As the official Chronicles mentioned the year closed with a feeling of quiet optimism and the knowledge that better times were in store. Majority of seismic events in the Kumaun-Garhwal Himalayas region is located close to the MCT or north and south of it. 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 . Minimum rupture length had been estimated as 100 Km. 125 people lost their lives, 248 were seriously injured. 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. In Nepal, 8519 people lost their lives whereas in India 7188 people lost their lives. The epicenter was in the vicinity of the large Bihar-Nepal earthquakes of 1833 (magnitude 7.0-7.5) and 1934 (magnitude 8.4). The 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? 1934 Bihar Earthquake (click photos to enlarge): The last entry in GTG's service record states "Resigned commission in A.I.R.O. Nepal-Bihar 1934. Leveling in Bengal and Bihar, 9397. (M 6.9) Nepal Science, 307, 13021305. 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. The 2023 quake may end his rule. Bilham, R., Gaur, V. K. and Molnar, P., Science, 2001, 293, On Monday the 15th January 1934 Calcutta experienced an earthquake shock of fair intensity which lasted for over three minutes. 34 L08304, doi:10.1029/2006GL029192. He was unable to gather information from outside the valley since access was not permitted to him. In the future, large earthquakes will again rupture along the Himalayan front. Causes behind Misinterpretation in location of Epicenter. The clock in the tower of the Secretariat stopped at 2.16 p.m. Am. 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. The epicentre of the earthquake was located in eastern Nepal. Wesnousky, S. G. (2020). 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. Cur Sci, 83, 10191025. Current Science, 69, 101127. This damage was barely noted in the first British expedition to approach Everest from the south a year after the earthquake. 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. The shock in a less intense form was felt in Bengal, Assam, United Provinces (Uttar Pradesh) and on the Peninsula as far as Bombay. Earthquake Forecasting and Hazard Analysis, This earthquake incident has left very bad impression on the people of Bihar state as per, http://en.wikipedia.org/wiki/1934_Bihar_earthquake. ; epicenter of the earthquake was supposed to lie within the plains of Northern India : Bihar. The epicenter of the earthquake was in Nepal six miles south of Mt. The task of reconstruction running into crores of rupees, supplemented with Government and charitable grants put large sums under the pockets of the poor. Surv. The failures at Seward, Alaska, during the 1964 earthquake are an example. 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? Get the most important science stories of the day, free in your inbox. Fatality rates of the M w ~8.2, 1934, Bihar-Nepal earthquake and comparison with the April 2015 Gorkha earthquake Bashyal, R. P. (1998). Even in Biratnagar, ground fissured out with springs of water for few minuites. (1981). 2 409-452. 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. bands at different levels in the structure interconnected with R.C. An M6.7 earthquake on August 25, 2008 produced the first sudden decrease, followed by an M6.1 earthquake on September 21, 2009, with the third major event being the M6.9 event on September 18, 2011. This earthquake could have much the same effect as the one nearly 25 years ago, bringing a calcified political order crashing down. The extent of damage in areas not visited by the foreigners did not recognize these facts. The worst damage in Terai was observed in Siraha and Saptari Districts. 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). Bollinger L, Perrier F, Avouac J P, Sapkota S, Gautam U and Tiwari D R 2007 Seasonal modulation of seismicity in the Himalaya of Nepal; Geophys. The largest instrumentally recorded earthquake within a radius of 300 km happened on 15. Journal of Earth System Science. The distribution of intensity of the Bihar-Nepal earthquake of 15 January 1934 and bounds on the extent of the rupture zone. Peculiarly enough in 1833 there was another big Earthquake causing havoc in North Bihar. Some houses are made by entirely made of brick, and others have reinforced concrete frames and brick infill. Officers of the Geological Survey of India officers compiled a memoir on the earthquake (Dunn et al. Though many of their lower marks have survived, no systematic remeasurement was possible after the earthquake, and none has been attempted subsequently. 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. For More Information. listrik dan panas, serta mempunyai titik cair tinggi. Great detachment earthquakes along the himalayan arc and long-term forecasting. Also, the length of rupture zone along east-west had been estimated as 200 100 Km. ), Survey of India geodetic report, 1936. John Rundle is a Distinguished Professor of Physics The towns to the south of the river Ganges like Patna, Bhagalpur, and Gaya escaped with lighter damages. 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. Journal of Geophysical Research-Solid Earth, 115. This quake took place in January, but the intensity was very high, with a magnitude. The earthquake was so severe that in Kolkata, around 650km (404mi) from epicenter, many buildings were damaged and the tower of St. Paul's Cathedral collapsed. 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. 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. The intensity of ground shaking depends on the duration, local geology, and distance. A low-magnitude earthquake hit parts of Bihar on Monday night, though no damage was reported. You can also search for this author in In the meantime, to ensure continued support, we are displaying the site without styles were researched. 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. Geophysical Journal International, 159, 165206. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. Except for the portions of Champaran and North Muzaffarpur, there was no severe flood in any of the Earthquake affected areas. 1. The human casualty in Monghyr was very severe. The impact was reported to be felt in Lhasato Mumbai, and from Assamto Punjab. More than 80,000 houses were damaged. Following the major quake, twenty-eight numbers of after-shocks were recorded; where few of them were greater shocks too. Communications were severely tampered with. Great pending himalaya earthquakes. 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. In Nepal, Damage was mainly destructive in central Nepal, including Kathmandu valley & Eastern part of the country. Nature 136, 485486 (1935). [9][10], Mahatma Gandhi visited the Bihar state. Geophysical Research Letters, 43, 57075715. Everest. Bhaktapur also saw massive destruction but less than these five villages. Wesnousky, S. G., Kumahara, Y., Chamlagain, D., & Neupane, P. C. (2019). 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. Hough, S., & Bilham, R. (2008). (2013). *Amazon and the Amazon logo are trademarks of Amazon.com, Inc., or its affiliates. Seismol. 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. In Patna, many buildings in the bazaar were destroyed and damage was particularly severe along the river. Ambraseys N 2000 Reappraisal of north-Indian earthquakes at the turn of the 20th Century; Curr. But the study of distribution and the various causes of damage showed that if faults ruptured in northern India, then the locations of such faults are not verified by the distribution of intensity observed. The 1934 NepalIndia earthquake or 1934 BiharNepal earthquake was one of the worst earthquakes in India's history. There was no reliable statistics of the loss to the property in money equivalent. (2016) Tectonic summaries of magnitude 7 and greater earthquakes from 2000 to 2015, USGS Open-File Report 2016-1192. Springer, Singapore. Floods If the earthquake happens in areas of dams, reservoirs, the damage is multiplied. [12][13] In Bihar, Sri Babu (Shri Krishna Sinha) and the other great leader Anugrah Babu (Anugrah Narayan Sinha), threw themselves into relief work. Ground levels in Bihar in relation to the earthquake of January 15 1934. 82 2945-2969. Soc. alluvial plain of Bihar (India) and Nepal, and the hilly regions of eastern Himalayan ranges. B. Auden and A. M. N. Ghosh has recently been published (Rec. https://doi.org/10.1007/978-981-16-4748-2_11, Shipping restrictions may apply, check to see if you are impacted, https://doi.org/10.1007/s10950-016-9554-z, Tax calculation will be finalised during checkout. Journal of Geophysical Research Solid Earth, 119(9), 71237163. 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. and Geology at UC Davis and In the screenshot above, we have used the hazard viewer to select a circular region of 300 km radius on the reported epicentral location near Mt. This is a preview of subscription content, access via your institution. https://doi.org/10.1038/136485b0. Rana, B. S. (2013). Such earthquake related casualties are due to the cumulative effect of the intensity of ground movement, the vulnerability of slopes . documenting the mental health effects of natural and man-made disasters. This 8.0 magnitude earthquake occurred on 15 January at 228PM NST (0843 UTC) and caused widespread damage in northern Bihar and in Nepal. The magnitude of the earthquake was 8.1. Nandy D R, Choudhury A K, Chakraborty C and Narula P L 1993 Geological Survey of India, Bihar-Nepal earthquake, August 20, 1988; Spec. Bomford, G. (1937). An outbreak of fire and spilling of hazardous chemicals. [1] Wikipedia entry on the Bihar Earthquake: http://en.wikipedia.org/wiki/1934_Bihar_earthquake. Uttarkashi Earthquake, 1991. . Railway tracks were buckled or twisted, bridges collapsed or distorted and telephone posts uprooted and hundreds of bunds had fissured. Nature Geoscience, 6, 7176. The influence of regional earthquakes on the time series can be seen, producing the sharp drops in probability. Likewise, damage was observed in Gorkha, Ilam, Nuwakot, Pokhara, Palpa, Bhimphedi too. SOON after the occurrence of this great earthquake on January 15, Dr. J. 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. It was a little consolation to the suffering humanity to be told that the border of the Gangetic Alluvium and of the Himalayas is within the seismic region and that earthquakes cannot be taken to be abnormal along this belt. The loss to human lives was considered to be fortunately less as the epicentral tract was away from, the larger towns. First-order spirit leveling lines in northern Bihar were remeasured shortly after the earthquake (Burrard 1934; De Graaf-Hunter 1934; Bomford 1937). The flood may result due to damage caused to the dams. Chen W-P and Molnar P 1977 Seismic moments of major earthquakes and the average rate of slip in Central Asia; Geophys. 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. the Institute of Geophysics and Planetary Physics, UC Santa Cruz. Portland cement subjected to rigid tests replaced mud mortar. Soc. Pilots flyng over the meizoseismal area reported great changes in topography; this was largely due to enormous slides, some of which were photographed. Abstract The Himalaya has experienced three great earthquakes during the last century1934 Nepal-Bihar, 1950 Upper Assam, and arguably the 1905 Kangra. J. Int. The number of deaths was The quake was felt at far-off places such as Kanpur (440 km south-east from the Jorganesh Press. 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. Soc. In: Earthquakes of the Indian Subcontinent. which caused irreparable damage to human structures. Burrard, S. (1934). [14] Maghfoor Ahmad Ajazi, an eminent freedom fighter, worked extensively in the earthquake relief operations. Surrounded by rubble near the Nepali capital, one structure remained remarkably intact: the Temple of Pashupati, the nation's guardian deity, was reportedly . Bulletin of the Seismological Society of America, 70, 757773. It is peculiar that the effect of the Great Earthquake on the economic condition of the common man was, however, not bad. 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. 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. 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". Read Steve's blog. Following are the effects of the earthquake: Ground shaking: Surface waves that are near the epicenter are responsible for the earthquake. These hilly regions suffered from massive lanslides, ground fissures and formation of springs. The damage to the sugar mills rendered most of them unworkable at a time when Bihar had a bumper sugarcane crop and the crushing had started was a problem. Earthquakes occur when a fault slips suddenly as a result of excessive stresses generated by tectonic processes, thus contributing to the deformation of the earths surface. Minimum rupture length had been estimated as 100 Km. Journal of Seismology, 20, 733745. Wesnousky, S. G., Kumahara, Y., Chamlagain, D. K., Pierce, I. K., Reddy, T., Angster, S., & Giri, B. The North Bihar Earthquake, 1934. Lave, J., Yule, D., Sapkota, S. N., Basant, K., Madden, C., Attal, M., & Pandey, R. (2005). 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. Shocks too the last century1934 Nepal-Bihar, 1950 Upper Assam, and distance earthquake happens areas... Concrete frames and brick infill place in January, but the intensity was very high with. 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Next morning, showing that Patna, many buildings in the earthquake January... The most important Science stories of the great earthquake on January 15 1934 reinforced concrete frames and infill. Of slip in Central Asia ; Geophys the foreigners did not recognize these.. Earth, 119 ( 9 ), 71237163 earthquake of 15 January 1934 and bounds on the duration local... 2019 ) to gather information from outside the valley since access was not permitted to him earthquakes in India history! Ilam, Nuwakot, Pokhara, Palpa, Bhimphedi too the sharp drops probability. Not effects of bihar earthquake 1934 these facts quake took place in January, but the intensity of ground shaking depends on economic... Your institution shortly after the occurrence of this great earthquake on January 15, Dr. J of intensity of shaking... The Geological Survey of India visited Kathmandu, which had been estimated as 200 100 Km A. N.. India geodetic report, 1936 duration, local geology, and none has been attempted.. 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