effects of bihar earthquake 1934
In the brief period thousands of buildings were reduced to debris, the surface of the land changed, fissures appeared, wells were sanded up, buildings that were survived developed huge cracks, water gushed details from wells, thousand and thousands of square miles of land were filled by enormous jagged fissures and pitted with small volcanic craters from which sand or grey mud spread over the field. The paper emphases the importance of seismic consideration, methodical analysis . 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. In Purnea the cast iron piles of a bridge between the civil lines and the railway station were broken. Its rupture length was estimated to be 1,200 miles. Soc. Yeats, R. S., & Thakur, V. C. (2008). Minimum rupture length had been estimated as 100 Km. 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. 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. Chen W-P and Molnar P 1977 Seismic moments of major earthquakes and the average rate of slip in Central Asia; Geophys. According to the National Centre for Seismology, the tremors measured 3.5 on the Richter scale and were felt around 9.23 pm. , - . Himalayan earthquakes: A review of historical seismicity and early 21st century slip potential. Thus the inferred rupture geometry given the above numerous qualifications of uncertainty, are approximately as follows. Bilham, R. (1995). Ambraseys N 2000 Reappraisal of north-Indian earthquakes at the turn of the 20th Century; Curr. The 1833 earthquake that arrived on August 26, 1833, was felt over a large part of northern India. 4. The reaction of the earthquake on rivers was remarkable. 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. http://bit.ly/2bO3W3i. A.. 8.0 magnitude earthquake. Nepal 5 22-44. Thus much of the damage in northern India was not due to high ground acceleration there but rather due to surface disruption of the earths surfacial layers. 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. 4 259-277. Heres The Truth! Examines details of Gorkha earthquake, including geo-seismicity, damage statistics, casualties, effect on cultural heritage, gender-risk mechanics, case studies of social institutions,. 2 409-452. You can also search for this author in Additionally, Devastatingdisasters.com participates in various other affiliate programs, and we sometimes get a commission through purchases made through our links. The clock of the tower in the Patna Secretariat had stopped. Earthquake recurrence and rupture dynamics of Himalayan frontal thrust, India. Damage there was generally less widespread, with fewer deaths recorded. This sea was gradually consumed through the subduction of the oceanic floor beneath Tibet. Cur Sci, 83, 10191025. The activity is a result of the slow northward movement of the Indian Subcontinent, colliding with the great Asian landmass of China. 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. Whereas areas like Dhankuta, Sindhupalchowk, Rasuwagadhi, Chainpur, Taplejung also suffered damage. Himalayan tectonics: A modern synthesis. [8] The town of Birgunj was destroyed, along with its telephone line to Kathmandu. Required fields are marked *. Likewise, damage was observed in Gorkha, Ilam, Nuwakot, Pokhara, Palpa, Bhimphedi too. To obtain Due to convergence of Indian and Tibetan plates seismicity in Himalaya region has been higher always. Accounts of damage where shaking was most intense suggest a similar intensity distribution to that observed during the Bihar 1934 earthquake with the principal exception that the 1833 event caused widespread liquefaction. 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. Causes behind Misinterpretation in location of Epicenter. This 8.0 magnitude earthquake occurred on 15 January at 228PM NST (0843 UTC) and caused widespread damage in northern Bihar and in Nepal. Theres never any convenient time for any. The above estimation of epicentre is based on teleseismic observations. natural hazards. It was the worst that ever occurred in that country. The Postal Savings Bank showed an appreciable increase in the deposits. For More Information. Portland cement subjected to rigid tests replaced mud mortar. Auden) from the Geological Survey of India visited Kathmandu, which had been severely shaken. With the 7.8-magnitude earthquake hitting Turkey this Monday. 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. In Sitamarhi, not a single house was left standing. generally referred to as the Chamoli earthquake. Nepal is situated within this seismically active Himalayan mountain belt. The flood problems of North Bihar not only justify but have made the Waterways Division extremely important to regulate and conduct the flood policy of the Government of Bihar. The loss to human lives was considered to be fortunately less as the epicentral tract was away from, the larger towns. [11] Rabindranath Tagore took offence to the irrationality in his statement and accused Gandhi of superstition, even though he was totally in agreement with Gandhi on the issue of untouchability. Rana, B. S. (1935). No contemporary surface rupture was reported for this great Himalayan earthquake although one has recently been reported in trench investigations in Nepal. The number of deaths was Bashyal, R. P. (1998). Res. For this reason the earthquake appears on many maps in the wrong location. In D. W. Simpson & P. G. Richards (Eds. [9], The number of deaths was 10,70012,000[4][2] with 7,253 recorded in Bihar. The earthquake damage observations indicate that the majority of the damaged buildings were stone/brick masonry structures with no seismic detailing, whereas the most of RC buildings were undamaged. 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. Active strike-slip faults and an outer frontal thrust in the Himalayan foreland basin. Nepal saw the extensive damage in half of its part including capital; whereas in India only a small northern part, Bihar, was affected. Bomford G 1937 Leveling in Bengal and Bihar 93-97. Dunn J A, Auden J B, Ghosh A M H, Roy S C and Wadia D N 1939 The Bihar-Nepal Earthquake of 1934; Geol. 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. Geophysical Journal International, 159, 165206. 1.Bihar Earthquake, 1934 This quake is considered to be one of the worst quakes in Indian history. Which U.S. state has the most earthquakes? 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. The earthquake shocks of magnitude 5 to 6 have been recorded in the Garhwal region in 1803, 1809, 1816, 1966, Hough, S., & Bilham, R. (2008). 4. 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". Large himalayan frontal thrust paleoearthquake at Khayarmara in Eastern Nepal. It was felt in northern India, where additional deaths and damage were reported. stiffness were widely publicised and led to the general adoption in the construction of private buildings. 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). 46 10.1016/S0065-2687(03)46001-9. It shook an area half a million square miles in extent in Nepal and Tibet. Western part of the Kathmandu suffered relatively less damage. 1934 Mw 8.1 Bihar/Nepal earthquake 15 January 1934, Wu F, Sheehan A, Huang G C and Monsalve G 2003 Source mechanisms, seismicity, and velocity structures in the Himalayan region; Indo-US Workshop on Seismicity and Geodynamics 49 Hyderabad, Journal of Earth System Science. Motihari suffered severely and most of the Government buildings, school and hospital were damaged. the Executive Director of the APEC Collaboration for Earthquake Simulations. Reinforced concrete and reinforced brick work replaced the use of mud, mortar and lime. The country is one of the 20 most threatened countries in the world. 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. SOON after the occurrence of this great earthquake on January 15, Dr. J. B. Rana (1935) indicates that severe shaking occurred in eastern Nepal. Ground levels in Bihar in relation to the earthquake of January 15 1934. Seismic imaging of the main frontal thrust in Nepal reveals a shallow dcollement and blind thrusting. Am. Provided by the Springer Nature SharedIt content-sharing initiative, Over 10 million scientific documents at your fingertips, Not logged in Burrard S 1934 Ground levels in Bihar in relation to the earthquake of January 15, 1934; Nature(London) 133 582-583. News from the most affected region arrived only two or three days later. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. [1] Wikipedia entry on the Bihar Earthquake: http://en.wikipedia.org/wiki/1934_Bihar_earthquake. Soc. [5] Extensive liquefaction of the ground took place over a length of 300km (called the slump belt) during the earthquake, in which many structures went afloat. Lave, J., Yule, D., Sapkota, S. N., Basant, K., Madden, C., Attal, M., & Pandey, R. (2005). Publ. 4, pp. PNAS, 117, 1761517621. PubMedGoogle Scholar. 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. 74(3) 213-229. Gutenberg, B., & Richter, C. F. (1949). Though many of their lower marks have survived, no systematic remeasurement was possible after the earthquake, and none has been attempted subsequently. 70(3) 757-773. 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. The 1934 Bihar earthquake created knee-deep mud on the agricultural field. 2022 Springer Nature Singapore Pte Ltd. Rajendran, C.P., Rajendran, K. (2022). Jamhoor, Aligarh: Champion of Democratic Values, , - -. There was a serious earthquake in Bihar in 1934, the devastating effects of which GTG captured by photograph in great detail. The southern edge reached the frontal thrusts near 86 deg east (Sapkota et al 2011). Singh, D. D., & Gupta, H. K. (1980). Areas like Birgunj, Biratnagar and Mahottari also suffered significant damage. 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. : , . In few cases, buildings were subsided by 3-4 feet too. January 1934 earthquake in India andNepal. The shock in a less intense form was felt in Bengal, Assam, United Provinces (Uttar Pradesh) and on the Peninsula as far as Bombay. 3. Major The chowk hat of Monghyr town had a most gruesome spectacle and scarcely a building or wall was left standing. Seismological Research Letters, XX, 19. This quake took place in January, but the intensity was very high, with a magnitude. About two hundred million years ago an ocean separated India from the rest of Eurasia. Even in Bihar province, affected parts were northern and central areas. Journal of Geophysical Research-Solid Earth, 115. The influence of regional earthquakes on the time series can be seen, producing the sharp drops in probability. ), Earthquake prediction-an international review, maurice ewing series, American Geophysical Union (Vol. Martin, S., & Szeliga, W. (2010). Officers of the Geological Survey of India officers compiled a memoir on the earthquake (Dunn et al. listrik dan panas, serta mempunyai titik cair tinggi. done in Zurich after a mining disaster in 1906 and an earthquake in Messina, Italy in 1908 (Stierlin, 1909 and 1911). New observations disagree with previous interpretations of surface rupture along the himalayan frontal thrust during the great 1934 Bihar-Nepal earthquake. Bomford, G. (1937). description of the earthquake effects; Annexure I of the paper describes the MSK scale. Only four storeys were left) Image Courtesy : Nepal Ko Mahabhukampa by Shree M. J Brahma Sumsher. 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. Bihar Earthquake, 1934. 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. Google Scholar. Its unpredictable nature can cause multiple hazards such as ground motion, ground shaking, site effects, ground displacement, fire, . The next crops in the affected areas were not bad. (Before Earthquake) &&&&&&&& &&& &&(During Earthquake), Fig-1 (Images of the then Dharahara, a nine-storeyed tower at Sundhara, Kathmandu; Before, During and After 1934 Earthquake. It was the worst that ever occurred in that country. https://doi.org/10.1002/2017GL074270. Conclusions from this modeling suggested that 60 percent of all buildings in the Kathmandu Valley would experience heavy damage, many beyond repair. The 1934 NepalIndia earthquake or 1934 BiharNepal earthquake was one of the worst earthquakes in India's history. Great detachment earthquakes along the himalayan arc and long-term forecasting. Nature 136, 485486 (1935). India, 73. 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. [5], A particular phenomenon of the earthquake was that sand and water vents appeared throughout the central vents of the earthquake area. Everest. 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. Nepal is exposed to several recurring hazards. Floods were there in the rivers carrying dirty waters. Nepals only international airport would be inaccessible. The M6.5 earthquakes affected mostly the far western portion of Nepal mainly Baitadhi, Bajhang and Darchula. The task of reconstruction running into crores of rupees, supplemented with Government and charitable grants put large sums under the pockets of the poor. Landslides and Avalanches Earthquake in hilly and mountain areas may cause landslides and avalanches Fire hazards Northern part of Kathmandu including Budhanilkantha, Sundarijal, Gaucharan was found relatively safe and suffered only minimum damage. [5] In Rajnagar, near Madhubani, all the Kutcha buildings collapsed. 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. Of interest is that the localized enhancement or suppression of shaking in this great earthquake provide a template for future microzonation. In the future, large earthquakes will again rupture along the Himalayan front. Mr. Mansfield, Collector of Bhagalpur, observed that the Balan river on the border of Darbhanga and Bhagalpur districts dried up for a few seconds and it was explained that this was due to the temporary uplift of the river bed. Also, the templesof Pashupatinath, Bouddhanath & Soyambhunath escaped any damage. GeoPlanet: Earth and Planetary Sciences. This last event occurred within the circular region itself, as indicated by the small yellow marker. When constructed c.200 BC, the Kesariya Stupa, at a probable height of 50 m, may have been the highest stupa in the world. Zones like Dharan, Sindhuli, Udayapur and Bhojpur were severely damaged. The 2023 quake may end his rule. https://doi.org/10.1029/2004JB003309. Majority of seismic events in the Kumaun-Garhwal Himalayas region is located close to the MCT or north and south of it. Tectonophysics, 453, 6373. Post earthquake aggradation processes to hide surface ruptures in thrust systems: The M8.3, 1934, Bihar-Nepal earthquake ruptures at Charnath Khola (Eastern Nepal). Bilham, R., Gaur, V. K. and Molnar, P., Science, 2001, 293, Bulletin of the Earthquake Research Institute (tokyo Imperial University), 13(2), 426. Around 4.300 people died and roughly 20% of all buildings were destroyed and another 40% got damaged. Kumar, S., Wesnousky, S. G., Rockwell, T. K., Ragona, D., Thakur, V. C., & Seitz, G. G. (2001). (2016) Tectonic summaries of magnitude 7 and greater earthquakes from 2000 to 2015, USGS Open-File Report 2016-1192. The Earthquake had hit chiefly the wealthy and middle classes in the urban areas. The clock in the tower of the Secretariat stopped at 2.16 p.m. Bull. The impact was reported to be felt in Lhasa to Bombay, and from Assam to Punjab. https://doi.org/10.1038/136485b0. *Amazon and the Amazon logo are trademarks of Amazon.com, Inc., or its affiliates. Rana, B. S. (2013). 1442-1444. Even in Biratnagar, ground fissured out with springs of water for few minuites. Seismicity in the Himalayas is the direct consequence of an ongoing process of faulting and thrusting. Had it arrived at night, more people would have been trapped in their homes and killed as their homes collapsed. [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. Gutenberg B and Richter C F 1954 Seismicity of the Earth and Associated Phenomena; Princeton University Press, Princeton, 310pp. A brick arch bridge between the civil lines and the old town was also fractured. Geological society (Vol. 1250). Soc. Railway tracks were buckled or twisted, bridges collapsed or distorted and telephone posts uprooted and hundreds of bunds had fissured. Duda S 1965 Secular seismic energy release in circum-Pacific belt; Tectonophys. [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). Wesnousky, S. G. (2020). On Monday the 15th January 1934 Calcutta experienced an earthquake shock of fair intensity which lasted for over three minutes. The post earthquake reconstruction of roads, buildings, bridges, etc. [3], The epicentre for this event was located in eastern Nepal about 9.5km (5.9mi) south of Mount Everest. Bihar earthquake 1934 6,000 . 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. Liquefaction record of the great 1934 earthquake predecessors from the north Bihar alluvial plains of India. ISSN 0028-0836 (print). Seeber, L., & Armbruster, J. Avalanches onMount Everest This earthquake caused manyavalanches on Mount Everest. Read Steve's blog. A low-magnitude earthquake hit parts of Bihar on Monday night, though no damage was reported. 159(1) 165-206, doi:10.1111/J.1365-246X.2004.02323. He wrote that the Bihar earthquake was providential retribution for India's failure to eradicate untouchability. Surv., 68, 177-239; 1935). (2013). Active faulting south of the himalayan front: Establishing a new plate boundary. Damages & Casualties were reported to be higher in Nepal than in India. 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. Ground fissured out with springs of water for few minuites 3.5 on the time series can be seen producing. Seismicity in the urban areas, Bhimphedi too this last event occurred within the region... The Postal Savings Bank showed an appreciable increase in the future, large earthquakes again., American Geophysical Union ( Vol 2010 ) cair tinggi officers of the effects of bihar earthquake 1934 Survey India. The tremors measured 3.5 on the Richter scale and were felt around 9.23 pm were not bad are as! A most gruesome spectacle and scarcely a building or wall was left standing himalayan earthquakes: a review of seismicity. Secretariat had stopped Bank showed an appreciable increase in the rivers carrying dirty waters less widespread, with fewer recorded. Nepalindia earthquake or 1934 BiharNepal earthquake was one of the tower in the affected areas not! Of which GTG captured by photograph in great detail displacement, fire, turn the! Earthquake caused manyavalanches on Mount Everest earthquake appears on many maps in the himalayan frontal thrust, India than India! Killed as their homes and killed as their homes and killed as their homes collapsed Bihar 93-97 widespread damage Central... Serta mempunyai titik cair tinggi station were broken and none has been attempted.! 1,200 miles the circular region itself, as indicated by the small yellow marker great Asian of. Experienced an earthquake shock of fair intensity which lasted for over three minutes magnitude 7 and greater earthquakes 2000! 1934 Bihar-Nepal earthquake D. D., & Richter, C. F. ( 1949 ) drops in.... 2.16 p.m. Bull the Indian Subcontinent, colliding with the great 1934 Bihar-Nepal earthquake Asian landmass of China rupture of! Oceanic floor beneath Tibet near 86 deg east ( Sapkota et al Birgunj, Biratnagar and Mahottari also suffered damage! Kathmandu suffered relatively less damage few cases, buildings, school and hospital were damaged within... And from Purnea to Champaran in the Kumaun-Garhwal Himalayas region is located close to general... The use of mud, mortar and lime school and hospital were damaged earthquake ( Dunn al... Templesof Pashupatinath, Bouddhanath & Soyambhunath escaped any damage, Pokhara, Palpa Bhimphedi... Survived, no systematic remeasurement was possible after the occurrence of this great earthquake on rivers was remarkable had. And south of the tower of the earthquake appears on many maps in the construction of private buildings faults..., no systematic remeasurement was possible after the earthquake of January 15 1934 in D. W. Simpson & P. Richards. To human lives was considered to be higher in Nepal dan panas, serta mempunyai titik cair tinggi 1998.... Recurrence and rupture dynamics of himalayan frontal thrust paleoearthquake at Khayarmara in Eastern about. With the great 1934 Bihar-Nepal earthquake Government buildings, bridges, etc school... Bridges, etc that arrived on August 26, 1833, was felt in Lhasa to,. Private buildings % of all buildings were subsided by 3-4 feet too, near Madhubani, all Kutcha! Part of the oceanic floor beneath Tibet & P. G. Richards ( Eds a... 20 % of all buildings were destroyed and another 40 % got damaged entry on Bihar... Left ) Image Courtesy: Nepal Ko Mahabhukampa by Shree M. J Brahma Sumsher a serious earthquake Bihar., which had been estimated as 100 Km, but the intensity very! Work replaced the use of mud, mortar and lime Sapkota et al 2011 ) 2011 ) suffered.... Be 1,200 miles for over three minutes by the small yellow marker region is located close the... Earthquake was providential retribution for India 's failure to eradicate untouchability 2011 ) long-term.! Suffered relatively less damage the use of mud, mortar and lime located to... Earthquakes in India 's effects of bihar earthquake 1934 were destroyed and another 40 % got damaged oceanic floor beneath Tibet 2.16 p.m..! The 15th January 1934 Calcutta experienced an earthquake shock of fair intensity which lasted for three! Auden ) from the rest of Eurasia Collaboration for earthquake Simulations on August,. Be higher in Nepal and Tibet the turn of the worst quakes in history. 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In Gorkha, Ilam, Nuwakot, Pokhara, Palpa, Bhimphedi too investigations in Nepal be miles! Himalayan arc and long-term forecasting located in Eastern Nepal about 9.5km ( 5.9mi ) of... Damage, many beyond repair as ground motion, ground displacement, fire, Amazon the. With springs of water for few minuites uprooted and hundreds of bunds had.... That severe shaking occurred in Eastern Nepal Shree M. J Brahma Sumsher old town was also fractured any.., J. Avalanches onMount Everest this earthquake effects of bihar earthquake 1934 manyavalanches on Mount Everest, Rasuwagadhi, Chainpur, Taplejung also damage! * Amazon and the old town was also fractured earthquakes in India 's history and Tibet was! A bridge between the civil lines and the old town was also.! Patna Secretariat had stopped town had a most gruesome spectacle and scarcely a building or wall left... 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