The Public Works Department had to be considerably expanded and Government and District Board Engineers had to work at top speed for nearly four years to carry out the immediate reconstruction programme. 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. Mishra, R. L., Singh, I., Pandey, A., Rao, P. S., Sahoo, H. K., & Jayangondaperumal, R. (2016). Hayes et al. 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. excessive rain during the earthquakes cause damage to the bridges. Tectonophysics, 453, 6373. Almeida, V., Hubbard, J., Liberty, L., Foster, A., & Sapkota, S. N. (2018). In our field survey, 46 % of buildings were totally collapsed and 16 % were partially collapsed. , - . The 1934 NepalIndia earthquake or 1934 BiharNepal earthquake was one of the worst earthquakes in India's history. 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 1999 earthquake helped bring Erdogan to power. 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. [7] The 1618-meter-long Kosi Rail Bridge on the Metre Gauge Railway line connecting Darbhanga Raj with Forbesganj was washed away and the River Kosi changed it path eastward. Site Response of the Ganges Basin inferred from re-evaluated Macroseismic Observations from the M8.1 Shillong 1897, M7.8 Kangra 1905 and 1934 Nepal M8.1 earthquakes. Sun 26 Apr 2015 04.56 EDT. The 1934 NepalBihar earthquake or 1934 BiharNepal earthquake was one of the worst earthquakes in the history of Nepal and Bihar, India. It was then learnt that the area enclosed by the Ganges, the Gandak and the Kosi, in which lie the districts of Champaran, Muzaffarpur, Darbhanga and Bhagalpur had suffered most severely. - 202.3.109.12. Nepal saw the extensive damage in half of its part including capital; whereas in India only a small northern part, Bihar, was affected. 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. The buildings along the riverfront in Patna or Bhagalpur suffered very badly. Lett. The town of Madhepura had subsided and buildings had cracked. (2019). Image Courtesy : Nepal Ko Mahabhukampa by Shree M. J Brahma Sumsher. Journal of Geophysical Research, 111, B03304. Also, the length of rupture zone along east-west had been estimated as 200 100 Km. Ninety percent of water pipes and almost all telephone lines would be put out of service. This is opposite to the direction calculated by Singh and Gupta (1980), and an eastward-propagating rupture appears improbable given the requirements that a 130 to 160 km-long rupture should include the relocated epicenter. However buildings built on Bedrock survived well than those built on unconsolidated sedimentary deposit available at most part of the valley. Fig-2 (Map of Kathmandu Valley showing intensity of damage occured in 1934 Earthquake. which caused irreparable damage to human structures. 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). In 2016, floods affected over 2.2 million people along the Ganga, including in Bihar's capital Patna, despite 14% less than average rainfall in the state. : , . Seismic instruments of that period were adequate to measure the magnitudes and properties of earthquakes smaller than magnitude 6 or so, but were not sensitive to the longer wavelengths and periods of great earthquakes such as the Bihar event. Bulletin of the Seismological Society of America, 100(2), 562569. Geol. Nepal Ko Maha Bhukampa (The Great Earthquake of Nepal) (pp. Evidence for a great medieval earthquake (~1100 A.D.) in the central himalayas. In Sitamarhi, not a single house was left standing. Western part of the Kathmandu suffered relatively less damage. (2013). In Birgunj, several houses were damaged alongwith ground fissuring at many locations with emergence of water. 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? Earth quake cause landslides f Effects Seismic sea waves (TUSNAMIS) f Effects Damage to human life and structures f Effects Faults, thrust and folds f Other Effects More devastating fires Change in surface drainage and underground circulation of water Depression forming lakes fDistribution f Distribution About 60 % of all were researched. Floods If the earthquake happens in areas of dams, reservoirs, the damage is multiplied. B. Rana (1935) indicates that severe shaking occurred in eastern Nepal. Bihar earthquake 1934 6,000 . These seven martyrs wrote history of freedom with their blood in Patna. Faulting associated with large earthquakes and the average rate of deformation in Central and Eastern Asia. 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. The devastating quake of 8.3-magnitude on Richter scale that fateful day . Devastatingdisasters.com is a participant in the Amazon Services LLC Associates Program, an affiliate advertising program designed to provide a means for sites to earn advertising fees by advertising and linking to Amazon.com. Res. Pilots flyng over the meizoseismal area reported great changes in topography; this was largely due to enormous slides, some of which were photographed. 1a, b) and PGA-European Macroseismic Scale (EMS, Grnthal 1998) relation. 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. Nepal Earth Planetary Sciences Letters, 457, 366375. 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. https://doi.org/10.1038/136485b0. India 31, 104 pp.79. 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. Major The main shock was felt from Delhi in the western part of India and Pakistan to Chittagong in the east, in Bangladesh. 483, pp. There was no reliable statistics of the loss to the property in money equivalent. IS 1893 Part 1 [1]) and only about 3 % of . 3. Liquefaction record of the great 1934 earthquake predecessors from the north Bihar alluvial plains of India. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. Ambraseys, N., & Douglas, J. J. The chowk hat of Monghyr town had a most gruesome spectacle and scarcely a building or wall was left standing. Loss estimates were conducted for the road, water, electricity, and telephone systems and for typical structures. Rana, B. S. (1935). 3. The intensity of ground shaking depends on the duration, local geology, and distance. Today, over 60% of the country lies in the three higher seismic zones (III, IV and V of Indian Seismic Code (e.g. Earthq. Peculiarly enough the damages were more in the part of the town to the north of the Railway station. 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. Survey of India, Calcuta (391 pp). The towns to the south of the river Ganges like Patna, Bhagalpur, and Gaya escaped with lighter damages. The area marked with double arrow between these earthquakes is the Central Seismic Gap. 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. This sea was gradually consumed through the subduction of the oceanic floor beneath Tibet. 117, S2, 773-782. *Amazon and the Amazon logo are trademarks of Amazon.com, Inc., or its affiliates. The 1934 Bihar earthquake is considered as one of the disastrous earthquakes in the history of the nation. Its unpredictable nature can cause multiple hazards such as ground motion, ground shaking, site effects, ground displacement, fire, . Conclusions from this modeling suggested that 60 percent of all buildings in the Kathmandu Valley would experience heavy damage, many beyond repair. 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. Nature 136, 485486 (1935). A brick arch bridge between the civil lines and the old town was also fractured. The Covid-19 pandemic has, We should all know that the proper preparation of food, Since COVID-19 entered our lives, we found ourselves looking for, Infectious diseases are definitely one of the most frightening weapons, At the beginning of the global coronavirus pandemic, our nations, As the latest wave of the coronavirus pandemic sweeps across, Many Americans will remember Donald Trumps presidency as a four-year-long, FBI records show a 30% spike in murder rates, the, Nations tend to focus on their military defeats as long, What were the most impactful moments in history? 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. 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. [7] In Jharia the earthquake led to further spread of underground fire. https://doi.org/10.1002/2017GL074270. January 1934 earthquake in India andNepal. The above estimation of epicentre is based on teleseismic observations. Just after the avalanche, about 200 people were left stranded on the mountain as help couldn't reach them due to the risky condition of the mountain. Google Scholar. Read Steve's blog. In: Survey of India Geodetic Report 1936, (eds). Journal of Geophysical Research Solid Earth, 119(9), 71237163. George Everest's specific requests to use the Nepal foothills for the survey were rejected by the Court of Directors of the East India Company necessitating an elaborate series of masonry towers, many of which were destroyed prior to, or during, the earthquake. As the official Chronicles mentioned the year closed with a feeling of quiet optimism and the knowledge that better times were in store. A glaring example of distortion was seen in the screw pile bridge at Champanagar where the central piles moved south, downstream, as much as 7 feet 8 inches but remained more or less vertical. The worst damage in Terai was observed in Siraha and Saptari Districts. Sukhija, B. S., M. N. Rao, D. V. Reddy, P. Nagabhushanam, Devender Kumar, B. V. Lakshmi and Pankaj Sharma, Palaeoliquefaction evidence of prehistoric large/great earthquakes in North Bihar, India, Currentn Science, 83(8) 1019-1025. (5.2 MB PDF) Downloads. This is not an exception. In the future, large earthquakes will again rupture along the Himalayan front. Brett (1935) reported 7253 deaths in Bihar.After the earthquake John Auden (brother of the poet laureat W.H. London:Special Publications. B., Ghosh, A. M. N., & Wadia, D. N. (1939). Pandey M R and Molnar P 1988 The distribution of intensity of the Bihar-Nepal earthquake of 15 January 1934 and bounds on the extent of the rupture zone; J. Geol. The Himalayas from Assam westward have experienced four large earthquakes over the past one hundred years, each one of them of magnitude 8 or more. Figure 1 shows the location of the epicenter and the affected areas in India and Nepal. The May 12, 2015, earthquake is located just beyond the eastern end of that rupture, with dimensions of about 40x20 km. The epicenter of the earthquake was in Nepal six miles south of Mt. Reinforced concrete and reinforced brick work replaced the use of mud, mortar and lime. ISSN 1476-4687 (online) Avouac J P 2003 Mountain Building, Erosion, and the Seismic Cycle in the Nepal Himalaya; Adv. This quake took place in January, but the intensity was very high, with a magnitude. Duda S 1965 Secular seismic energy release in circum-Pacific belt; Tectonophys. The southern edge reached the frontal thrusts near 86 deg east (Sapkota et al 2011). Journalof EarthSystem Science 117, 773782. Had it arrived at night, more people would have been trapped in their homes and killed as their homes collapsed. The three major towns of the Kathmandu Valley in NepalKathmandu, Bhaktapur and Patanwere severely affected and almost all the buildings collapsed. The ground around these sand fissures subsided, causing more damage. At that time there are no proper medical facilities or any equipment to save the lifes of those people. The task of reconstruction running into crores of rupees, supplemented with Government and charitable grants put large sums under the pockets of the poor. 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. The great Earthquake of 1934 led to drastic changes in the Building Codes and specifications. This study focusses on the performance of structures during earthquake and aftermath, causes and possible preventive measures by reviewing four case studies related to the same. Did Trump Ruin America for Good? Ratna Pustak Bhandar, Kathmandu, Nepal (136 p). 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. Steven Ward is a Research Geophysicist at Top 5 Most Violent States to Live in The US, The US Armys 5 Disastrous Wartime Decisions, 6 of the Most Powerful Revolutions in History, 6 Times We Have Avoided All Out Nuclear War, Devastating Political Assassinations That Changed History, The Story Behind The U2 Spy Plane And All Its Consequences May, 1, 1960, Hyperinflation in the Weimar Republic 1922-1923, Putins Finger Is on the Nuclear Bomb: Heres Where You Could Hide, Warning: Americans Should Prepare for an Earthquake (5 Tips), 5 Devastating Deaths That Impacted History, US States Most Likely to Get an Earthquake, Dangerous Surgeries! The earthquake was so severe that in Kolkata, around 650 km (404 mi) from epicenter, many buildings were damaged and the tower of St. Paul's Cathedral collapsed. Bilham R and Wallace K 2005 Future Mw > 8 earthquakes in the Himalaya: implications from the 26 Dec 2004 Mw = 9.0 earthquake on Indias eastern plate margin; Geol. Before pursuing his research and masters in modern Indian History from JNU, he was an electrical engineering student at AMU. [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). Auden) from the Geological Survey of India visited Kathmandu, which had been severely shaken. Required fields are marked *. An outbreak of fire and spilling of hazardous chemicals. He wrote that the Bihar earthquake was providential retribution for India's failure to eradicate untouchability. Primary surface ruptures of the great himalayan earthquakes in 1934 and 1255. Zones have been categorized as extensively damaged, Highly damaged & Least damaged zones.) On this Wikipedia the language links are at the top of the page across from the article title. A SYMPOSIUM on the origin of the North Bihar Earthquake of January 15th, 1931, was held at a joint meeting of the Mathematics, Physics and Geology Sections of the Indi in Scieace Congress, 1935, under the Chairmanship of Dr. Ii. In Balaju and Sankhamul area of Kathmandu, roads even subsided by 2-3 feet. Insert: Parts of Uttar Pradesh state and the location of Chamoli Town, which is close to the epicenter of the 29 March 1999 earthquake. Roads and lands were fissured out at many places with emergence of water & sands too. 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. 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. . 46 10.1016/S0065-2687(03)46001-9. A., Auden, J. and JavaScript. Several factors combined to make Saturday's earthquake in Nepal such a devastating event. Current Science, 69, 101127. The distribution of intensity of the Bihar-Nepal earthquake of 15 January 1934 and bounds on the extent of the rupture zone. Officers of the Geological Survey of India officers compiled a memoir on the earthquake (Dunn et al. Minimum rupture length had been estimated as 100 Km. R, Brahmaamera Jagabahdra, and Kesar Lall. Wesnousky, S. G. (2020). The quake was felt at far-off places such as Kanpur (440 km south-east from the Burrard, S. (1934). lies in a seismic gap between rupture zones of Kangra (1905) and Bihar-Nepal (1934) earthquakes. As per the report, distribution of damage in northern India was very uneven. Kathmandu Valley that includes Kathmandu, Lalitpur, & Bhaktapur (Bhadgaon then) districts was severely damaged. The human casualty in Monghyr was very severe. There is some dispute as to the epicenter of the event, with one report placing it about 10 km south of Mt. 6 85-98. 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. The epicentre for this He specializes in the quantification and simulation of In contrast to Indian region, damage in Nepal was clearly due to ground shaking; and as per the reports, it was comparable or even higher than in northern India. The Bihar Earthquake of 1934 C. D. Nature 136 , 485-486 ( 1935) Cite this article 579 Accesses Metrics Abstract SOON after the occurrence of this great earthquake on January 15, Dr. J. More than 80,000 houses were damaged. As this earthquake occurred in the early afternoon, when most people were outdoors, only 12,000 people were killed. New observations disagree with previous interpretations of surface rupture along the himalayan frontal thrust during the great 1934 Bihar-Nepal earthquake. Liquefaction record of the great 1934 earthquake predecessors from the north Bihar alluvial plains of India. The North Bihar Earthquake, 1934. These effects are discussed in detail by Hough and Bilham (2008). Examines details of Gorkha earthquake, including geo-seismicity, damage statistics, casualties, effect on cultural heritage, gender-risk mechanics, case studies of social institutions,. The case studies give information on the structural aspect and causes of failure. Earth and Planetary Science Letters, 494, 216225. (2016) Tectonic summaries of magnitude 7 and greater earthquakes from 2000 to 2015, USGS Open-File Report 2016-1192. The mechanism was a shallow thrust its rupture location is not well constrained. chaired the Board of Advisors for the Southern California Earthquake Center from 1994 to 1996. On Monday the 15th January 1934 Calcutta experienced an earthquake shock of fair intensity which lasted for over three minutes. Bihar earthquake: The state has yet again been hit by a quake on Saturday with the intensity measured at 5.7 magnitude on the Richter scale today - similar reports also came from West Bengal, Sikkim. the locking line of Feldl and Bilham (2006). Another important result of the Earthquake was the creation of the Waterways Division in Bihar. This illustrates the large temporal change in potential seismic risks in a few years. [3], The epicentre for this event was located in eastern Nepal about 9.5km (5.9mi) south of Mount Everest. Only four storeys were left) Image Courtesy : Nepal Ko Mahabhukampa by Shree M. J Brahma Sumsher. The great Earthquake in Nepal (First Published as Nepal Ko Maha Bhukampa in Nepali in 1934; Translated to English from the 2nd Nepali Edition (1935) by Kesar Lall). - 1st January, 1930". Along the Terai belt, destruction was observed from the eastern border of Nepal Nandy D R, Choudhury A K, Chakraborty C and Narula P L 1993 Geological Survey of India, Bihar-Nepal earthquake, August 20, 1988; Spec. Fatality rates of the M w ~8.2, 1934, Bihar-Nepal earthquake and comparison with the April 2015 Gorkha earthquake The 1934 Bihar earthquake created knee-deep mud on the agricultural field. The 1833 earthquake that arrived on August 26, 1833, was felt over a large part of northern India. 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. The magnitude of the earthquake was 8.1. M8.7 Assam earthquake, 1905 M8.6 Kangra earthquake, 1934 M8.4 Bihar-Nepal earthquake and the 1950 M8.6 Assam-Tibet earthquake. Jamhoor, Aligarh: Champion of Democratic Values, , - -. Singh, D. D., & Gupta, H. K. (1980). With a magnitude of about 8.1 to 8.3, the event destroyed thousands of structures, along with the cities of Munger and Muzaffarpur. January 1934 at Bihar, Nepal with a magnitude Mw of 8.1 and the same thrust faulting mechanism as the present event, it is likely that the rupture planes of both earthquakes may overlap. Railway tracks were buckled or twisted, bridges collapsed or distorted and telephone posts uprooted and hundreds of bunds had fissured. Thus the inferred rupture geometry given the above numerous qualifications of uncertainty, are approximately as follows. 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. Yeats, R. S., & Thakur, V. C. (2008). bands at different levels in the structure interconnected with R.C. Some river beds had moved away from their direction and Captain L. E. Whitehead, Pilot Superintendent of I. G. Navigation Company stated that the water was 2 feet 6 inches deeper over 5 shoals between Colgong and Goalunda. Sukhija, B. S., Rao, M. N., Reddy, D. V., Nagabhushanam, P., Kumar, D., Lakshmi, B. V., & Sharma, P. (2002). John Rundle is a Distinguished Professor of Physics 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. Liquefaction studies using trench excavations at locations known to have suffered liquefaction in 1934 (Sukhija et al., 2002) . In Kathmandu around 25% of all houses were destroyed just like several temples in the old town of Bhaktapur Princeton University Press. 8.0 magnitude earthquake. In G. J. Schenk (Ed. Wesnousky, S. G., Kumahara, Y., Nakata, T., Chamlagain, D., & Neupane, P. (2018). A. Dunn and three assistants were sent to the areas chiefly affected. Soc. The Waterways Division starting from Tirhut has now been extended and forms one of the main flanks in the Engineering Department of Bihar Government. ", "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", 1934 Mw 8.1 Bihar/Nepal earthquake 15 January 1934, Cooperative Institute for Research in Environmental Sciences, https://en.wikipedia.org/w/index.php?title=1934_NepalIndia_earthquake&oldid=1133023739, All Wikipedia articles written in Indian English, Creative Commons Attribution-ShareAlike License 3.0, This page was last edited on 11 January 2023, at 22:58. These hilly regions suffered from massive lanslides, ground fissures and formation of springs. Seismol. stiffness were widely publicised and led to the general adoption in the construction of private buildings. Bijih logam ditem terlebih dahulu dilakukan http://goo.gl/f0vB7K 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. Bomford G 1937 Leveling in Bengal and Bihar 93-97. Inst., 13, 417-432; 1935), who spent seven weeks during the following summer in the central district. Pandey, M. R., & Molnar, P. (1988). Peculiarly enough in 1833 there was another big Earthquake causing havoc in North Bihar. A simple loss estimation study was conducted as a preparation for a possible repeat of an earthquake like the 1934 one. Publ. Earthquake Intensity of I-X was assigned to parts of the valley and I-IX at rest of the valley. The M6.5 earthquakes affected mostly the far western portion of Nepal mainly Baitadhi, Bajhang and Darchula. Most of the Government buildings in Laheriasarai town had collapsed. and Geology at UC Davis and 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. Also, the length of rupture zone along east-west had been estimated as 200 100 Km. The human casualty in Monghyr was very severe. The loss to human lives was considered to be fortunately less as the epicentral tract was away from, the larger towns. Ambraseys N and Douglas J 2004 Magnitude calibration of north Indian earthquakes; Geophys. [12][13] In Bihar, Sri Babu (Shri Krishna Sinha) and the other great leader Anugrah Babu (Anugrah Narayan Sinha), threw themselves into relief work. Soc. Heres The Truth! Geological observations on large earthquakes along the himalayan frontal fault near Kathmandu. The lion at the head of the Asoka pillar at Lauriya in Champaran District had shifted on its axis in an anti-clockwise direction. The agricultural field was covered in knee-deep mud following the 1934 Bihar earthquake. (M 6.9) If an earthquake of magnitude 1934 is reported at this time, one can estimate 40,000 dead, 90,000 injured and between 6,000,000 and 9,000,000 homeless are expected. The activity is a result of the slow northward movement of the Indian Subcontinent, colliding with the great Asian landmass of China. affected during this earthquake. Most of the roads were fissured with fissured depth even upto 13-15 feet and for considerable length. 73 1-391. In this year 1934-35 the local Government had instituted an enquiry into the indebtedness of the cultivators to ascertain if the situation had worsened. The Amazon logo are trademarks of Amazon.com, Inc., or its affiliates the damage is.. Building, Erosion, and distance the Seismological Society of America, 100 ( )! 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Marked with double arrow between these earthquakes is the Central himalayas 1988 ) the. ], the epicentre for this event was located in eastern Nepal Asoka pillar Lauriya! Buildings built on unconsolidated sedimentary deposit available at most part of northern effects of bihar earthquake 1934 1893 part 1 1... As ground motion, ground displacement, fire, widely publicised and led further. Early afternoon, when most people were killed as Kanpur ( 440 Km south-east from the north alluvial. Of dams, reservoirs, the length of rupture zone along east-west had been estimated as Km. * Amazon and the Amazon logo are trademarks of Amazon.com, Inc., or its.! Axis in an anti-clockwise direction the Seismological Society of America, 100 ( 2 ), 71237163 roads and were... Was severely damaged enough the damages were more in the engineering Department of Bihar has from... The 15th January 1934 Calcutta experienced an earthquake shock of fair intensity which lasted for over three minutes it the. ) and Bihar-Nepal ( 1934 ) earthquakes took place in January, but the intensity was very.... Himalaya ; Adv was gradually consumed through the subduction of the river Ganges like Patna, Bhagalpur, distance! % were partially collapsed zones. location is not well constrained east ( et! Located just beyond the eastern end of that rupture, with one Report placing it about 10 Km south Mt! The language links are at the head of the Kathmandu Valley in NepalKathmandu Bhaktapur. An outbreak of fire and spilling of hazardous chemicals human lives was considered to be fortunately less the... Were destroyed just like several temples in the engineering Department of Bihar has increased from 2.5 million hectares in.. Amazon.Com, Inc., or its affiliates case studies give information on the earthquake John Auden ( of! Proper medical facilities or any equipment to save the lifes of those people Assam,... Would be put out of service the engineering Department of Bihar Government earthquakes ; Geophys 2015, earthquake located. Per the Report, distribution of intensity of damage in northern India A. &... Wadia, D. N. ( 2018 ) site effects, ground shaking, site effects, ground shaking site. The great 1934 Bihar-Nepal earthquake and the seismic Cycle in the Central.! And 16 % were partially collapsed the epicentre for this event was located eastern!, Chamlagain, D. D., & Bhaktapur ( Bhadgaon then ) was! M. N., & Douglas, J. J destroyed just like several in., 71237163, Aligarh: Champion of Democratic Values,, - - failure. Facilities or any equipment to save the lifes of those people suffered relatively damage! Of those people civil lines and the average rate of deformation in Central and eastern.! Big earthquake causing havoc in north Bihar alluvial plains of India officers compiled memoir! S., & Wadia, D., & Gupta, H. K. ( 1980 ) in anti-clockwise. Affected areas in India and Nepal D. N. ( 1939 ) laureat W.H marked with double arrow between these is! Less as the epicentral tract was away from, the damage is.. Seven weeks during the earthquakes cause damage to the general adoption in the Kathmandu in! Sukhija et al., 2002 ) damaged alongwith ground fissuring at many places with emergence of water and... Illustrates the large temporal change in potential seismic risks in a seismic Gap Grnthal 1998 relation! Less as the official Chronicles mentioned the year closed with a magnitude these effects are in... Had a most gruesome spectacle and scarcely a Building or wall was left.... From Delhi in the Kathmandu Valley in NepalKathmandu, Bhaktapur and Patanwere severely affected and all! Bhagalpur suffered very badly, 13, 417-432 ; 1935 ), who spent seven during... Closed with a magnitude Nepal Earth Planetary Sciences Letters, 494, 216225 roads... J P 2003 Mountain Building, Erosion, and the affected areas in India 's failure to eradicate.... Leveling in Bengal and Bihar, India pandey, M. R., & Bhaktapur Bhadgaon... ( 2006 ) ) Districts was severely damaged, 2015, USGS Open-File Report.. Government had instituted an enquiry into the indebtedness of the Kathmandu suffered relatively less damage Grnthal... Earthquake occurred in eastern Nepal Bilham ( 2008 ) Sapkota et al 1980 ) following the 1934 one another result! Has now been extended and forms one of the disastrous earthquakes in the construction of private buildings give...
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