The first was its basic . [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). Following the major quake, twenty-eight numbers of after-shocks were recorded; where few of them were greater shocks too. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. Journal of Earth System Science. Bulletin of the Seismological Society of America, 70, 757773. 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. 2022 Springer Nature Singapore Pte Ltd. Rajendran, C.P., Rajendran, K. (2022). Whereas areas like Dhankuta, Sindhupalchowk, Rasuwagadhi, Chainpur, Taplejung also suffered damage. 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. (1939) and by Major General Brahma Geophys. Seismicity of the earth and associated phenomena. Get the most important science stories of the day, free in your inbox. Roads and lands were fissured out at many places with emergence of water & sands too. On this Wikipedia the language links are at the top of the page across from the article title. The source characteristics of Gorkha earthquake show that the maximum slip of 5 to 6 m was concentrated at a depth of 8 to 15 km, 70 km southeast of the epicenter [ [8] , [9 . Great detachment earthquakes along the himalayan arc and long-term forecasting. 82 2945-2969. 3. The chowk hat of Monghyr town had a most gruesome spectacle and scarcely a building or wall was left standing. Conclusions from this modeling suggested that 60 percent of all buildings in the Kathmandu Valley would experience heavy damage, many beyond repair. 2015 Nepal Earthquake Ahsan Jadoon Department of E&ES Bahria University 2. There was a serious earthquake in Bihar in 1934, the devastating effects of which GTG captured by photograph in great detail. Ambraseys N 2000 Reappraisal of north-Indian earthquakes at the turn of the 20th Century; Curr. The 1934 Bihar earthquake is considered as one of the disastrous earthquakes in the history of the nation. The epicentre for this https://doi.org/10.1029/2004JB003309. Following are the effects of the earthquake: Ground shaking: Surface waves that are near the epicenter are responsible for the earthquake. Today, over 60% of the country lies in the three higher seismic zones (III, IV and V of Indian Seismic Code (e.g. 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. As per the report, distribution of damage in northern India was very uneven. This innovation has lead to decrease the effect of earthquake on a building and is evaluated . 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. Chen W-P and Molnar P 1977 Seismic moments of major earthquakes and the average rate of slip in Central Asia; Geophys. which caused irreparable damage to human structures. Faulting associated with large earthquakes and the average rate of deformation in Central and Eastern Asia. 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. Along the Terai belt, destruction was observed from the eastern border of Nepal Only four storeys were left) Image Courtesy : Nepal Ko Mahabhukampa by Shree M. J Brahma Sumsher. The task of reconstruction running into crores of rupees, supplemented with Government and charitable grants put large sums under the pockets of the poor. 1.Bihar Earthquake, 1934 This quake is considered to be one of the worst quakes in Indian history. In H. J. Couchman (Ed. 73 1-391. As per the recorded data velocity of ground shaking had been estimated in Kathmandu as 8 ft/sec with higher values of 10 ft/sec in Bhaktapur, and in some villages of Lalitpur. Bilham, R. (2019). 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). Overcoming the odds How Babur Arafat brought Pride to India. 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). This indicates that adequate structural design is the key to reduce the earthquake risk in Nepal. Of interest is that the localized enhancement or suppression of shaking in this great earthquake provide a template for future microzonation. Explaining the 1934 Bihar-Nepal Earthquake: The Role of Science, Astrology, and Rumours. 117, S2, 773-782. 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. New quake hits Turkey, toppling more buildings: 1 killed Officials say a magnitude 5.6 earthquake shook southern Turkey causing some damaged buildings to collapse and killing at least one person Feb. 25, 2023, 9:00 AM ET (AP) Turkey launches investigation into 612 people after quake The human casualty in Monghyr was very severe. The ground around these sand fissures subsided, causing more damage. At Lakhisarai the water was observed to recede from mid-stream and sand gushed up the exposed bed of the river. Examines details of Gorkha earthquake, including geo-seismicity, damage statistics, casualties, effect on cultural heritage, gender-risk mechanics, case studies of social institutions,. 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. The following entry is based on summaries found in Bilham et al (1998; 2001) and Hough & Bilham,(2008). The 1999 earthquake helped bring Erdogan to power. Majority of seismic events in the Kumaun-Garhwal Himalayas region is located close to the MCT or north and south of it. India As of 27 April 2015 at 4:14 p.m., Indian Home Minister Rajnath Singh,confirmed that56 people died in the state of Bihar,12 in Uttar Pradesh,3 in West Bengal and 1 in Rajasthan. Location and magnitude of the 1833 Nepal earthquake and its relation to the rupture zones of contiguous great Himalayan earthquakes. With the 7.8-magnitude earthquake hitting Turkey this Monday. Darbhanga and Laheriasarai had similar damages and the buildings belonging to the Darbhanga Raj were very badly affected. In: P. J. Treloar, & M. P. Searle (Eds. Impact Summary; 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. The total casualties was about 10,000 people in the area and many thousands were injured by the falling debris. Half of all electric lines would be knocked out. (Following is a reproduction of the account written by P.C Roy Choudhury). the Executive Director of the APEC Collaboration for Earthquake Simulations. The loss to human lives was considered to be fortunately less as the epicentral tract was away from, the larger towns. . Nasu, N. (1935). Everest. Gutenberg B and Richter C F 1954 Seismicity of the Earth and Associated Phenomena; Princeton University Press, Princeton, 310pp. The maximum Mercalli Intensity was estimated about XI, on a scale of I to XII. Earthquakes of the Indian Subcontinent pp 159171Cite as, Part of the GeoPlanet: Earth and Planetary Sciences book series (GEPS). 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. Wesnousky, S. G., Kumahara, Y., Chamlagain, D., Pierce, I. K., Karki, A., & Gautam, D. (2017a). bands at different levels in the structure interconnected with R.C. He wrote that the Bihar earthquake was providential retribution for India's failure to eradicate untouchability. The impact was reported to be felt in Lhasato Mumbai, and from Assamto Punjab. It was the worst that ever occurred in that country. The influence of regional earthquakes on the time series can be seen, producing the sharp drops in probability. Springer, Singapore. Fortunately, the floods following after some time were not very severe in the districts affected by the Earthquake. Communications were severely tampered with. 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. Earthquake Intensity of I-X was assigned to parts of the valley and I-IX at rest of the valley. Intensities reported for the earthquake were rendered complex by the prevalence of liquefaction, by basin resonance and by directivity. India 31, 104 pp.79. Sapkota, S., Bollinger, L., Klinger, Y., et al. 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. Rizza, M., Bollinger, L., Sapkota, S. N., Tapponnier, P., Klinger, Y., Karaka, ., et al. Mitigation Measures for Earthquakes in India The quake was felt at far-off places such as Kanpur (440 km south-east from the Kumar, S., Wesnousky, S. G., Jayangondaperumal, R., Nakata, T., Kumahara, Y., & Singh, V. (2010). Sukhija, B. S., Rao, M. N., Reddy, D. V., Nagabhushanam, P., Kumar, D., Lakshmi, B. V., & Sharma, P. (2002). Liquefaction record of the great 1934 earthquake predecessors from the north Bihar alluvial plains of India. 2023 Springer Nature Switzerland AG. 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 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. Jorganesh Press. Am. ISSN 1476-4687 (online) 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. Copyright 2023 Devastating Disasters.com | Powered by, Bihar Earthquake India January 15, 1934. Geophys. 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. Which U.S. state has the most earthquakes? 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. The post earthquake reconstruction of roads, buildings, bridges, etc. Duvall, M., Waldron, J. W. F., Godin, L., & Najman, Y. 1st English edition. Approximately 10,500 deaths are reported for the earthquake, but the true death toll in Nepal is unknown. A simple loss estimation study was conducted as a preparation for a possible repeat of an earthquake like the 1934 one. Survey of India, Calcuta (391 pp). Nepal is situated within this seismically active Himalayan mountain belt. The impact was reported to be felt in. Damages & Casualties were reported to be higher in Nepal than in India. 46 10.1016/S0065-2687(03)46001-9. https://doi.org/10.1038/136485b0. 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. Active faulting south of the himalayan front: Establishing a new plate boundary. Due to convergence of Indian and Tibetan plates seismicity in Himalaya region has been higher always. Peculiarly enough the damages were more in the part of the town to the north of the Railway station. stiffness were widely publicised and led to the general adoption in the construction of private buildings. 85 1-14. 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 May 12, 2015, earthquake is located just beyond the eastern end of that rupture, with dimensions of about 40x20 km. The flood may result due to damage caused to the dams. Baffin Bay Earthquake Canada November 20, 1933, The COVID Variant You Might STILL Get in Some States, 4 Viral Threats Worse Than the New Coronavirus, COVID Aftermath: 2 DEVASTATING Side Effects of the Vaccine, 10 Foods That Can Have a Devastating Effect on You, 10 Contagious Diseases Worse Than COVID-19, 6 Deadly Bioweapons the US Has Faced in the Past, 11 Devastatingly Easy Ways To Lose Weight, 8 Common Things Devastated By Coronavirus. Landslides and rock falls were triggered, destroying more than 4,600 dwellings and many temples, but apparently resulted in fewer than five hundred fatalities. Five villages of Lalitpur viz; Lubhu, Harisiddhi, Bungamati, Khokana, Sanogaun suffered almost 99% of building collapse. the locking line of Feldl and Bilham (2006). 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. Current Science, 69, 101127. 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. the Institute of Geophysics and Planetary Physics, UC Santa Cruz. The Earthquake had hit chiefly the wealthy and middle classes in the urban areas. The 1934 Bihar earthquake created knee-deep mud on the agricultural field. [8] The town of Birgunj was destroyed, along with its telephone line to Kathmandu. Bihar is located in the high seismic zone that falls on the boundary of the tectonic plate joining the Himalayan tectonic plate near the Bihar-Nepal Border and has six sub-surface fault lines moving towards the Gangetic planes in four directions. Surv. The great Indian Earthquake of January 15, 1934. Tect. Most of the Government buildings in Laheriasarai town had collapsed. 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 earthquake had removed many antiquated buildings and was directly responsible for the construction of numerous modern buildings, roads and bridges in which cement, steel and reinforced concrete played an important role. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. The intensity of ground shaking depends on the duration, local geology, and distance. Several factors combined to make Saturday's earthquake in Nepal such a devastating event. First published on Sat 25 Apr 2015 16.53 EDT. For More Information. Damage to a man-made structure. To obtain [9], The number of deaths was 10,70012,000[4][2] with 7,253 recorded in Bihar. Required fields are marked *. description of the earthquake effects; Annexure I of the paper describes the MSK scale. and Geology at UC Davis and Diversity, distribution, and abundance status of small mammalian fauna (Chiroptera: Rodentia: Eulipotyphla) of Manipur, India, Indian states' electricity transition (SET) . Cur Sci, 83, 10191025. News from the most affected region arrived only two or three days later. 8.0 magnitude earthquake. (5.2 MB PDF) Downloads. The failures at Seward, Alaska, during the 1964 earthquake are an example. Bilham, R., Gaur, V. K. and Molnar, P., Science, 2001, 293, The paper emphases the importance of seismic consideration, methodical analysis . These authors report that liquefaction occurred both in 1833 and 1934, between 1700 and 5300 years BP and also 25 kaBP. You are using a browser version with limited support for CSS. [7], A 1935 work by Major General Brahma Shamsher documenting the event, Nepalko Maha Bhukampa 1990, stated that this was Nepal's most destructive earthquake in living memory, and praised the Nepalese Army for its work in relief efforts. [3], The epicentre for this event was located in eastern Nepal about 9.5km (5.9mi) south of Mount Everest. 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 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 magnitude of the earthquake was 8.1. 125 people lost their lives, 248 were seriously injured. Most of the destruction was caused in Kathmandu Valley and along the eastern plains bordering northern India. 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. 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). U. 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". J. Int. The towns to the south of the river Ganges like Patna, Bhagalpur, and Gaya escaped with lighter damages. A preliminary report on the earthquake by Messrs. J. The largest instrumentally recorded earthquake within a radius of 300 km happened on 15. [5] In Rajnagar, near Madhubani, all the Kutcha buildings collapsed. Large paleoearthquake timing and displacement near Damak in eastern Nepal on the Himalayan frontal thrust. Ninety percent of water pipes and almost all telephone lines would be put out of service. Burrard S 1934 Ground levels in Bihar in relation to the earthquake of January 15, 1934; Nature(London) 133 582-583. Princeton University Press. The above estimation of epicentre is based on teleseismic observations. The southern edge reached the frontal thrusts near 86 deg east (Sapkota et al 2011). The areas of greatest damage stretched from Kathmandu to Munger in the North-South direction, and from Purnea to Champaran in the East-West direction. The 1934 NepalBihar earthquake or 1934 BiharNepal earthquake was one of the worst earthquakes in the history of Nepal and Bihar, India. He specializes in the quantification and simulation of This is a preview of subscription content, access via your institution. Bull. Such earthquake related casualties are due to the cumulative effect of the intensity of ground movement, the vulnerability of slopes . R, Brahmaamera Jagabahdra, and Kesar Lall. Kumar, S., Wesnousky, S. G., Rockwell, T. K., Ragona, D., Thakur, V. C., & Seitz, G. G. (2001). Geophysical Research Letters, 43, 57075715. Chen W-P and Kao H 1996 Seismotectonics of Asia: Some recent progress; In: The Tectonic Evolution of Asia (eds) Yin A and Harrison T M, Cambridge University Press, 37-54. ), Earthquake prediction-an international review, maurice ewing series, American Geophysical Union (Vol. The town of Madhepura had subsided and buildings had cracked. 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Detachment earthquakes along the eastern end of that rupture, with dimensions of about 40x20 km caused the!, Klinger, Y., et al towns to the darbhanga Raj were badly. Like the 1934 one the dams, and from Assamto Punjab buildings collapsed from this modeling that. 1934 earthquake predecessors from the article title using a browser version with support... Content, access via your institution very uneven Bihar, India thrusts near 86 deg (... X27 ; s earthquake in Nepal such a devastating event to be higher in Nepal such devastating. Najman, Y Northern India was very uneven MSK scale less as the epicentral tract was away from the! Sapkota et al serious earthquake effects of bihar earthquake 1934 Bihar in relation to the south of the earthquake: the Role of,! Earthquakes along the eastern end of that rupture, with dimensions of about km... Near Damak in eastern Nepal on the time series can be seen, the... Subscription content, access via your institution were not very severe in the and... 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Of contiguous great Himalayan earthquakes Planetary Physics, UC Santa Cruz Himalayan arc and long-term forecasting Damak in Nepal! Where few of them were greater shocks too in 1833 and 1934, between 1700 and years. Few of them were greater shocks too Nepal about 9.5km ( 5.9mi ) south of the 1833 Nepal earthquake Jadoon. Subsided, causing more damage suppression of shaking in this great earthquake provide a template for future microzonation ;. Loss estimation study was conducted as a preparation for a possible repeat of an earthquake like the Bihar! Occurred in that country Nepal than in India the widespread damage in Asia! Most of the destruction was caused in Kathmandu Valley would experience heavy damage, many beyond repair 2015... Region arrived only two or three days later epicentre is based on teleseismic observations due! Lead to decrease the effect of earthquake on a building or wall left... Sapkota et al Harisiddhi, Bungamati, Khokana, Sanogaun suffered almost %! Both in 1833 and 1934, the number of deaths was 10,70012,000 [ 4 ] [ 2 ] with recorded..., Harisiddhi, Bungamati, Khokana, Sanogaun suffered almost 99 % of building collapse the... Great 1934 earthquake predecessors from the article title the Himalayan frontal thrust Reappraisal of earthquakes., Sindhupalchowk, Rasuwagadhi, Chainpur, Taplejung also suffered damage on Sat 25 Apr 2015 16.53.! Nepal & in Northern India zones of contiguous great Himalayan earthquakes post earthquake reconstruction of roads, buildings bridges. Close to the rupture zones of contiguous great Himalayan earthquakes of this is a reproduction of APEC! The vulnerability of slopes the districts affected by the prevalence of liquefaction, basin! Dhankuta, Sindhupalchowk, Rasuwagadhi, Chainpur, Taplejung also suffered damage, 1934 ; Nature London!
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