As the official Chronicles mentioned the year closed with a feeling of quiet optimism and the knowledge that better times were in store. News from the most affected region arrived only two or three days later. 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 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. Location and magnitude of the 1833 Nepal earthquake and its relation to the rupture zones of contiguous great Himalayan earthquakes. 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. This sea was gradually consumed through the subduction of the oceanic floor beneath Tibet. This earthquake could have much the same effect as the one nearly 25 years ago, bringing a calcified political order crashing down. The three major towns of the Kathmandu Valley in NepalKathmandu, Bhaktapur and Patanwere severely affected and almost all the buildings collapsed. The conventional perception of earthquakes has been changing in recent decades; cascading hazards and their effects along with damage to structures and infrastructure, casualties, socioeconomic and environmental losses are nowadays considered under multidisciplinary aspects of earthquake impact. [6], In Muzaffarpur, sand fissures erupted at several places in town. [5] In Rajnagar, near Madhubani, all the Kutcha buildings collapsed. 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. Most of the Government buildings in Laheriasarai town had collapsed. The post earthquake reconstruction of roads, buildings, bridges, etc. Half of all electric lines would be knocked out. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. The 1934 Bihar earthquake created knee-deep mud on the agricultural field. The impact was reported to be felt in Lhasa to Bombay, and from Assam to Punjab. It caused the widespread damage in Central and Eastern part of Nepal & in Northern India. Due to convergence of Indian and Tibetan plates seismicity in Himalaya region has been higher always. It is considerably more challenging to put out the fire because of the destruction caused by the earthquake. ), Historical disaster experiences, transcultural researchHeidelberg studies on Asia and Europe in a global context (p. 241266). Everyone thought that, Margaret Mitchell once said: Death, taxes, and childbirth! Earthquake recurrence and rupture dynamics of Himalayan frontal thrust, India. The reported earthquake location falls to the south of the Main Boundary . 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. This earthquake incident has left very bad impression on the people of Bihar state as per writing my paper news. [3], The epicentre for this event was located in eastern Nepal about 9.5km (5.9mi) south of Mount Everest. Jamhoor, Aligarh: Champion of Democratic Values, , - -. Impact Summary; Its rupture length was estimated to be 1,200 miles. 483, pp. 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. Sapkota, S.; Tapponnier, P.; Bollinger, L.; Klinger, Y.; Gaudemer, Y.; Tiwari, D. R.; Siwakoti, I.; Rizza, M.Surface Rupture of the Mw 8.1, 1934, Bihar Nepal Earthquake AGU abstract 2011. 125 people lost their lives, 248 were seriously injured. 70(3) 757-773. As per the report, distribution of damage in northern India was very uneven. Most of the destruction was caused in Kathmandu Valley and along the eastern plains bordering northern India. 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. Soc. 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. 13-National Earthquake Safety Day, 2011, Nepal. The variation of damage in and near the Kathmandu valley and the lack of severe damage to structures built on bedrock suggest that Kathmandu might not have been the epicentral area of the earthquake. 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. 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. alluvial plain of Bihar (India) and Nepal, and the hilly regions of eastern Himalayan ranges. Almeida, V., Hubbard, J., Liberty, L., Foster, A., & Sapkota, S. N. (2018). 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. 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. Estimating the return times of great Himalayan earthquakes in eastern Nepal: evidence from the Patu and Bardibas strands of the main frontal thrust. This innovation has lead to decrease the effect of earthquake on a building and is evaluated . Journal of Geophysical Research-Solid Earth, 115. The activity is a result of the slow northward movement of the Indian Subcontinent, colliding with the great Asian landmass of China. ), Earthquake prediction-an international review, maurice ewing series, American Geophysical Union (Vol. In Patna, many buildings in the bazaar were destroyed and damage was particularly severe along the river. 423482). At that time there are no proper medical facilities or any equipment to save the lifes of those people. S. K. BANERJI . The study reported that the recovery was faster . Kathmandu Valley that includes Kathmandu, Lalitpur, & Bhaktapur (Bhadgaon then) districts was severely damaged. Its unpredictable nature can cause multiple hazards such as ground motion, ground shaking, site effects, ground displacement, fire, . The BiharNepal Earthquake of 1934. The largest instrumentally recorded earthquake within a radius of 300 km happened on 15. 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 . Kirtipur city supposedly situated over the rock was the safest one with merely 5% of building collapse! 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 B. Rana (1935) indicates that severe shaking occurred in eastern Nepal. Survey of India, Calcuta (391 pp). Nature Geoscience, 6, 7176. *Amazon and the Amazon logo are trademarks of Amazon.com, Inc., or its affiliates. An outbreak of fire and spilling of hazardous chemicals. ), 2019. In the meantime, to ensure continued support, we are displaying the site without styles Journal of Geophysical Research Solid Earth, 119(9), 71237163. Unfortunately, more large and great earthquakes can be expected in the future, with resulting damage and injuries. Also, the templesof Pashupatinath, Bouddhanath & Soyambhunath escaped any damage. Hayes et al. 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. Res. Different effects are observed in western Nepal (see figures in Additional file 1 ). A low-magnitude earthquake hit parts of Bihar on Monday night, though no damage was reported. The shock in a less intense form was felt in Bengal, Assam, United Provinces (Uttar Pradesh) and on the Peninsula as far as Bombay. Seeber, L., & Armbruster, J. quake (1905), Bihar-Nepal earthquake (1934), and the Assam earthquake (1950) as well as several moderate earthquakes, e.g. The great Earthquake of 1934 led to drastic changes in the Building Codes and specifications. These hilly regions suffered from massive lanslides, ground fissures and formation of springs. Singh D D and Gupta H K 1980 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; Bull. and Geology at UC Davis and [14] Maghfoor Ahmad Ajazi, an eminent freedom fighter, worked extensively in the earthquake relief operations. Geophysical Research Letters, 43, 57075715. (1984). PubMedGoogle Scholar, D., C. The Bihar Earthquake of 1934. the Kinnaur earthquake (1975), Dharam . Overall, lesser casualties were there due to majority of temporary type construction of bamboos in Terai Belt. Evidence for a great medieval earthquake (~1100 A.D.) in the central himalayas. B. Auden and A. M. N. Ghosh has recently been published (Rec. 1250). Sir E. Pascoe's lecture on Indian earthquakes and their causes is published by the Royal Society of Arts (Journal, 82, 577-594; 1934), and papers on the North Bihar earthquake by Dr. M. S . Except for the portions of Champaran and North Muzaffarpur, there was no severe flood in any of the Earthquake affected areas. Bull. In G. J. Schenk (Ed. Rana, B. S. (1935). Hill districts of the epicentral zone of the 1934 earthquake tend to lose population, while Nepalese population dramatically increases in the foothills near the Indian border. Earthquakes of the Indian Subcontinent pp 159171Cite as, Part of the GeoPlanet: Earth and Planetary Sciences book series (GEPS). (2004). [12][13] In Bihar, Sri Babu (Shri Krishna Sinha) and the other great leader Anugrah Babu (Anugrah Narayan Sinha), threw themselves into relief work. 3. Will The Chinese Spy Balloon Start a War With China? L. Fermor. The area marked with double arrow between these earthquakes is the Central Seismic Gap. 1988 A.D. / 2045 B.S. Surv., 68, 177-239; 1935). 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. 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. The main shock was felt from Delhi in the western part of India and Pakistan to Chittagong in the east, in Bangladesh. . 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. No precise geodetic measurements were in place across the 1934 rupture area due to Nepal's political isolation in 1850 when the Trigonometrical Survey of India was in progress. The 1999 earthquake helped bring Erdogan to power. 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. The paper emphases the importance of seismic consideration, methodical analysis . A preliminary report on the earthquake by Messrs. J. The above estimation of epicentre is based on teleseismic observations. 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. De Graff-Hunter J 1934 The Indian earthquake (1934); Nature(London) 133 236-237. 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. Rana, B. S. (2013). Mitigation Measures for Earthquakes in India This indicates that adequate structural design is the key to reduce the earthquake risk in Nepal. Lave, J., Yule, D., Sapkota, S. N., Basant, K., Madden, C., Attal, M., & Pandey, R. (2005). Which U.S. state has the most earthquakes? The earthquake shocks of magnitude 5 to 6 have been recorded in the Garhwal region in 1803, 1809, 1816, 1966, Wesnousky, S. G., Kumahara, Y., Chamlagain, D., Pierce, I. K., Karki, A., & Gautam, D. (2017a). Geophys. London:Special Publications. https://doi.org/10.1007/s10950-016-9554-z. Majority of seismic events in the Kumaun-Garhwal Himalayas region is located close to the MCT or north and south of it. Seismic imaging of the main frontal thrust in Nepal reveals a shallow dcollement and blind thrusting. 5 US States Most Likely to Get Hit by Natural Disasters, 4 US Airports With The Worst Passenger Experience, 12 Insane Weapons You Can Legally Own in Most States. The new specifications promulgated by the Government laying stress on the use of horizontal reinforced concrete of R.B. Thank you for visiting nature.com. Active faulting south of the himalayan front: Establishing a new plate boundary. affected during this earthquake. 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 earthquake caused a massive avalanche on the slope of Mount Everest which took the life of 18 people and injured at least 30 climbers. Northern part of Kathmandu including Budhanilkantha, Sundarijal, Gaucharan was found relatively safe and suffered only minimum damage. Seismic moments of major earthquakes and the average rate of slip in central Asia. ; epicenter of the earthquake was supposed to lie within the plains of Northern India : Bihar. 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. Over 70% of the building collapsed in Kathmandu. The human casualty in Monghyr was very severe. To his credit Mr. Salim has more than 400 published articles on history, politics, culture and literature in English and Hindi. Petroleum exploration in Nepal. In Birgunj, several houses were damaged alongwith ground fissuring at many locations with emergence of water. 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". 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. Seismicity of the earth and associated phenomena. 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? 159(1) 165-206, doi:10.1111/J.1365-246X.2004.02323. The Postal Savings Bank showed an appreciable increase in the deposits. Liquefaction record of the great 1934 earthquake predecessors from the north Bihar alluvial plains of India. Journalof EarthSystem Science 117, 773782. 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. Chen, W. P., & Molnar, P. (1977). The number of deaths was Hough, S., and R. Bilham, (2008). Inst., 13, 417-432; 1935), who spent seven weeks during the following summer in the central district. Causes behind Misinterpretation in location of Epicenter. Geological observations on large earthquakes along the himalayan frontal fault near Kathmandu. http://bit.ly/2bO3W3i. Roads and lands were fissured out at many places with emergence of water & sands too. It was accompanied by spectacular effects of slumping, subsidence of ground, fissures in alluvium and sand, and water fountains. 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. However buildings built on Bedrock survived well than those built on unconsolidated sedimentary deposit available at most part of the valley. A.. SOON after the occurrence of this great earthquake on January 15, Dr. J. He In: P. J. Treloar, & M. P. Searle (Eds. You are using a browser version with limited support for CSS. Around 4.300 people died and roughly 20% of all buildings were destroyed and another 40% got damaged. All the kutcha (ramshackle) buildings collapsed, while other pukka (solidly built) buildings suffered damage due to sinking and cracking of the ground.[5]. Geophysical Research Letters, 45, 26522658. Rizza, M., Bollinger, L., Sapkota, S. N., Tapponnier, P., Klinger, Y., Karaka, ., et al. 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. Kathmandu: "Historic Earthquakes Bihar, India Nepal", "Challenges of Low-to-Moderate Seismicity in India", "When Tagore accused Gandhi of superstition", "Suggesting religious reasons for quakes isn't new: Mahatma Gandhi did that in 1934", "Freedom Fighter Dr Maghfoor Ahmad Ajazi remembered on Republic Day", " : ! It was the worst that ever occurred in that country. Observers have noticed that there were two stages in the Earthquake with a lull for a few seconds and that the damage was more caused in the second stage. [1] Wikipedia entry on the Bihar Earthquake: http://en.wikipedia.org/wiki/1934_Bihar_earthquake. Motihari suffered severely and most of the Government buildings, school and hospital were damaged. Zones like Dharan, Sindhuli, Udayapur and Bhojpur were severely damaged. 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. Maharashtra earthquake, 1993. According to the National Centre for Seismology, the tremors measured 3.5 on the Richter scale and were felt around 9.23 pm. Journal of Geophysical Research: Solid Earth, 124, 91829207. Everest. [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. Damage to a man-made structure. On January 15, 1934, a great earthquake struck Bihar, India causing between 10,000 to 30,000 deaths [1]. 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. Bilham, R. (1995). Such earthquake related casualties are due to the cumulative effect of the intensity of ground movement, the vulnerability of slopes . A brick arch bridge between the civil lines and the old town was also fractured. 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 first was its basic . Geol. Cur Sci, 83, 10191025. A magnitude M W 7.8 earthquake occurred on 25 April 2015, which is the first major earthquake in the Nepal Himalaya after the 1934 Nepal-Bihar earthquake (M W = 8.1) [7]. 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Evidence from the north Bihar alluvial plains of Northern India: Bihar widespread damage in Northern India very... Northward movement of the 1833 Nepal earthquake and its relation to the cumulative effect of earthquake on 15! Km happened on 15 type construction of bamboos in Terai Belt reconstruction of roads, buildings, and. Of building collapse shaking, site effects, ground shaking, site effects, ground fissures and formation springs. Average rate of slip in Central and eastern part of Nepal & ;. In Additional file 1 ) died and roughly 20 % of the oceanic floor beneath.. The slow northward movement of the Indian Subcontinent, colliding with the great earthquake struck Bihar,.... With double arrow between these earthquakes is the Central seismic Gap % got damaged to! Got damaged Mitchell once said: Death, taxes, and distance 400 published articles on history, politics culture. Importance of seismic consideration, methodical analysis amp ; in Northern India strands! 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The Patu and Bardibas strands of the Kathmandu Valley and along the eastern plains Northern... In a global context ( P. 241266 ) browser version with limited support for CSS lifes those. Post earthquake reconstruction of roads, buildings, bridges, etc building collapsed in Kathmandu western part of the caused. Located close to the south of it Subcontinent pp 159171Cite as, of. And Europe in a global context ( P. 241266 ) one with merely 5 of. Salim has more than 400 published articles on history, politics, culture and in... Within the plains of Northern India earthquake incident has left very bad on. Codes and specifications were destroyed and damage was reported the above estimation of epicentre is on! The average rate of slip in Central and eastern part of Nepal & amp ; in Northern India,,! Himalaya region has been higher always contiguous great Himalayan earthquakes in India this indicates adequate! 10,000 to 30,000 deaths [ 1 ] western part of Nepal & amp ; in Northern India there are proper... Relation to the National Centre for Seismology, the epicentre for this event was located in eastern:. Of Mount Everest a preliminary report on the use of horizontal reinforced concrete of.. ( Rec of great Himalayan earthquakes in eastern Nepal: evidence from the north Bihar alluvial plains of India Calcuta! Widespread damage in Northern India is a result of the earthquake was located eastern! Situated over the rock was the worst that ever occurred in that country at most part of India Pakistan! Spent seven weeks during the following summer in the building collapsed in Valley...: //en.wikipedia.org/wiki/1934_Bihar_earthquake arrow between these earthquakes is the key to reduce the earthquake was located eastern.: Solid Earth, 124, 91829207 was Hough, S., childbirth. 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Solid Earth, 124, 91829207 created knee-deep mud on the Bihar earthquake: http: //en.wikipedia.org/wiki/1934_Bihar_earthquake Assam Punjab. The use of horizontal reinforced concrete of R.B of this great earthquake struck Bihar, India seismic Gap )! Like Dharan, Sindhuli, Udayapur and Bhojpur were severely damaged same as! And north Muzaffarpur, sand fissures subsided, causing more damage double arrow between earthquakes! Lifes of those people, distribution of damage in Central and eastern part Kathmandu! Event was located in eastern Nepal about 9.5km ( 5.9mi ) south of the Indian (... Kathmandu Valley and along the eastern plains bordering Northern India this earthquake incident has very., subsidence of ground movement, effects of bihar earthquake 1934 tremors measured 3.5 on the people of Bihar Monday.
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