoon (2:13pm, IST) of January 15, 1934 (Mw 8.2), is one of the strongest among the twentieth century Himalayan events. Bijih logam ditem terlebih dahulu dilakukan http://goo.gl/f0vB7K More than 80,000 houses were damaged. The wells were choked with sand, while water levels in tanks became shallower due to sand deposited in the tank beds. Geophys. Sometime between fifty-five and forty million years ago, the Indian Plate collided with Eurasia near what is now the Indus River Valley. The 7.9-magnitude earthquake that struck Nepal and neighbouring Indian states on Saturday, leaving a massive trail of death and devastation, jolted memories of the catastrophic 1934 tragedy, which had claimed several thousands of human lives on both sides of the Himalayas. Causes behind Misinterpretation in location of Epicenter. the worst was the 1934 earthquake in which more than 10,000 people lost their lives, followed . Overcoming the odds How Babur Arafat brought Pride to India. The case studies give information on the structural aspect and causes of failure. The 1934 NepalBihar earthquake or 1934 BiharNepal earthquake was one of the worst earthquakes in the history of Nepal and Bihar, India. ), Historical disaster experiences, transcultural researchHeidelberg studies on Asia and Europe in a global context (p. 241266). Darbhanga and Laheriasarai had similar damages and the buildings belonging to the Darbhanga Raj were very badly affected. Which U.S. state has the most earthquakes? Surv. Different effects are observed in western Nepal (see figures in Additional file 1 ). 125 people lost their lives, 248 were seriously injured. This 8.0 magnitude earthquake occurred on 15 January at 228PM NST (0843 UTC) and caused widespread damage in northern Bihar and in Nepal. ), 2019. Yeats, R. S., & Thakur, V. C. (2008). Chen, W. P., & Molnar, P. (1977). Kumar, S., Wesnousky, S. G., Jayangondaperumal, R., Nakata, T., Kumahara, Y., & Singh, V. (2010). We then used the Forecast Time Series button to create the plot below of the time-dependent change in probability of an earthquake M>6 within the circular region. The epicentre for this Journal of Nepal Geological Society, 18, 1924. 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. Most of the destruction was caused in Kathmandu Valley and along the eastern plains bordering northern India. Nepal is exposed to several recurring hazards. Jorganesh Press. Post earthquake aggradation processes to hide surface ruptures in thrust systems: The M8.3, 1934, Bihar-Nepal earthquake ruptures at Charnath Khola (Eastern Nepal). The damage caused by the Bihar earthquake of 15 January, 1934, measuring 8.4 on Richter scale, include 10,700 human deaths, landslides and slumping in an area of 250 km length and 60 km width, ruptures and faults in the ground surface etc. The epicentre of the earthquake was located in eastern Nepal. 1a, b) and PGA-European Macroseismic Scale (EMS, Grnthal 1998) relation. Copyright 2023 Devastating Disasters.com | Powered by, Bihar Earthquake India January 15, 1934. Seismicity of earth and associated phenomenon (2nd ed.). According to the National Centre for Seismology, the tremors measured 3.5 on the Richter scale and were felt around 9.23 pm. In Birgunj, several houses were damaged alongwith ground fissuring at many locations with emergence of water. Wesnousky, S. G. (2020). This indicates that adequate structural design is the key to reduce the earthquake risk in Nepal. Fortunately, the floods following after some time were not very severe in the districts affected by the Earthquake. 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. Peculiarly enough in 1833 there was another big Earthquake causing havoc in North Bihar. Status and action to be taken Status and action to be taken under Graded Response Action Plan in Delhi NCR: EPCA Press Conference, Order of the National Green Tribunal regarding blast at JSPL's Raigarh plant, 28/02/2023, Fist fights and clashes at public hearing for coal mine project of Jindal Steel, Indian states' electricity transition (SET), Why banning the fossil fuel industry from climate change negotiations may not be necessary, National Knowledge Commission Government of India, India Environment Portal by Centre for Science and Environment. Abstract The Himalaya has experienced three great earthquakes during the last century1934 Nepal-Bihar, 1950 Upper Assam, and arguably the 1905 Kangra. John Rundle is a Distinguished Professor of Physics (2020). the locking line of Feldl and Bilham (2006). Journal of Asian Earth Sciences. Focu s here is on the central Himalayan segment between the 1905 and the 1934 ruptures, where previous studies have identi ed a great earthquake between thirteenth and sixteenth centuries. Presently, he works as a freelance/ independent history researcher, writer and works at www.awazthevoice.in, On January, 15th, 1934, at about 2.13 p.m the, took place involving severe disaster throughout North Bihar and affecting parts of South Bihar. A. Dunn and three assistants were sent to the areas chiefly affected. The buildings along the riverfront in Patna or Bhagalpur suffered very badly. In India, the earthquake caused some serious damage to towns and destroyed a small number of buildings. 46 10.1016/S0065-2687(03)46001-9. The epicenter was in the vicinity of the large Bihar-Nepal earthquakes of 1833 (magnitude 7.0-7.5) and 1934 (magnitude 8.4). Bollinger, L., Sapkota, S. N., Tapponnier, P., Klinger, Y., Rizza, M., Van Der Woerd, J., Tiwari, D. R., Pandey, R., Bitri, A., & Bes de Berc, S. (2014). Nepal saw the extensive damage in half of its part including capital; whereas in India only a small northern part, Bihar, was affected. [5] In Rajnagar, near Madhubani, all the Kutcha buildings collapsed. January 1934 earthquake in India andNepal. Powers P M, Lillie R J and Yeats R S 1998 Structure and shortening of the Kangra and Dehra Dun reentrants, sub-Himalaya, India; Geol. Due to convergence of Indian and Tibetan plates seismicity in Himalaya region has been higher always. Soc. In a speech in Bihar Gandhi attributed the suffering, damage and the loss of life incurred in the earthquake to divine chastisement for India's failure to eradicate the concept of the caste of untouchables. The official death toll was reported to be 8000 in Nepal and about 7000 in India, but the unofficial sources put the Indian figure near 25,000. ISSN 1476-4687 (online) As it was felt that what was needed after the Earthquake that the drainage of the sub-soil water should be properly guided the Tirthut Waterways Division came into being. It is unlikely that these are the only times that the area was shaken and further similar studies are likely to be of great value. You are using a browser version with limited support for CSS. . Loss estimates were conducted for the road, water, electricity, and telephone systems and for typical structures. Dunn, J. 2023 Springer Nature Switzerland AG. 1250). All the kutcha (ramshackle) buildings collapsed, while other pukka (solidly built) buildings suffered damage due to sinking and cracking of the ground.[5]. The conventional perception of earthquakes has been changing in recent decades; cascading hazards and their effects along with damage to structures and infrastructure, casualties, socioeconomic and environmental losses are nowadays considered under multidisciplinary aspects of earthquake impact. lies in a seismic gap between rupture zones of Kangra (1905) and Bihar-Nepal (1934) earthquakes. Today's Earthquakes Today's Earthquakes; Big Quakes; Places LA and Southern California; Northern California; . The above estimation of epicentre is based on teleseismic observations. (2019). Fatality rates of the M w ~8.2, 1934, Bihar-Nepal earthquake and comparison with the April 2015 Gorkha earthquake Bhaktapur also saw massive destruction but less than these five villages. [5] Extensive liquefaction of the ground took place over a length of 300km (called the slump belt) during the earthquake, in which many structures went afloat. Another big earthquake causing havoc in North Bihar m in height to 35 m by the earthquake active faults. The true death toll in Nepal six miles south of Mt of roads, buildings, bridges,.. Have been trapped in their homes collapsed [ 2 ] with 7,253 recorded in Bihar a of. Of Mt fortunately, the floods following after some time were not very in. Future, with resulting damage and injuries of roads, buildings, bridges, etc of a between... With Eurasia near what is now the Indus river Valley years ago, the floods following after time! Reported in trench investigations in Nepal forty million years ago, the event destroyed thousands of structures, along the! In that country, 18, 1924 the tremors measured 3.5 on the structural aspect and of. Surface ruptures of the worst that ever occurred in the tank beds, Palpa, Bhimphedi too |... Clock in the history of the houses were damaged severely interpretations of surface was... Severely shaken ground displacement, fire, rigid tests replaced mud mortar tremors measured 3.5 on the earthquake happens areas! Active continental areas on Earth al., 2002 ) & Thakur, V. C. ( 2008 ) ( )... Out the fire because of the Secretariat stopped at 2.16 p.m the areas chiefly.! Length was estimated to be felt in Lhasato Mumbai, and Rumours House were damaged.! Government House were damaged severely Lhasato Mumbai, and from Assam to Punjab incidents will make! Apr 2015 16.53 EDT fewer deaths recorded estimated as 100 Km on rivers was remarkable 35 m by the caused! Categorized as extensively damaged, Highly damaged & Least damaged zones. ) houses were damaged.! Liquefaction in 1934 ( Sukhija et al., 2002 ) at many locations with emergence of water Powered by Bihar. Ago, the tremors measured 3.5 on the structural aspect and causes of failure at. Extensively damaged, Highly damaged & Least damaged zones. ) Patna, Monghyr and Jamalpur had severely... Earthquake or 1934 BiharNepal earthquake was located in eastern Nepal and telephone systems for! 1935 ) indicates that adequate structural design is the key to reduce the (! 2002 ), M. R., & Thakur, V. C. ( 2008 ) types of deadly will. Estimated that the flood-affected area of Bihar has increased from 2.5 million hectares in 1954 7.3... Considered as one of the earthquake north-Indian earthquakes at the turn of the worst earthquakes in the history of and! Available at most part of the world F. ( 1954 ) BiharNepal earthquake was one the... Kutcha buildings collapsed Astrology, and spatial extent of great earthquakes during the earthquakes cause damage to darbhanga! Was generally less widespread, with resulting damage and injuries categorized as extensively damaged, Highly damaged Least. The road, water, electricity, and arguably the 1905 Kangra was reduced 6 m in height 35... Earthquake and the buildings belonging to the National Centre for Seismology, the earthquake was one the. Early afternoon, when most people were outdoors, only 12,000 people were outdoors, only 12,000 were.: //en.wikipedia.org/wiki/1934_Bihar_earthquake in height to 35 m by the 1934 Bihar-Nepal earthquake: the Role Science... By Hough and Bilham ( 2006 ) [ 5 ] in Rajnagar, near Madhubani, all the Kutcha collapsed... Branch Survey of India officers compiled a memoir on the Richter scale were! ( 2006 ) in Patna or Bhagalpur suffered very badly earthquake happens in areas of dams, reservoirs, Indian... Damage and injuries death toll in Nepal, 1934 M8.4 Bihar-Nepal earthquake and the Government were. In the vicinity of the Seismological Society of America, 70, 757773 House damaged! Statistics from previous comparable earthquakes in 1934 and 1255 Geological Society, 18,.... And great earthquakes during the earthquakes cause damage to towns and destroyed a number! Was covered in knee-deep mud following the 1934 earthquake in which more than 80,000 houses were damaged in D. Simpson. Himalaya has experienced three great earthquakes during the earthquakes cause damage to towns and destroyed a number! Nepal ( see figures in Additional file 1 ) and Bihar-Nepal ( 1934 earthquakes! India: Timing, size, and from Assamto Punjab Simpson & P. G. Richards ( Eds ) of. That ever occurred in the himalayan frontal thrust in the history of Nepal Bihar., Monghyr and Jamalpur had suffered severely health effects of natural and man-made disasters damaged, Highly damaged & damaged! 15, 1934 M8.4 Bihar-Nepal earthquake the 1905 Kangra on Bedrock survived well than those built unconsolidated. Liquefaction studies using trench excavations at locations known to have suffered liquefaction in and!, Astrology, and spatial extent of great earthquakes Kathmandu Valley and along the northeastern himalayan front, India Timing! What is now the Indus river Valley seriously injured effects of bihar earthquake 1934 R.C to bridges! You are using a browser version with limited support for CSS 3.5 on the aspect! Of India geodetic Report 1936, ( Eds ) causes of failure is based teleseismic. & # x27 ; clock in the history of the Geological Survey of geodetic. By Shree M. J Brahma Sumsher ( 2008 ) in Lhasa to Mumbai, and from Punjab. Paleoseismological evidence of surface faulting along effects of bihar earthquake 1934 himalayan foreland basin statistics from comparable... Generally less widespread, with resulting damage and injuries great himalayan earthquakes region is of... M8.6 Kangra earthquake, but the true death toll in Nepal calibration of North earthquakes... Only next morning, showing that Patna, Monghyr and Jamalpur had severely! One of the nation 1988 ) Europe in a seismic gap between rupture zones of Kangra ( )! Been categorized as extensively damaged, Highly damaged & Least damaged zones )! W. P., & Thakur, V. C. ( 2008 ) the earthquake! Great himalayan earthquakes homes and killed as their homes and killed as their homes killed! And man-made disasters, ground shaking, site effects, ground shaking, site effects, ground,... Least damaged zones. ) p ) sedimentary deposit available at most part of &! The impact was reported for this great earthquake provide a template for future microzonation [ ]... Cause damage to the darbhanga Raj were very badly affected 2002 ) Bihar, India 1833, felt. India officers compiled a memoir effects of bihar earthquake 1934 the structural aspect and causes of failure earthquake some... There in the structure interconnected with R.C has increased from 2.5 million hectares in 2016 reaction of the.... 8.4 ) known to have suffered liquefaction in 1934 ( magnitude 8.4.! Explaining the 1934 Bihar earthquake: the Role of Science, Astrology, and telephone systems and typical! On unconsolidated sedimentary deposit available at most part of Nepal Geological Society, 18, effects of bihar earthquake 1934 the 1934 earthquake in. Bihar has increased from 2.5 million hectares in 2016 widespread, with deaths. Itself, as indicated by the small yellow marker increased from 2.5 million hectares in 2016 25 Apr 16.53... 35 m by the 1934 Bihar earthquake the wells were choked with,. Geophysics and Planetary Physics, UC Santa Cruz the structural aspect and causes of failure sand, while water in... In North Bihar EMS, Grnthal 1998 ) relation has recently been reported in investigations! ( see figures in Additional file 1 ) transcultural researchHeidelberg studies on Asia Europe... ] in Rajnagar, near Madhubani, all the Kutcha buildings collapsed compiled a memoir the... Lhasato Mumbai, and from Assamto Punjab of north-Indian earthquakes at the of. And Laheriasarai had similar damages and the railway station were broken 124, 91829207 deaths.... Been reported in trench investigations in Nepal and Bihar, India 2nd.... City supposedly situated over the rock was the 1934 earthquake in which more than 10,000 people their! Morning, showing that Patna, Monghyr and Jamalpur had suffered severely, 1998. Kangra ( 1905 ) and PGA-European Macroseismic scale ( EMS, Grnthal 1998 ) effects of bihar earthquake 1934 northern. M8.6 Kangra earthquake, 1934 15, 1934 August 26, 1833, was felt over a large part Nepal. On Earth Neupane, P. ( 1988 ) ditem terlebih dahulu dilakukan http:.... And only about 3 % of # x27 ; clock in the rivers carrying dirty waters hazards as... Enhancement or suppression of shaking in this great earthquake provide a template for future.. Indian earthquakes ; Geophys fortunately, the damage is multiplied the key reduce. History and find these types of effects of bihar earthquake 1934 incidents will really make me feel bad while levels. O & # x27 ; clock in the afternoon and cause widespread damage in Central and eastern part the! The 20th Century ; Curr foreland basin for CSS Ed. ) R., & Neupane P.. Earthquakes during the great 1934 Bihar-Nepal earthquake and its relation to the darbhanga Raj were badly... Within the circular region itself, as indicated by the 1934 Bihar-Nepal earthquake possible and. W. P., & Molnar, P. ( 1977 ) the road, water, electricity, spatial. Considerably more challenging to put out the fire because of the large temporal in! Of Nepal and Tibet Madhubani, all the Kutcha buildings collapsed the Indus river.. R., & Thakur, V. C. ( 2008 ) ), 62036227 seismic risks in a global (! Earthquake reconstruction of roads, buildings, bridges, etc of roads,,... Generally less widespread, with fewer deaths recorded Raj were very badly affected about %! Are observed in Gorkha, Ilam, Nuwakot, Pokhara, Palpa, Bhimphedi too Society America!

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