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1988 Nepal earthquake

(Redirected from 1988 Bihar earthquake)

An earthquake occurred near the Nepal–India border on 20 August 1988 at 23:09:09 UTC.[5] The epicenter was located in Udayapur District.[6] Measuring Mw  6.9, it was the largest earthquake recorded in the country since 1934.[7][8]

1988 Nepal Earthquake
1988 Nepal earthquake is located in Nepal
1988 Nepal earthquake
Epicentre of earthquake
UTC time1988-08-20 23:09:09
ISC event429573
USGS-ANSSComCat
Local dateAugust 21, 1988 (1988-08-21)
Local time04:39:11 NST
Magnitude6.9 Mw [1]
Depth57.4 km (35.7 mi)
Epicenter26°45′18″N 86°36′58″E / 26.755°N 86.616°E / 26.755; 86.616
Max. intensityMMI VIII (Severe)[2][3]
Casualties1,003 deaths, 9,979 injuries[3][4]

The death toll in Nepal and Bihar stood at 1,003.[9] [10] The was worsened by hillside erosion, landslide and floods, which increased the death toll by almost 300.[11] There was significant damage to buildings and infrastructure including schools and hospitals, which left up to half a million people homeless, which had a significant impact of health and desolated the economy.[12][9] This led to overcrowding and a lack of sanitation, which contributed to health conditions. Local and international response relief efforts were hindered by the heavy monsoon, mountainous terrain, infrastructure damage, lack of helicopters and uncoordinated response.[9]

Geology

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The entire region lies above two converging tectonic plates, the Indian and Eurasian plate. These plates are converging at a rate of 40-50 mm/year. [13] The continuous colliding of continental plates results in a seismic energy build-up, which is released in the form of tremors. [14] The Indian plate is continuously submerging beneath the Eurasian plate, rendering the entire of Hindu-Kush-Himalaya region prone to earthquakes.[6] There are three major thrust faults in the region, the Main Central Thrust (MCT), Main Boundary Thrust (MBT) and the Main Frontal Thrust (MFT).[15] This earthquake occurred in the Siwalik sedimentary region and involved oblique faulting with a combination of strike-slip and thrust fault movements contributing to the release of tectonic stress.[11][15]

Within 39 days of the mainshock, the Department of Mines and Geology recorded 155 aftershocks.[11] Six of which had a magnitude greater than 4Mw. [16][5]

Damage and casualties

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Country Deaths Injuries Ref.
    Nepal 721 6213 [9]
  India 282 3766 [9]
Total 1003 9979

In addition to the magnitude of earthquakes, the local geology and the building techniques also affect the extent of damage and devastation.[17] The major causes of fatalities and injuries were from the structural damages to the buildings caused by ground vibration, liquefaction, and landslides.[16] Similar damages to buildings occurred in the northern region of Bihar in India.[18] Considerable damage to buildings were reported in the eastern city of Dharan, rendering thousands of people homeless.[19] The buildings were not constructed to withstand the geological forces of nature as the brick masonry buildings used traditional and poor quality of construction, lacked maintenance, and the foundation designs were inadequate to resist the effects of liquefaction.[18] The lack of regard for the risks of earthquake was evident from the fact, that until 1994, there was no legislation or protocol requirement for earthquake resistant building designs and construction in Nepal; the 1988 earthquake instigated the development of safety initiatives and building codes.[20]

More than 720 fatalities and significant number of injuries were recorded, predominantly in the eastern plains and mountains as well as in some areas in the central mountainous region of Nepal.[6][9] The earthquake caused extensive damage to critical infrastructures, including houses, public buildings, schools, roads, bridges, as well as irrigation canals and water supplies.[6] Damage to the Easter highway at several places and disruption to telecommunications hindered access to the hardest hit areas.[21] Bihar state in India accounted for over 280 deaths and numerous injuries.[9]

The immediate aftermath of the earthquake saw a surge in injuries due to building collapses. Many of these injuries were severe, including crush injuries and fractures, requiring urgent medical attention.[22] The destruction of healthcare infrastructure and the displacement of populations led to an increased risk of infectious disease outbreaks. Poor sanitation, lack of clean water, and overcrowded shelters contributed to the spread of diseases such as diarrhoea, respiratory infections, and fever.[22]

The earthquake impacted educational attainment among children in the worst-affected areas, with the likelihood of completing secondary and tertiary education decreasing by 13.8 percent and 10 percent, respectively. Children from lower caste groups were the most severely affected, with a 17.6 percent reduction in the likelihood of completing secondary education, while children from higher castes were not significantly affected. At the same time, male children perform significantly better than female children in schooling, indicating gender bias in society. These reductions in education levels are directly linked to future health status, with less educated populations typically facing higher health risks and poorer health management skills. The study highlights that natural disasters not only affect education but also have a profound negative impact on children's human capital accumulation and health.[23]

Reports from a Japanese natural disaster study group showed that the causalities were higher among females, children and the elderly, compared to young males, due to their reduced ability to escape from the physical impact of the disaster. In the aftermath of 1988 Nepal earthquakes, personnel at the British military hospital based at Dharan described their experience of lack of facilities in dealing with mass causalities that was compounded by communication loss. They also highlighted the plight of pregnant ladies in labour.[24] The extensive damage to school buildings affected approximately 300,000 children for several months.[25]

Response

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Strong ground motion map

The Nepal government reacted mobilised resources and coordinated efforts across various agencies. The Royal Nepal Army, police, local officials, and the Nepal Red Cross Society collaborated to address the hardest-hit areas, such as Dharan and Dhankuta, despite the government’s limited resources.[26][27] Search and rescue teams were immediately dispatched from Kathmand while the army transported survivors to hospitals. Helicopters were essential in reaching isolated regions to transport survivors to medical facilities.[26][27]

Heavy monsoon rains followed soon after the earthquake, significantly hindering local relief efforts. The effects of these rains were especially challenging in mountainous regions with poor road infrastructure, where helicopters were the only viable option for reaching affected communities. The Nepalese Red Cross provided essential supplies, including food, clothing, blankets, and utensils, particularly in areas where local government support was insufficient. To coordinate the relief, the Home Secretary established the Central Disaster Relief Committee, which allocated over US$300,000 in disaster relief funds to the Eastern Zone.[26][27]

International response

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The United Nations Office for Disaster Risk Reduction quickly recognised the extent of the disaster and launched an international appeal, focusing on monetary donations rather than material aid.[27] The United States was one of the major donors, contributing over $380,000 to supply medical materials, disaster consultants, and plastic sheeting for temporary shelters. Japan also provided critical support, including around 2,000 blankets, medical supplies, and additional relief items, valued at approximately US$450,000.[27] Despite this extensive support, the international response encountered significant logistical challenges. The mountainous terrain, combined with widespread road damage, limited the efficiency of many relief efforts. Helicopters were in short supply and remained the only reliable means of accessing the most affected areas, slowing the distribution of crucial resources. Coordination issues also contributed to delays, emphasising the need for robust disaster response frameworks that can aid countries facing challenging conditions.[27]

Legacy

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Weak infrastructure, specifically medical facilities, transportation systems and communication networks, were particularly exposed after the earthquake. The destruction of roads and bridges after the earthquake resulted in the inability of relief supplies and personnel to reach the affected areas promptly. Future earthquakes could cause even greater damage unless regular reinforcements and countermeasures are implemented.[28]

After the 1988 Nepal earthquake, several disaster mitigation programmes were implemented in Nepal.[29] The Nepal Seismic Safety Centre (NSET) initiated the School Seismic Safety Program in 1998. The program helped to strengthen school buildings, their non-structural components.[30]. It was later expanded to include first aid training, disaster response plans, and the integration of Disaster Risk Management into school curricula.[25]

See also

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References

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  1. ^ ISC (19 January 2015), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 2.0, International Seismological Centre
  2. ^ PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey, September 4, 2009
  3. ^ a b National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Database (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K
  4. ^ Fujiwara, T.; Sato, T.; Kubo, T.; Murakami, H.O. (1989). "On the 21 August 1988 earthquake in the Nepal-India border region". Japanese Group for the Study of Natural Disaster Science. Reconnaissance Report No B-63-4.
  5. ^ a b "M 6.9 - 9 km WSW of Triyuga, Nepal". United States Geological Survey. Retrieved 29 October 2024.
  6. ^ a b c d Chaulagain, Hemchandra; Gautam, Dipendra; Rodrigues, Hugo (2018), "Revisiting Major Historical Earthquakes in Nepal", Impacts and Insights of Gorkha Earthquake in Nepal, Elsevier, pp. 1–17, ISBN 978-0-12-812808-4, retrieved 2024-11-03
  7. ^ Jain, Sudhir K. (August 1992). "On Better Engineering Preparedness: Lessons from the 1988 Bihar Earthquake". Earthquake Spectra. 8 (3): 391–402. doi:10.1193/1.1585687. ISSN 8755-2930.
  8. ^ Whelpton, John (2021). "Earthquakes in Nepali History". In Hutt, Michael; Liechty, Mark; Lotter, Stefanie (eds.). Epicentre to aftermath: rebuilding and remembering in the wake of Nepal's earthquakes. Cambridge, United Kingdom New York, NY: Cambridge University Press. ISBN 978-1-108-83405-6.
  9. ^ a b c d e f g Fujiwara, T; Sato, T; Murakami, H.O. (1989). "On the 21 August 1988 earthquake in the Nepal-India border region". Japanese Group for the Study of Natural Disaster Science. Reconnaissance Report No B-63-4.
  10. ^ "Significant Earthquake Information". National Oceanic & Atmosphere Administration (NOAA). Retrieved 17 November 2024.
  11. ^ a b c Pande, M. R.; Nicolas, M. (1991-12-01). "The aftershock sequence of the Udaypur (Nepal) earthquake of August 20, 1988". Journal of Nepal Geological Society. 7. doi:10.3126/jngs.v7i0.32589. ISSN 2676-1378.
  12. ^ Bista, Dor Bahadur (February 1989). "Nepal in 1988: Many Losses, Some Gains". Asian Survey. 29 (2): 223–228. doi:10.1525/as.1989.29.2.01p0251s. ISSN 0004-4687.
  13. ^ "USGS Open-File Report 2010‒1083–J: Seismicity of the Earth 1900‒2010 Himalaya and Vicinity". pubs.usgs.gov. Retrieved 2024-11-12.
  14. ^ Shanker, D.; Paudyal, Harihar; Singh, H. N. (2012-08-31). "Discourse on Seismotectonics of Nepal Himalaya and Vicinity:Appraisal to Earthquake Hazard". Journal of Geo-sciences. 1 (1): 1–15. doi:10.5923/j.geo.20110101.01. ISSN 2163-1697.
  15. ^ a b Ghimire, Subesh; Kasahara, Minoru (October 2007). "Source process of the Ms = 6.6, Udayapur earthquake of Nepal–India border and its tectonic implication". Journal of Asian Earth Sciences. 31 (2): 128–138. doi:10.1016/j.jseaes.2007.04.007.
  16. ^ a b Dikshit, A. M. (1991-12-01). "Geological effects and Intensity distribution of the Udayapur (Nepal) earthquake of August 20, 1988". Journal of Nepal Geological Society. 7. doi:10.3126/jngs.v7i0.32588. ISSN 2676-1378.
  17. ^ "How do earthquakes affect people?". British Geological Survey. Retrieved 2024-11-22.
  18. ^ a b Thakkar, S.; Paul, D.; Mukerjee, S.; Bandyopadhyay, S.; Kumar, Ashwani; Lavania, B. (1991-03-11). "Behavior of Buildings in August 21, 1988 Bihar-Nepal Earthquake". International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics.
  19. ^ Chamlagain, Deepak; Bhattarai, Ganesh Kumar; Rajaure, Sudhir (2011-09-24). "Seismic hazard assessment of eastern Nepal using 1934 and 1988 earthquakes". Journal of Nepal Geological Society. 42: 85–93. doi:10.3126/jngs.v42i0.31453. ISSN 2676-1378.
  20. ^ Bothara, J., Dizhur, D., Dhakal, R.P. and Ingham, J., (2018) From the 1988 Udaypur to the 2015 Gorkha Earthquake, Nepal and beyond. In 2018 NZSEE Conference, New Zealand Society for Earthquake Engineering.
  21. ^ "Nepal Earthquake Aug 1988 UNDRO Situation Reports 1 - 8 - Nepal". reliefweb.int. 1988-08-22. Retrieved 2024-11-21.
  22. ^ a b Mavrouli, Maria; Mavroulis, Spyridon; Lekkas, Efthymios; Tsakris, Athanassios (2023-02-07). "The Impact of Earthquakes on Public Health: A Narrative Review of Infectious Diseases in the Post-Disaster Period Aiming to Disaster Risk Reduction". Microorganisms. 11 (2): 419. doi:10.3390/microorganisms11020419. ISSN 2076-2607. PMC 9968131. PMID 36838384.{{cite journal}}: CS1 maint: unflagged free DOI (link)
  23. ^ Paudel, Jayash; Ryu, Hanbyul (November 2018). "Natural disasters and human capital: The case of Nepal's earthquake". World Development. 111: 1–12. doi:10.1016/j.worlddev.2018.06.019.
  24. ^ Guy, P. J.; Ineson, N.; Bailie, R.; Grimwood, A. (1990-02-01). "Operation Nightingale: The Role of BMH Dharan Following the 1988 Nepal Earthquake, and Some Observations on Third World Earthquake Disaster Relief Missions". BMJ Military Health. 136 (1): 7–18. doi:10.1136/jramc-136-01-02. ISSN 2633-3767. PMID 2319510.
  25. ^ a b Dixit, Amod Mani; Yatabe, Ryuichi; Dahal, Ranjan Kumar; Bhandary, Netra Prakash (2014-10-02). "Public School Earthquake Safety Program in Nepal". Geomatics, Natural Hazards and Risk. 5 (4): 293–319. doi:10.1080/19475705.2013.806363. ISSN 1947-5705.
  26. ^ a b c Office of U.S. Foreign Disaster Assistance. "Disaster Case Report: NEPAL- Earthquake FY 1988" (PDF). Office of U.S. Foreign Disaster Assistance.
  27. ^ a b c d e f "Nepal Earthquake Aug 1988 UNDRO Situation Reports 1 - 8 - Nepal". reliefweb.int. 1988-08-22. Retrieved 2024-11-03.
  28. ^ Gautam, Dipendra (1 August 2017). "On seismic vulnerability of highway bridges in Nepal: 1988 Udaypur earthquake (MW 6.8) revisited". Soil Dynamics and Earthquake Engineering. 99: 168–171. doi:10.1016/j.soildyn.2017.05.014. ISSN 0267-7261. Retrieved 24 November 2024.
  29. ^ Bothara, Jitendra; Ingham, Jason; Dizhur, Dmytro (1 January 2018). "Chapter 11 - Earthquake Risk Reduction Efforts in Nepal". Integrating Disaster Science and Management. Elsevier: 177–203. Retrieved 24 November 2024.
  30. ^ Bothara, J. K.; Pandey, B.; Guragain, R. (31 March 2004). "Seismic retrofitting of low strength unreinforced masonry non-engineered school buildings". Bulletin of the New Zealand Society for Earthquake Engineering. 37 (1): 13–22. doi:10.5459/bnzsee.37.1.13-22. ISSN 2324-1543. Retrieved 24 November 2024.
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