Archaeoseismology

Archaeoseismology is the study of past earthquakes deriving from the analysis of archaeological sites. Such analyses reveal information about seismic events that have not been historically recorded. Such data can also help to document seismic risk in areas subject to extremely destructive earthquakes.[1] In 1991, an international conference held in Athens marked the beginning of modern research in the field of archaeoseismology, described as a "study of ancient earthquakes, and their social, cultural, historical and natural effects".[2]

Archeological record

The archaeological record can carry three different types of evidence of seismic activity:

  • The archaeological remains are displaced due to the movement of an active fault.[3]
  • The remains and artefacts contained in destruction deposits, associated with the decline of soil or seismic vibration, can be used the dating of earthquake damage. Other archaeological evidence, such as repairs, abandonment of an archaeological site or architectural changes, can help in identifying ancient earthquakes.[4]
  • Αncient buildings and other man-made structures can be studied for signs of ancient seismic disaster, often associated with soil vibration.[5]

See also

References

  1. Giner-Robles, J.L.; et al. (2012). "Archaeoseismology as an emerging science". Sequridad Y Medio Ambiente. Retrieved 15 March 2016.
  2. Sintubin, Manuel (2012). "Archaeoseismology". In Beer, Michael; Kougioumtzoglou, A. Ioannis; Patelli, Edoardo; Au, Siu-Kui Ιvan (eds.). Encyclopedia of Earthquake Engineering. Berlin, Heidelberg: Springer Berlin Heidelberg. pp. 1–17. ISBN 978-3-642-36197-5.
  3. Altunel, E.; et al. (2003). "Earthquake faulting at ancient Cnidus, SW Turkey". Turkish Journal of Earth Sciences. 12 (1): 137–151.
  4. Marco, S. (2008). "Recognition of earthquake-related damage in archaeological sites: examples from the Dead Sea fault zone". Tectonophysics. 453: 148–156. doi:10.1016/j.tecto.2007.04.011.
  5. Silva, P.G.; et al. (2009). "Surface and subsurface palaeoseismic records at the ancient Roman city of Baelo Claudia and the Bolonia Bay area, Cádiz (south Spain)". Geological Society of London, Special Publications: 93–121.


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.