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1983 Liège earthquake: Difference between revisions

Coordinates: 50°41′46″N 5°20′46″E / 50.696°N 5.346°E / 50.696; 5.346
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1983 Liège earthquake
1983 Liège earthquake is located in Belgium
1983 Liège earthquake
Brussels
Brussels
UTC time1983-11-08 00:49:32
ISC event564506
USGS-ANSSComCat
Local dateNovember 8, 1983 (1983-11-08)
Local time01:49:32 CET
Magnitude4.7 mb[1]
Depth14 km (9 mi) [1]
Epicenter50°41′46″N 5°20′46″E / 50.696°N 5.346°E / 50.696; 5.346
Areas affectedBelgium Belgium
Netherlands Netherlands
Total damage42 Million[2] - 75 Million[3]
Max. intensityMMI VIII (Severe)
Peak acceleration0.13-0.20 g[4]
Aftershocks+10 aftershocks, the largest being a ML3.4 [5]
Casualties2 fatalities, 30 injuries[6]

The 1983 Liège earthquake occured on 8 november at 01:49 Central European Time, with the epicenter near Remicourt, in Liège province, Belgium. This earthquake's body wave magnitude measured 4.7 and had a depth of around 14km.[1] A Modified Mercalli Intensity of VIII (severe) was observed.[6]The event was followed by more than 10 aftershocks.[5] 2 people died, 30 were injured and over 16000 buildings were damaged.[6][4]The damage cost has been estaminated between 42 million and 75 million Euros.[2][3] It was the biggest earthquake since the 1938 Zulzeke earthquake in the history of Belgium.

Geological setting

The Liège province is situated on the southeastern corner of the Brabant Parautochthon and northeastern side of the Ardenne Allochthon, which are being seperared by the Midi-Eifelian Fault, a segment from the Variscan front thrust. The fault dates back to the Variscan orogeny, a late Paleozoic geologic mountain-building event.[7]

Earthquake

The earthquake which struck on the 8th of november in Remicourt, a munacipality northwest of Liège, was the biggest since the 1983 Zulzeke earthquake in Belgium. It was felt in Belgium, The Netherlands, Germany and Luxembourg. A maximum intensity of VIII (severe) has been observed.[6]More than 10 aftershocks have been registered, the biggest being a ML 3.4.[5] This disaster occured on the Midi-Eifellian fault, with a right latteral strike-slip fault mechanism at a depth of 14km.[1]The peak ground acceleration of the epicentral area was between 0.13-0.20 g.[4]

Impact

The total damage cost ranged from 42 million to 75 million .[2][3]Two individuals lost their lives, one of them due to a heart attack, along with 30 reported injuries.[6]The number of damaged buildings exceeded 16 000. The most common damaged structures were chimneys, roofs and walls.[4]Over 700 families were relocted.[7]

Response

A few weeks after the earthquake, the Belgian Government decided to reimburse part of the repair costs and invited the owners from the most affected localities to report the damage on their properties.[4]

See also

References

  1. ^ a b c d International Seismological Centre (2023), On-line Bulletin
  2. ^ a b c "Project VLA07-4.2 Compilatiestudie betreffende de seismiciteit in Vlaanderen". Project VLA07-4.2 Compilatiestudie betreffende de seismiciteit in Vlaanderen (in Dutch): 'p.26'.
  3. ^ a b c Plumier, Andre; Camelbeeck, Thierry. "Le risque sismique et sa prévention en Région wallonne" (PDF). Le risque sismique et sa prévention en Région wallonne (in French).
  4. ^ a b c d e García Moreno, D.; Camelbeeck, T. (2013-08-07). "Comparison of ground motions estimated from prediction equations and from observed damage during the M = 4.6 1983 Liège earthquake (Belgium)". Natural Hazards and Earth System Sciences. 13 (8): 1983–1997. doi:10.5194/nhess-13-1983-2013. ISSN 1684-9981.{{cite journal}}: CS1 maint: unflagged free DOI (link)
  5. ^ a b c Camelbeeck, Thierry. Seismic Activity in Western Europe with Particular Consideration to the Liège Earthquake of November 8, 1983. Springer Dordrecht. pp. 233–248. ISBN 978-94-009-5273-7.
  6. ^ a b c d e "USGS event page". earthquake.usgs.gov. Retrieved 2023-01-27.
  7. ^ a b Dejonghe, Léon; Cambier, Geoffrey. "Systematic inventory and ordering of faults in Belgium Part 2" (PDF). Systematic inventory and ordering of faults in Belgium Part 2.