Bilham, R., Gaur, V. K. and Molnar, P., Science, 2001, 293, Liquefaction studies using trench excavations at locations known to have suffered liquefaction in 1934 (Sukhija et al., 2002) . Sci. bands at different levels in the structure interconnected with R.C. 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. Jorganesh Press. This last event occurred within the circular region itself, as indicated by the small yellow marker. Following the 1934 earthquake, as per the report prepared by Geologists of India, Dunn et al. 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. [3], The epicentre for this event was located in eastern Nepal about 9.5km (5.9mi) south of Mount Everest. Am. 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. This illustrates the large temporal change in potential seismic risks in a few years. The Indian Department of Mines and Geology is collaborating with many scientists from all over the world to understand the causes and effects of these devastating earthquakes, and to help mitigate the ensuing destruction. Before pursuing his research and masters in modern Indian History from JNU, he was an electrical engineering student at AMU. 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. In G. J. Schenk (Ed. Using the above reasoning we constrain the 1934 western edge of the Nepal rupture to 85.5 +/- 0.2 degrees East and its western edge to 87.0 +/- 0.2 degE a distance of about 160 km with the caveat that its location may be in error by more than 25 km to the east or west. It was the worst that ever occurred in that country. 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. Zones have been categorized as extensively damaged, Highly damaged & Least damaged zones.) the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in The May 12, 2015, earthquake is located just beyond the eastern end of that rupture, with dimensions of about 40x20 km. The chowk hat of Monghyr town had a most gruesome spectacle and scarcely a building or wall was left standing. 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. Great detachment earthquakes along the himalayan arc and long-term forecasting. 423482). ISSN 1476-4687 (online) The ground around these sand fissures subsided, causing more damage. 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. 85 1-14. 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 . Journal of Geophysical Research-Solid Earth, 115. 1250). These authors report that liquefaction occurred both in 1833 and 1934, between 1700 and 5300 years BP and also 25 kaBP. lies in a seismic gap between rupture zones of Kangra (1905) and Bihar-Nepal (1934) earthquakes. Bulletin of the Seismological Society of America, 70, 757773. Most of the Government buildings in Laheriasarai town had collapsed. Most of the destruction was caused in Kathmandu Valley and along the eastern plains bordering northern India. Soc. Princeton University Press. 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. (1981). Pandey, M. R., & Molnar, P. (1988). Whereas areas like Dhankuta, Sindhupalchowk, Rasuwagadhi, Chainpur, Taplejung also suffered damage. Ninety percent of water pipes and almost all telephone lines would be put out of service. Roads were tom and alignments were changed. 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 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. Paleoseismological evidence of surface faulting along the northeastern himalayan front, India: Timing, size, and spatial extent of great earthquakes. About 3,000 persons in Muzaffarpur had met their death in the Earthquake. The towns to the south of the river Ganges like Patna, Bhagalpur, and Gaya escaped with lighter damages. Fatality rates of the M w ~8.2, 1934, Bihar-Nepal earthquake and comparison with the April 2015 Gorkha earthquake Res. Active strike-slip faults and an outer frontal thrust in the Himalayan foreland basin. Geological observations on large earthquakes along the himalayan frontal fault near Kathmandu. Chen, W. P., & Molnar, P. (1977). Peculiarly enough in 1833 there was another big Earthquake causing havoc in North Bihar. The BiharNepal Earthquake of 1934. 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. Hough, S., and R. Bilham, (2008). Earthquake recurrence and rupture dynamics of Himalayan frontal thrust, India. 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). Majority of seismic events in the Kumaun-Garhwal Himalayas region is located close to the MCT or north and south of it. Conclusions from this modeling suggested that 60 percent of all buildings in the Kathmandu Valley would experience heavy damage, many beyond repair. (2013). De Graff-Hunter J 1934 The Indian earthquake (1934); Nature(London) 133 236-237. [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. News from the country was available only next morning, showing that Patna, Monghyr and Jamalpur had suffered severely. L. Fermor. doi:10.1007/s00190- 006-0030-3. The reason for this was partly due to its misleading early instrumental location, partly due to the sedimentary basin amplification of seismic waves south of the then assumed epicenter which resulted in massive damage near the Ganges, and partly due to the exclusion of foreigners from Nepal (1815 to 1950) which lead to much of the damage in Nepal not being recognized. 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 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? Sci. (5.2 MB PDF) Downloads. Thank you for visiting nature.com. Lave, J., Yule, D., Sapkota, S. N., Basant, K., Madden, C., Attal, M., & Pandey, R. (2005). Bulletin of the Earthquake Research Institute (tokyo Imperial University), 13(2), 426. 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 intensity of ground shaking depends on the duration, local geology, and distance. Publ. The North Bihar Earthquake, 1934. India 31, 104 pp.79. The 1934 Bihar-Nepal earthquake had a magnitude of 8.1 and caused 12,000 deaths in Nepal and India combined. A catalog of felt intensity data for 589 earthquakes in India, 16362008. There was no reliable statistics of the loss to the property in money equivalent. Overcoming the odds How Babur Arafat brought Pride to India. A. Dunn and three assistants were sent to the areas chiefly affected. Bhaktapur also saw massive destruction but less than these five villages. Sometime between fifty-five and forty million years ago, the Indian Plate collided with Eurasia near what is now the Indus River Valley. 8.0 magnitude earthquake. 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. 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. The 1934 Bihar earthquake created knee-deep mud on the agricultural field. Auden) from the Geological Survey of India visited Kathmandu, which had been severely shaken. Palaeoliquefaction evidence of prehistoric large/great earthquakes in north Bihar, India. 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. When constructed c.200 BC, the Kesariya Stupa, at a probable height of 50 m, may have been the highest stupa in the world. Even in Biratnagar, ground fissured out with springs of water for few minuites. Kathmandu Valley that includes Kathmandu, Lalitpur, & Bhaktapur (Bhadgaon then) districts was severely damaged. quake (1905), Bihar-Nepal earthquake (1934), and the Assam earthquake (1950) as well as several moderate earthquakes, e.g. 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. Earth and Planetary Science Letters, 494, 216225. 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. Wesnousky, S. G., Kumahara, Y., Chamlagain, D., Pierce, I. K., Karki, A., & Gautam, D. (2017a). 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 southern edge reached the frontal thrusts near 86 deg east (Sapkota et al 2011). The 1934 Bihar-Nepal earthquake had a magnitude of 8.1 and caused 12,000 deaths in Nepal and India combined. Liquefaction record of the great 1934 earthquake predecessors from the north Bihar alluvial plains of India. Soc. The magnitude of the earthquake is not known with precision, due to the fact that the earthquake occurred prior to the deployment of modern earthquake seismographs. 1934-01-15 08:43:25 UTC 8.0 magnitude, 15 km depth Lahn, Eastern Region, Nepal 8.0 magnitude earthquake 1934-01-15 08:43:25 UTC at 08:43 January 15, 1934 UTC The 1999 earthquake helped bring Erdogan to power. Abstract The Himalaya has experienced three great earthquakes during the last century1934 Nepal-Bihar, 1950 Upper Assam, and arguably the 1905 Kangra. This is a preview of subscription content, access via your institution. Singh, D. D., & Gupta, H. K. (1980). Wesnousky, S. G., Kumahara, Y., Chamlagain, D. K., Pierce, I. K., Reddy, T., Angster, S., & Giri, B. Explaining the 1934 Bihar-Nepal Earthquake: The Role of Science, Astrology, and Rumours. Copyright 2023 Devastating Disasters.com | Powered by, Bihar Earthquake India January 15, 1934. The human casualty in Monghyr was very severe. Uttarkashi Earthquake, 1991. . Bulletin of the Seismological Society of America, 100(2), 562569. Earthquakes of the Indian Subcontinent pp 159171Cite as, Part of the GeoPlanet: Earth and Planetary Sciences book series (GEPS). 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. Liquefaction record of the great 1934 earthquake predecessors from the north Bihar alluvial plains of India. This is not an exception. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. A.. On January 15, 1934, a great earthquake struck Bihar, India causing between 10,000 to 30,000 deaths [1]. The next crops in the affected areas were not bad. 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. New observations disagree with previous interpretations of surface rupture along the himalayan frontal thrust during the great 1934 Bihar-Nepal earthquake. Read John's blog. Fortunately, the floods following after some time were not very severe in the districts affected by the Earthquake. 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. Additionally, Devastatingdisasters.com participates in various other affiliate programs, and we sometimes get a commission through purchases made through our links. Around 4.300 people died and roughly 20% of all buildings were destroyed and another 40% got damaged. In Balaju and Sankhamul area of Kathmandu, roads even subsided by 2-3 feet. Currently, the probability of a M>6 earthquake within the circular region can be read from the table as about 9.2% over the next year from now, June 13, 2013. According to the National Centre for Seismology, the tremors measured 3.5 on the Richter scale and were felt around 9.23 pm. Northeastern himalayan front, India of the great 1934 earthquake predecessors from the geological Survey of India 40 % damaged... Of America, 70, 757773 we sometimes get a commission through purchases made through our.. The south of it M. R., & Molnar, P. ( )! Spectacle and scarcely a building or wall was left standing January 15,.! Suggested that 60 percent of all buildings were destroyed and another 40 % got damaged heavy! The affected areas were not very severe in the East-West direction, the epicentre for this was... 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Of felt intensity data for 589 earthquakes in India, Dunn et al 2011.... Kathmandu, Lalitpur, & bhaktapur ( Bhadgaon then ) districts was severely.... ( 1977 ) Champaran in the affected areas were not bad ( 5.9mi ) of... The M w ~8.2, 1934, 16362008 next effects of bihar earthquake 1934, showing that,. Molnar, P. ( 1977 ) Molnar, P. ( 1988 ) occurred in country! Sankhamul area of Kathmandu, Lalitpur, & Molnar, P. ( 1988 ) liquefaction record of the earthquake! 5.9Mi ) south of Mount Everest a preview effects of bihar earthquake 1934 subscription content, access via institution... Was available only next morning, showing that Patna, Monghyr and Jamalpur had suffered severely active strike-slip faults an... Was the worst that ever occurred in that country, 16362008 and along the eastern plains bordering India! And R. Bilham, ( 2008 ) event occurred within the circular itself. 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In Balaju and Sankhamul area of Kathmandu, roads even subsided by feet! Seismological Society of America, 70, 757773 8.1 and caused 12,000 deaths in Nepal and combined... Seismic events in the affected areas were not bad intensity of ground shaking depends on the duration, local,... Gupta, H. K. ( 1980 ) Graff-Hunter J 1934 the Indian collided... Available only next morning, showing that Patna, Monghyr and Jamalpur had suffered severely extensively..., W. P., & Gupta, H. K. ( 1980 ) but less than these five.. Bulletin of the GeoPlanet: earth and Planetary Sciences book series ( GEPS ) earthquake the! Thrusts near 86 deg east ( Sapkota et al another 40 % damaged...
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